HomeMy WebLinkAboutCT 05-13; La Costa Ridge Neighborhood 2.6 - Horton; La Costa Ridge Neighborhood 2.6; 2007-10-01Initial Date
HYDROLOGY AND HYDRAULICS SI BUY
RECORD COPY
AU
FOR
LA COSTA RIDGE NEIGHBORHOOD 2.6
CARLSBAD, CALIFORNIA
PREPARED FOR:
D. R. HORTON
5790 FLEET ST., SUITE 210
CARLSBAD, CA 92009
(760)929-1600
PREPARED BY:
DAVID EVANS AND ASSOCIATES, INC.
800 NORTH HAVEN AVENUE, SUITE 300
ONTARIO, CA 91764
(909)481-5750
JUNE, 2006
REVISED FEBRUARY 2007
REVISED APRIL 2007
REVISED OCTOBER 2007
DRHH0030
AND AS "T sr o.
o
UJ
Xoz
HYDROLOGY AND HYDRAULICS STUDY
FOR
LA COSTA RIDGE NEIGHBORHOOD 2.6
CARLSBAD, CALIFORNIA
PREPARED FOR:
D. R. HORTON
5790 FLEET ST., SUITE 210
CARLSBAD, CA 92009
(760)929-1600
PREPARED BY:
WAGNER HAWTHORNE, P.E.
JUNE, 2006
REVISED FEBRUARY 2007
REVISED APRIL 2007
REVISED OCTOBER 2007
DRHH0030
TABLE OF CONTENTS
A. Purpose of Study and Narrative 1
B. Location and Vicinity Map 2
C. Methodology 3
D. Tables and References 4
Rational Method Appendix A
Hydrology Table - Software input data
10 yr Developed Flows
100 yr Developed Flows
Catch Basin Calculations Appendix B
Storm Drain Hydraulic Calculations Appendix C
Rip rap (splash guard at channel) Calculations Appendix D
Hydrology K Maps Back Pocket
Developed Hydrology Map
A. PURPOSE OF STUDY AND NARRATIVE
The purpose of this study is to satisfy the City of Carlsbad drainage concerns
for the development of "La Costa Ridge Neighborhood 2.6". The Drainage
study is based on the San Diego County Hydrology Manual, June 2003. A
rational method study of the tributary area will be used to determine the flow
rate entering and being generated on the site.
EXISTING DRAINAGE CONDITIONS:
The La Costa Ridge Neighborhood 2.6 site is part of the La Costa Ridge
development in the City of Carlsbad, California. The site has been mass
graded in anticipation for residential development per the "Grading and
Erosion Control Plans for La Costa Ridge Stockpile Plan" dated September,
2004 by Hunsaker & Associates.
The "Mass Grading Hydrology Study for the Villages of La Costa
Neighborhoods 2.1 through 2.5" dated January, 2004 by Hunsaker &
Associates, shows a 48-inch storm drain, located within the adjacent Corintia
Street, conveys a flow of approximately 154 cfs from the neighboring La
Costa Ridge Neighborhood 2.5.
This 48-inch RCP storm drain discharges runoff to the project site, into a
trapezoidal earthen channel that drains to San Marcos Creek, a 2-ft deep by
10-ft wide concrete channel that runs southeast of the project boundary. The
Regional Water Quality control Board has identified San Marcos Creek as
part of the Carlsbad Hydrologic Unit, San Marcos Hydrologic Area, and the
Batiquitos Subarea (basin number 904.51).
PROPOSED CONDITIONS:
Development of the La Costa Ridge Neighborhood 2.6 will consist of
approximately 10 acres of single family residences, foot paths, communal
open space and underground utilities with two (2) entrances from the adjacent
Corintia Street.
Runoff generated by the proposed development will be conveyed in a
southerly direction via a curb and gutter system within the proposed site,
draining to a curb inlet and a sidewalk under drain, which discharges to a
vegetated swale in the park area. Flows from the adjacent Neighborhood 2.5
48-inch RCP storm drain will be conveyed south in a proposed storm drain
extension system within the proposed development. A concrete structure has
been designed at the junction of the storm drain outlet and the San Marcos
Creek concrete channel. Rip-rap has also been designed as slope protection
on the opposing bank of the channel.
Two existing catch basins located on Corintia that drain to a existing cleanout
on the existing 48-in storm drain will be removed and the connector 24-in pipe
will be plugged at the cleanout. The street runoff from an existing catch basin
to the west, upstream of the southern project entrance will be diverted and
routed through the project site, being collected at the sidewalk under drain.
The drainage study will be revised to reduce the additional area draining to
the existing catch basin at Corintia and Melrose by ± 0.30-acres. This
reduction will occur because the south easterly half of Corintia south of "A"
Street (as labled on the TTM) will be conveyed onto this project and will not
continue north to the intersection of Corintia and Melrose. This run-off is from
the private portion of Corintia. Based on this reduction there will be less than
1 cfs conveyed to the existing catch basin. We believe the analysis that the
City is requesting is a significant engineering effort for an increase flow rate of
less than 1 cfs.
As the runoff conveyed by the existing 48-in storm drain, which discharges to
an open channel, is being canalized through a proposed 48-in storm drain
system, and as a 24-in connector is being plugged at the receiving cleanout,
an analysis of the hydraulic grade line has been performed to ensure the
water surface elevation at the cleanout will not reach the street surface level.
The analysis shows that the HGL-100 will be contained within the storm drain
system and thus the existing condition has been unchanged.
Flows from Neighborhood 2.6 site will discharge to the receiving San Marcos
Creek. Discharge to the receiving San Marcos Creek was analyzed per the
"Preliminary Hydrology for Villages of La Costa - The Ridge and the Oaks"
dated April, 2001 by Hunsaker & Associates.
Creek concrete channel. Rip-rap has also been designed as slope protection
on the opposing bank of the channel.
Two existing catch basins located on Corintia that drain to a existing cleanout
on the existing 48-in storm drain will be removed and the connector 24-in pipe
will be plugged at the cleanout. The street runoff from an existing catch basin
to the west, upstream of the southern project entrance will be diverted and
routed through the project site, being collected at the sidewalk under drain.
The rest of the street flows from the southern entrance towards Melrose will
be directed to an existing catch basin on Corintia near the intersection with
Melrose Drive.
As the runoff conveyed by the existing 48-in storm drain, which discharges to
an open channel, is being canalized through a proposed 48-in storm drain
system, and as a 24-in connector is being plugged at the receiving cleanout,
an analysis of the hydraulic grade line has been performed to ensure the
water surface elevation at the cleanout will not reach the street surface level.
The analysis shows that the HGL-100 will be contained within the storm drain
system and thus the existing condition has been unchanged.
Flows from Neighborhood 2.6 site will discharge to the receiving San Marcos
Creek. Discharge to the receiving San Marcos Creek was analyzed per the
"Preliminary Hydrology for Villages of La Costa - The Ridge and the Oaks"
dated April, 2001 by Hunsaker & Associates.
B. LOCATION AND VICINITY MAP
t i t «t i t t * i
(CARLSBAD
^^~X ^
C/7Y OF ENCINITAS
VICINITY MAP
C/7Y OF
SAN MARCOS
PROJECT
TE
NTS
'':;''-~'-l t: l*f' •^%SL\^'';iWiS
\K\ jSfttl;^ 1^^
PROJECT SITE
C. METHODOLOGY
All drainage design and requirements shall be in accordance with the latest
City of Carlsbad Standard Urban Storm Water Mitigation Plan (SUSMP),
jurisdictional Urban Runoff Management Plan (JURMP), Master Drainage and
Storm Water Quality Management Plan and the requirements of the City
Engineer and be based on full development of upstream tributary basins.
Public drainage facilities shall be designed to carry the ten-year six-hour
storm underground and the 100-year six-hour storm between the top of curbs.
All culverts shall be designed to accommodate a 100-year six-hour storm
with a one foot freeboard at entry conditions such as inlets and head walls.
The Rational Method (RM) is a mathematical formula used to determine the
maximum runoff rate from a given rainfall. It has particular application in
urban storm drainage, where it is used to estimate peak runoff rates from
small urban and rural watersheds for the design of storm drains and small
drainage structures. The RM is recommended for analyzing the runoff
response from drainage areas up to approximately 1 square mile in size. It
should not be used in instances where there is a junction of independent
drainage systems or for drainage areas greater than approximately 1 square
mile in size. In these instances, the Modified Rational Method (MRM) should
be used for junctions of independent drainage systems in watersheds up to
approximately 1 square mile in size; or the NRCS Hydrologic Method should
be used for watersheds greater than approximately 1 square mile in size.
The RM formula estimates the peak rate of runoff at any location in a
watershed as a function of the drainage area (A), runoff coefficient (C), and
rainfall intensity (I) for a duration equal to the time of concentration (Tc),
which is the time required for water to flow from the most remote point of the
basin to the location being analyzed. The RM formula is expressed as follows:
Q = CIA
Where: Q = peak discharge, in cubic feet per second (cfs)
C = runoff coefficient, proportion of the rainfall that runs off the surface (no
units)
I = average rainfall intensity for a duration equal to the Tc for the area, in
inches per hour (Note: If the computed Tc is less than 5 minutes, use 5
minutes for computing the peak discharge, Q)
A = drainage area contributing to the design location, in acres
The software used to solve the rational method hydrology models is the
CICILCADD/CIVILDESIGN Hydrology and Hydraulics Package by Civil
Design Corporation, San Bernardino, CA.
D. TABLES AND REFERENCES
32*30'
County of San Diego
Hydrology Manual
Soil Hydrologic Groups
Legend
Soil Groups
Group A
Group B
Group C
Group D
Undetermined
Data Unavailable
DPWe^GIS
09fartr.en< ofPuific Warns CIS
Have San l!Hugt'j (Covered!
THIS MAP IS PROVIDED WITHOUT WARRANTY OF ANY KIND, EITHER EXPRE!
OR IMPLIED, INCLUDING, BUT NOT LIMITED TO, THE IMPLIED WARRANTIES
OF MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE.
Copyright SanGIS. All Rights Reserved.
This products may contain information from the SANDAG Regional
*C Information System which cannot be reproduced without the1-J written permission of SANDAG.
This product may contain Information which has been reproduced with
permission granted by Thomas Brothers Maps.
3 Miles
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Riverside County
32°30(
32°30'
County of San Diego
Hydrology Manual
Rainfall Isopluvials
10 Year Rainfall Event - 6 Hours
Isopluvial (inches)
\X'o Hive San Dicgu (..o
THIS MAP IS PROVIDED WITHOUT WARRANTY OF ANY KIND, EITHER EXPRESS
OR IMPLIED, INCLUDING, BUT NOT LIMITED TO, THE IMPLIED WARRANTIES
OF MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE.Copyright SanGIS. All Rights Reserved
This products may contain Information from the SANDAG RegionalInformation System which cannot be reproduced without thewritten permission at SANDAG.
This product may contain Information which has been reproduced with
permission granted by Thomas Brothers Maps.
303 Miles
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33°30'
Riverside County
32°45'
32°30'32°30'
County of San Diego
Hydrology Manual
Rainfall Isopluvials
10 Year Rainfall Event - 24 Hours
Isopluvial (inches)
DPW CIS
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vered!
THIS MAP IS PROVIDED WITHOm' WARRAhfTY OF ANY KIND, EITHER EXPRESS
OR IMPLIED. INCLUDING, BUT NOT LIMfTED TO, THE IMPLIED WARRANTIES
OF MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE.
Copyright SanGIS. All Rights Reserved
This products may contain Information from the SANDAG Regional
Information System which cannot be reproduced without the
written permission of SANDAG.
This product may contain Information which has been reproduced with
permission granted by Thomas Brothers Maps.
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32°30'
County of San Diego
Hydrology Manual
Rainfall Isopluvials
100 Year Rainfall Event - 6 Hours
Isopluvial (inches)
DPWCIS
_ Sjn
THIS MAP IS PROVIDED WITHOUT WARRANTY OF ANY KIND, EITHER EXPRESS
OR IMPLIED, INCLUDING, BUT NOT LIMITED TO, THE IMPLIED WARRANTIES
OF MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE.
Copyright SanGIS. All Rights Reserved.
This products may contain Information from the SANDAG Regional
Information System which cannot be reproduced witnout the
written permission of SANDAG.
This product may contain Information which has been reproduced with
permission granted by Thomas Brothers Maps.
3 Miles
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County of San Diego
Hydrology Manual
Rainfall Isopluvials
100 Year Rainfall Event - 24 Hours
Isopluvial (inches)
DPW CIS
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THIS MAP IS PROVIDED WITHOUT WARRANTY OF ANY KIND, EITHER EXPRESSOR IMPLIED, INCLUDING, BUT NOT LIMITED TO, THE IMPLIED WARRANTIES
OF MERCHANTABIUTY AND FITNESS FOR A PARTICULAR PURPOSE.Copyright SanSIS. All Rights Reserved.
This products may contain Information from the SANDAG Regional
InfOfmation System wnich cannot be reproduced without the
written permission of SANDAG.
This product may contain information which has been reproduced withpermission granted by Thomas Brothers Maps.
3 Miles
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jgy Manual (10, 50, and 100 yr maps included
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Jesert),
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rough the point parallel to the plotted lines.
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530 636 742!8.48 9.54 1060 1166 1272
421 505 590; 674 ' 7.58 ' 842 927 1011
324 389.454' 519' 5.84 649 713 7.78
2 69 3 23 3 77 4 31 ' 4 85 5 39 5 93 ' 6.46
2 33 2 80 3 27' 3.73 '. 4,20 ] 4 67 5 13 ] 5.60
207 249*290; 3.32; 3.73 4.15 4.56 4.98
1 72 207j241i 276 ', 3.10 I 3.45 379 4.13
1 49* 1 79(2 09| 2.39 1 2.69 2.98 3.28 3.58
1 33 ' 1 59! 1 86; 2.12 ! 2.39 ' 2.65 2 92 ' 3.18
1 02 1 23 1 1 43! 1.63 ] 1.84 ' 2.04 2 25 t 2.45
0 85 1 02' 1 19; 1.36 j 1 S3 ' 1.70 1.87 2 04
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[065,0781091^1041118 131 14411.57
'054 Q65l076 0.87 j 098 108 119 1.30
047 056 1 066" 0.75 085 0.94 103 113
0.42 050 058" 067 ' 075 ' 084 092 100
FIGURE
Intensity-Duration Design Chart - Template 3-1
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ie selected frequency. These maps are included in the
nty Hydrology Manual (10, 50, and 100 yr maps included
e Design and Procedure Manual).
st 6 hr precipitation (if necessary) so that it is within
ange of 45% to 65% of the 24 hr precipitation (not
icaple to Desert).
6 hr precipitation on the right side of the chart.
n a line through the point parallel to the plotted lines.
line is the intensity-duration curve for the location
g analyzed.
itlon Form:
cted frequency ^ QQ year
-4 P24
sted P6<2> * in.
min.
in./hr.
•^lote: This chart replaces the Intensity-Duration-Frequency
curves used since 1965.
PJL,Duration1
S
7
10
15
20
25
30
40
SO
60
120
150
180
240
300
~360~
1 ,1,5 2 2.5 3 3.5 4 4.5 S 5.5 6
I ; I ' 1 ' 1 1 1 ' 1 ' 1 1 1 t
263 395^527' 659 790 922 10 54 1186 1317 1449 1581
2 12 "3 18' 4 24* 5 30 636 742 848 ' 954 1060 1166 1272
168 "2 53] 3 37* 4 21 505590" 674 758 842 927 1011
"1.30*195259*324 389(454 519 584 649 713 778
108 '162 215[269 323 377 431 485 539 593 646
093 !1.40| 187 233 280 337' 3.73 ' 420 467 513 560
083 '124 t.66'207 2.49!29fl' 332 ' 373 415 456 4.98
069 ,1 03*1 38J 1 72 207>241i 276 ' 3 10 345 379 413
060 1090J1 19' 1 49 1 79 209' 239 269 298 328 358
053l080!106i 1 33 1 59 1 861 2 12 239 265 292 318
041 !061]0821 102 123,1 43 163 ' 184 204 '225 245
0.34 1051]068f085 102 1 19h.36 , 153 ' 170 187 204
029 10440591073 088* 1 03M 18 ', 132 , 1 47 162 176
0.26 |039[052|06S 0781091; 104 ! 1.18 131 1 44 1 1.57
6.22 10.33' 0.4310 54 'o.eSiO 76* 087 098^ 108* 1 19 j 1 30
0.19 1028!038[047'056j066 075 ' 085 094*103 1.13
017 '025' 0,331 042*0 SO1 058' 067 ' 075 ' 084 092 ' 100
Intensity-Duration Design Chart - Template
FIGURE
3-1
RATIONAL METHOD
SUMMARY OF TRIBUTARY CONDITIONS
PROJECT: DRHH0030 - LA COSTA RIDGE
STRUCT / FACILITY: DEVELOPED HYDROLOGY
SEGMENT
UP
10
20
30
35
40
40
50
60
70
80
80
90
92
90
100
110
120
120
130
140
150
150
160
160
170
170
170
DOWN
20
30
40
40
90
90
60
70
80
90
90
92
190
190
110
120
160
160
140
150
160
160
180
180
180
180
180
FLOW TYPE
INITIAL
STREET
STREET
SUB-ADD
STREET
ELEVATIONS
UP
388.0
377.0
365.0
358.0
DOWN
377.0
365.0
358.0
346.1
CONFLUENCE OF MINOR STREAMS 1/2
INITIAL
STREET
STREET
STREET
354.7
352.3
352.0
350
352.3
352.0
350
346.1
CONFLUENCE OF MINOR STREAMS 2/2
IMPROV CHANNEL
PIPE
346.1
335.5
343.5
329.1
CONFLUENCE OF MAJOR STREAMS 1/2
INITIAL
STREET
STREET
355.2
353.0
351.5
353
351.5
346.2
CONFLUENCE OF MINOR STREAMS 1/2
INITIAL
STREET
STREET
355.6
353.4
351.0
353.4
351.0
346.1
CONFLUENCE OF MINOR STREAMS 2/2
PIPE 340.0 335.0
CONFLUENCE OF MINOR STREAMS 1/2
USER DEFINED FLOW INFORMATION
PIPE 347.2 329.8
CONFLUENCE OF MINOR STREAMS 2/2
LENGTH
(ft)
100.0
190.0
200.0
460.0
180.0
180.0
178.0
412.0
80.0
35.0
100.0
151.0
485.0
100.0
163.0
290.0
15.0
535.0
LAND USE
COMMERCIAL
COMMERCIAL
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
RES. MED. DENSITY
AREA
(AC)
0.07
0.13
0.33
1.33
0.25
0.4
0.88
1.20
0.17
0.11
0.41
0.87
0.12
0.74
0.88
SUB-ADD
AREA (AC)
0.56
SOIL TYPE
100%D
100%D
100% D
100%D
100%D
100%D
100%D
100%D
100%D
100%D
100%D
100%D
100%D
100%D
1 00% D
100 yr
Qtrib
(CFS)
0.44
0.69
1.05
1.97
3.31
7.46
0.80
0.86
1.98
2.06
5.70
0.20
11.14
11.14
0.30
1.00
1.60
2.90
0.40
2.21
2.09
4.70
6.64
6.64
154.00
154.00
154.00
^cumulative
(CFS)
0.44
1.13
2.17
4.14
7.46
7.46
0.80
1.66
3.64
5.70
10.94
11.14
11.14
11.14
0.30
1.30
2.90
2.90
0.40
2.61
4.70
6.64
6.64
6.64
154.00
154.00
159.50
P:\D\DRHH00000030\0600INFO\EC\Hydrology\HYDTABLE2.xls 10/25/2007
SUMMARY OF TRIBUTARY CONDITIONS
PROJECT: DRHH0030 - LA COSTA RIDGE
STRUCT / FACILITY: DEVELOPED HYDROLOGY
SEGMENT
UP
180
180
190
320
330
340
345
DOWN
190
190
200
330
340
350
350
FLOW TYPE
PIPE
ELEVATIONS
UP
329.8
DOWN
329.1
CONFLUENCE OF MAJOR STREAMS 2/2
PIPE
INITIAL
STREET
STREET
SUB-ADD
329.1
363.0
360.8
355.0
328.3
360.8
359.5
347.0
LENGTH
(ft)
74.0
79.0
180.0
170.0
421.3
LAND USE
COMMERCIAL
COMMERCIAL
COMMERCIAL
COMMERCIAL
AREA
(AC)
0.16
0.13
0.38
SUB-ADD
AREA (AC)
0.64
SOIL TYPE
100%D
100%D
100%D
100 yr
Qtrib
(CFS)
159.50
159.50
169.50
0.89
0.47
1.24
2.45
^cumulative
(CFS)
159.50
169.50
169.50
0.89
1.36
2.60
5.05
P:\D\DRHH00000030\0600INFO\EC\Hydrology\HYDTABLE2.xls 10/25/2007
10 yr Developed Flows
san Diego County Rational Hydrology Program
CIVILCADD/CIVILDESIGN Engineering Software,(c)1991-2004 version 7.4
Rational method hydrology program based on
san Diego County Flood Control Division 2003 hydrology manualRational Hydrology study Date: 10/04/07
JN DRHH0030 - LA COSTA RIDGE
DAVID EVANS AND ASSOCIATES, INC.
DEVELOPED FLOWS TO EXISTING PIPE - 1/17/06, REV 10/04/07
P:\D\DRHH0030\600lNFO\EC\HYDROLOGY\DEV2
********* Hydrology Study control information **********
Program License Serial Number 4009
Rational hydrology study storm event year is 10.0
English (in-lb) input data units used
Map data precipitation entered:
6 hour, precipitation (inches) = 1.900
24 hour precipitation(inches) = 3.250
P6/P24 = 58.5%
San Diego hydrology manual 'c1 values used
Process from Point/Station 10.000 to Point/Station 20.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(General commercial )
impervious value, Ai = 0.850
Sub-Area C Value = 0.820
initial subarea total flow distance = 100.000(Ft.)
Highest elevation = 388.000(Ft.)
Lowest elevation = 377. 000 (Ft.)
Elevation difference = 11.000(Ft.) slope = 11.000 %
Top of initial Area slope adjusted by user to 1.000 %
Bottom of initial Area slope adjusted by user to 1.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 60.00 (Ft)
for the top area slope value of 1.00 %, in a development type of
General Commercial
In Accordance with Figure 3-3
initial Area Time of Concentration = 3.90 minutes
TC = [1.8*(l.l-C)*distance(Ft.)A.5)/(% slopeA(l/3)]
TC = [1.8*(1.1-0.8200)*( 60.000A.5)/( 1.00QA(l/3)]= 3.90
The initial area total distance of 100.00 (Ft.) entered leaves a
remaining distance of 40.00 (Ft.)
using Figure 3-4, the travel time for this distance is 0.79 minutes
for a distance of 40.00 (Ft.) and a slope of 1.00 %
with an elevation difference of 0.40(Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)
0.787 Minutes
Tt=[(11.9*0.0076A3)/( 0.40)]A.385= 0.79
Total initial area Ti = 3.90 minutes from Figure 3-3 formula plus
0.79 minutes from the Figure 3-4 formula = 4.69 minutes
Rainfall intensity (I) = 5.216(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is c = 0.820
Subarea runoff = 0.299(CFS)
Total initial stream area = 0.070(Ac.)
Page 1 of 14
10 yr Developed Flows
H-+++++++++++++++++++++++4
Process from Point/Station 20.000 to Point/Station 30.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 377.000(Ft.)
End of street segment elevation = 365.000(Ft.)
Length of street segment = 190.000(Ft.)
Height of curb above gutter flow/line = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)Gutter hike from flowline = 1.500 (in.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street = 0.504(CFS)Depth of flow = 0.150(Ft.), Average velocity = 3.405(Ft/s)Streetflow hydraulics at midpoint of street travel:
Half street flow width = 2. 772 (Ft.)Flow velocity = 3.40(Ft/s)Travel time = 0.93 mi n. TC = 5.62 min.Adding area flow to streetDecimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[COMMERCIAL area type ](General Commercial )impervious value, Ai = 0.850Sub-Area c value = 0.820Rainfall intensity = 4.642(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area(Q=KCIA) is C = 0.820 CA = 0.164subarea runoff = 0.462(CFS) for 0.130(Ac.)Total runoff = 0.761(CFS) Total area = 0.200(Ac.)Street flow at end of street = 0.761(CFS)
Half street flow at end of street = 0.761(CFS)Depth 9f flow = 0.170(Ft.), Average velocity = 3.561(Ft/s)Flow width (from curb towards crown)= 3.775(Ft.)
Process from Point/Station 30.000 to Point/Station 40.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 365.000(Ft.)
End of street segment elevation = 358.000(Ft.)
Length of street segment = 200.000(Ft.)
Height of curb above gutter flowline = 6.0(In.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)
Gutter hike from flowline = 1.500 (in.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.145(CFS)
Depth of flow = 0.206(Ft.), Average velocity = 3.021(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Half street flow width = 5. 547 (Ft.)
Flow velocity = 3.02(Ft/s)
Travel time = 1.10 min. TC = 6.72 min.
Page 2 of 14
10 yr Developed Flows
Adding area flow to streetDecimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ](7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area c value = 0.570
Rainfall intensity = 4.135(ln/Hr) for a 10.0 year stormEffective runoff coefficient used for total area
(Q=KCIA) is C = 0.664 CA = 0.352
Subarea runoff = 0.695(CFS) for 0.330(Ac.)
Total runoff = 1.456(CFS) Total area = 0.530(Ac.)
Street flow at end of street = 1.456(CFS)Half street flow at end of street = 1.456(CFS)
Depth of flow = 0.219(Ft.), Average velocity = 3.180(Ft/s)
Flow width (from curb towards crown)= 6.218(Ft.)
+++++++++++++++++++++++++++++4
Process from Point/station
**** SUBAREA FLOW ADDITION ****
35.000 to Point/Station 40.000
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400Sub-Area C value = 0.570Time of concentration = 6.72 min.Rainfall intensity = 4.135(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.616 CA = 0.671subarea runoff = 1.320(CFS) for 0.560(Ac.)Total runoff = 2.776(CFS) Total area = 1.090(Ac.)
+++++++++++++++++++++++++++H
Process from Point/Station
**** STREET FLOW TRAVEL TIME +
40.000 to Point/Station
SUBAREA FLOW ADDITION ****
90.000
Top of street segment elevation = 358.000(Ft.)
End of street segment elevation = 346.100(Ft.)Length of street segment = 460.000(Ft.)
Height of curb above gutter flowline = 6.0(In.)width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the streetDistance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025Gutter width = 1.500(Ft.)Gutter hike from flowline = 1.500(ln.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street = 3.898(CFS)
Depth of flow = 0.298(Ft.), Average velocity = 3.551(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 10.132(Ft.)Flow velocity = 3.55(Ft/s)
Travel time = 2.16 min. TC = 8.88 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000[MEDIUM DENSITY RESIDENTIAL ]
Page 3 of 14
10 yr Developed Flows
(7.3 DU/A or Less )
Impervious value, Ai = 0.400
Sub-Area C Value = 0.570
Rainfall intensity = 3.455(In/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.591 CA = 1.429
subarea runoff = 2.163(CFS) for 1.330 (AC.)
Total runoff = 4.939(CFS) Total area = 2.420(Ac.)
street flow at end of street = 4.939(CFS)
Half street flow at end of street = 4.939(CFS)
Depth 9f flow = 0.318(Ft.), Average velocity = 3.758(Ft/s)
Flow width (from curb towards crown)= 11.149(Ft.)
Process from Point/Station 40.000 to Point/Station 90.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main Stream number: 1 in normal stream number 1
stream flow area = 2.420(Ac.)Runoff from this stream = 4.939(CFS)
Time of concentration = 8.88 min.
Rainfall intensity = 3.455(ln/Hr)
Process from Point/station 50.000 to point/station 60.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )impervious value, Ai = 0.400
sub-Area C value = 0.570
initial subarea total flow distance = 180.000(Ft.)
Highest elevation = 3 54. 700 (Ft.)
Lowest elevation = 352.300(Ft.)
Elevation difference = 2.400(Ft.) Slope = 1.333 %Top of initial Area Slope adjusted by User to 1.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 65.00 (Ft)for the top area slope value of 1.00 %, in a development type of
7.3 DU/A or Less
In Accordance With Figure 3-3
initial Area Time of concentration = 7.69 minutes
TC = [1.8*(l.l-C)*distance(Ft.)A.5)/(% slopeA(l/3)]TC = [1.8*(1.1-0.5700)*( 65.000A.5)/( 1.000A(l/3)]= 7.69
Rainfall intensity (I) = 3.792(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is c = 0.570
Subarea runoff = 0.540(CFS)
Total initial stream area = 0.250(Ac.)
Process from Point/station 60.000 to Point/Station 70.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 352.300(Ft.)
End of street segment elevation = 352.000(Ft.)Length of street segment = 180.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)Slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020
street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Page 4 of 14
10 yr Developed Flows
Gutter hike from flowline = 1.500(ln.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street = 0.862(CFS)
Depth of flow = 0.287(Ft.), Average velocity = 0.872(Ft/s)
Streetflow hydraulics at midpoint of street travel:Half street flow width = 9. 578 (Ft.)Flow vel9city = 0.87(Ft/s)
Travel time = 3,44 min. TC = 11.13 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
sub-Area C value = 0.570
Rainfall intensity = 2.988(In/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.370
Subarea runoff = 0.567(CFS) for 0.400(Ac.)
Total runoff = 1.107(CFS) Total area = 0.650 (AC.)street flow at end of street = 1.107(CFS)Half street flow at end of street = 1.107(CFS)
Depth of flow = 0.307(Ft.), Average velocity = 0.926(Ft/s)
Flow width (from curb towards crown)= 10. 604 (Ft.)
process from Point/Station 70.000 to Point/Station 80.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 352.000(Ft.)
End of street segment elevation = 350.000(Ft.)
Length of street segment = 178.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
Width of half street (curb to crown) = 18.000(Ft.)Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500 (in.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street = 1.809(CFS)Depth of flow = 0.270(Ft.), Average velocity = 2.154(Ft/s)Streetflow hydraulics at midpoint of street travel:Half street flow width = 8.768(Ft.)Flow velocity = 2.15(Ft/s)Travel time = 1.38 min. TC = 12.51 min.
Adding area flow to streetDecimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C value = 0.570
Rainfall intensity = 2.771(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.872Subarea runoff = 1.310(CFS) for 0.880(Ac.)
Total runoff = 2.417(CFS) Total area = 1.5 30 (Ac.)Street flow at end of street = 2.417(CFS)
Half street flow at end of street = 2.417(CFS)
Page 5 of 14
10 yr Developed Flows
Depth 9f flow = 0.293(Ft.), Average velocity = 2.306(Ft/s)Flow width (from curb towards crown)= 9.882(Ft.)
H-++++++++++++
Process from Point/station 80.000 to Point/Station 90.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 350.000(Ft.)
End of street segment elevation = 346.100(Ft.)
Length of street segment = 412.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)Gutter hike from flowline = 1.500(In.)Manning's N in gutter =. 0.0150Manning's N from gutter to grade break = 0.0150Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street =Depth of flow = 0.322(Ft.), Average velocity =Streetflow hydraulics at midpoint or street travel:Halfstreet flow width = 11.347(Ft.)Flow velocity = 2.30(Ft/s)Travel time = 2.99 min. TC = 15.50 min.Adding area flow to streetDecimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )Impervious value, Ai = 0.400
Sub-Area C Value = 0.570
Rainfall intensity = 2.413(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 1.556
Subarea runoff = 1.339(CFS) for 1.200(Ac.)Total runoff = 3.755(CFS) Total area = 2.730(Ac.)
Street flow at end of street = 3.755(CFS)Half street flow at end of street = 3.755(CFS)Depth 9f flow = 0.339(Ft.), Average velocity = 2.402(Ft/s)
Flow width (from curb towards crown)= 12.214(Ft.)
3.122(CFS)2.297(Ft/s)
Process from Point/Station 80.000 to Point/Station 90.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main Stream number: 1 in normal stream number 2Stream flow area = 2.730(AC.)Runoff from this stream = 3.755(CFS)Time of concentration = 15.50 min.Rainfall intensity = 2.413(In/Hr)Summary of stream data:
Stream
No.
Flow rate
(CFS)
TC
(mi n)
Rainfall intensity
(In/Hr)
1
2
Qmax(l)
Qmax(2)
4.939
3.755
~ 1.0001.000
0.698 *
8.88
15.50
1.000
0.573
1.000 *
3.455
2.413
4.939) +
3.755) +
4.939) +
7.092
Page 6 of 14
10 yr Developed Flows
1.000 * 1.000 * 3.755) + = 7.205
Total of 2 streams to confluence:
Flow rates before confluence point:
4.939 3.755
Maximum flow rates at confluence using above data:
7.092 7.205
Area of streams before confluence:2.420 2.730
Results of confluence:
T9tal flow rate = 7.205(CFS)
Time of concentration = 15.497 min.
Effective stream area after confluence = 5.150(Ac.)
Process from Point/Station 90.000 to Point/Station 92.000
**** IMPROVED CHANNEL TRAVEL TIME ****
Upstream point elevation = 346.100(Ft.)Downstream point elevation = 343. 500 (Ft.)channel length thru subarea = 80.000(Ft.)Channel base width = 4. 000 (Ft.)Slope or 'z' of left channel bank = 3.000
Slope or 'z' of right channel bank = 3.000
Estimated mean flow rate at midpoint of channel = 7.295(CFS)
Manning's 'N1 = 0.025
Maximum depth of channel = 2.000(Ft.)
Flow(q) thru subarea = 7.295(CFS)
Depth of flow = 0.328 (Ft.), Average velocity = 4.465(Ft/s)
channel fl9w top width = 5. 967 (Ft.)Flow Vel9city = 4.47(Ft/s)
Travel time = 0.30 min.
Time of concentration = 15.80 min.
Critical depth = 0.422 (Ft.)
Adding area flow t9 channel
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(4.3 DU/A or Less )
impervious value, Ai = 0.300
Sub-Area C value = 0.520
Rainfall intensity = 2.384(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.578 CA = 3.074
Subarea runoff = 0.123(CFS) for 0.170(Ac.)Total runoff = 7.327(CFS) Total area = 5.320(Ac.)
Depth of flow = 0.329(Ft.), Average velocity = 4.472(Ft/s)Critical depth = 0.422 (Ft.)
process from Point/Station 92.000 to Point/Station 190.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
upstream point/station elevation = 335.500(Ft.)Downstream point/station elevation = 329.100(Ft.)
Pipe length = 35.00(Ft.) Manning's N = 0.014
NO. of pipes = 1 Required pipe flow = 7.327(CFS)
Given pipe size = 18.00(ln.)
Calculated individual pipe flow = 7.327(CFS)
Normal flow depth in pipe = 5.11(ln.)Flow top width inside pipe = 16. 2 3 (in.)
critical Depth = 12. 59 (in.)
pipe flow velocity = 17.76(Ft/s)
Travel time through pipe = 0.03 min.
Time of concentration (TC) = 15.83 min.
Page 7 of 14
10 yr Developed Flows
Process from Point/Station 92.000 to Point/Station 190.000
**** CONFLUENCE OF MAIN STREAMS ****
The f 9! lowing data inside Main stream is listed:
in Main stream number: 1
Stream flow area = 5.320(Ac.)
Runoff from this stream = 7.327(CFS)
Time of concentration = 15.83 mi n.
Rainfall intensity = 2.381(ln/Hr)
Program is now starting with Main stream No. 2
Process from Point/Station 100.000 to Point/Station 110.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400Sub-Area C value = 0.570initial subarea total flow distance = 100.000(Ft.)Highest elevation = 355.200(Ft.)Lowest elevation = 353.000(Ft.)Elevation difference = 2.200(Ft.) slope = 2.200 %Top of Initial Area Slope adjusted by user to 0.500 %Bottom of initial Area Slope adjusted by User to 0.500 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:The maximum overland flow distance is 50.00 (Ft)for the top area slope value of 0.50 %, in a development type of7.3 DU/A or Lessin Accordance with Figure 3-3
initial Area Time of concentration = 8.50 minutesTC = [1.8*(l.l-c)*distance(Ft.)A.5)/(% slopeA(l/3)]TC = [1.8*(1.1-0.5700)*( 50.000A.5)/C 0.500A(l/3)]= 8.50The initial area total distance of 100.00 (Ft.) entered leaves aremaining distance of 50.00 (Ft.)Using Figure 3-4, the travel time for this distance is 1.22 minutes
f9r a distance of 50.00 (Ft.) and a slope of 0.50 %with an elevation difference of 0.2 5 (Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)
1.221 MinutesTt=[(11.9*0.0095A3)/( 0.25)]A.385= 1.22Total initial area Ti = 8.50 minutes from Figure 3-3 formula plus1.22 minutes from the Figure 3-4 formula = 9.72 minutesRainfall intensity (I) = 3.260(In/Hr) for a 10.0 year stormEffective runoff coefficient used for area (Q=KCIA) is C = 0.570Subarea runoff = 0.204(CFS)Total initial stream area = 0.110(Ac.)
Process from Point/Station 110.000 to Point/Station 120.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 353.000(Ft.)
End of street segment elevation = 351.500(Ft.)
Length of street segment = 151.000(Ft.)
Height of curb above gutter flowline = 6.0 (in.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope fr9m curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)
Gutter hike from flowline = 1.500 (in.)
Page 8 of 14
10 yr Developed Flows
Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 0.585(CFS)
Depth of flow = 0.204(Ft.), Average velocity = 1.596(Ft/s)
Streetflow hydraulics at midpoint of street travel:Half street flow width = 5. 437 (Ft.)Flow velocity = 1.60(Ft/s)
Travel time = 1.58 mi n. TC = 11.30 mi n.
Adding area flow to streetDecimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000Decimal fraction soil group c = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )impervious value, Ai = 0.400Sub-Area C value = 0.570Rainfall intensity = 2.959(ln/Hr) for a 10.0 year stormEffective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.296
Subarea runoff = 0.673(CFS) for 0.410(Ac.)
Total runoff = 0.877(CFS) Total area = 0.520(Ac.)
Street flow at end of street = 0.877(CFS)
Half street flow at end of street = 0.877(CFS)
Depth 9f flow = 0.227(Ft.), Average velocity = 1.740(Ft/s)
Flow width (from curb towards crown)= 6.578(Ft.)
Process from Point/Station 120.000 to Point/Station 160.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 351.500(Ft.)
End of street segment elevation = 346.200(Ft.)
Length of street segment = 485.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)Gutter hike from flowline = 1.500 (in.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.430(CFS)
Depth of flow = 0.255(Ft.), Average velocity = 2.017(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Half street flow width = 7. 985 (Ft.)
Flow velocity = 2.02(Ft/s)
Travel time = 4.01 min. TC = 15.30 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL 3
(7.3 DU/A or Less )
impervious value, Ai = 0.400Sub-Area c value = 0.570Rainfall intensity = 2.433(In/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.792
Subarea runoff = l.OSO(CFS) for 0.870(Ac.)
Total runoff = 1.928(CFS) Total area = 1.390 (AC.)Street flow at end of street = 1.928(CFS)Half street flow at end of street = 1.928(CFS)Depth 9f flow = 0.276(Ft.), Average velocity = 2.163(Ft/s)
Flow width (from curb towards crown)= 9. 05 5 (Ft.)
Page 9 of 14
10 yr Developed Flows
Process from Point/Station 120.666 to Point/Station 160.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main stream number: 2 in normal stream number 1
Stream flow area = 1.390(Ac.)Runoff from this stream = 1.928(CFS)Time of concentration = 15.30 min.Rainfall intensity = 2.433(ln/Hr)
Process from Point/Station 130.000 to Point/Station 140.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ](7.3 DU/A or Less )
impervious value, Ai = 0,400Sub-Area C Value = 0.570initial subarea total flow distance = 100. 000 (Ft.)Highest elevation = 355.600(Ft.)Lowest elevation = 353.400(Ft.)Elevation difference = 2.200(Ft.) Slope = 2.200 %Top of initial Area Slope adjusted by user to 2.000 %Bottom of Initial Area Slope adjusted by User to 2.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 80.00 (Ft)
for the top area slope value of 2.00 %, in a development type of
7.3 DU/A or Less
in Accordance with Figure 3-3initial Area Time of concentration = 6.77 minutesTC = [1.8*(l.l-c)*distance(Ft.)A.5)/(% slopeA(l/3)]TC = [1. 8* (1.1-0. 5700) *( 80.000A.5)/( 2.00QA(l/3)]= 6.77The initial area total distance of 100.00 (Ft.) entered leaves a
remaining distance of 20.00 (Ft.)using Figure 3-4, the travel time for this distance is 0.35 minutesf9r a distance of 20.00 (Ft.) and a slope of 2.00 %with an elevation difference of 0.40(Ft.) from the end of the top areaTt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)0.354 Minutes
Tt=[(11.9*0.0038A3)/( 0.40)]A.385= 0.35Total initial area Ti = 6.77 minutes from Figure 3-3 formula plus
0.35 minutes from the Figure 3-4 formula = 7.13 minutesRainfall intensity (I) = 3.983(ln/Hr) for a 10.0 year stormEffective runoff coefficient used for area (Q=KCIA) is c = 0.570subarea runoff = 0.272(CFS)Total initial stream area = 0.120 (AC.)
Process from Point/Station 140.000 to Point/Station 150.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 353.400(Ft.)
End of street segment elevation = 351.000(Ft.)
Length of street segment = 163.000(Ft.)
Height of curb above gutter flowline = 6.0 (in.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500 (in.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Page 10 of 14
10 yr Developed Flows
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.064(CFS)
Depth of flow = 0.226(Ft.), Average velocity = 2.117(Ft/s)
streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 6.566(Ft.)
Flow velocity = 2.12(Ft/s)
Travel time = 1.28 min. TC = 8.41 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area c value = 0.570
Rainfall intensity = 3.580(in/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.490
Subarea runoff = 1.482(CFS) for 0.740(AC.)
Total runoff = 1.755(CFS) Total area = 0.860(Ac.)Street flow at end of street = 1.755(CFS)
Half street flow at end of street = 1.755(CFS)
Depth 9f flow = 0.259(Ft.), Average velocity = 2.372(Ft/s)
Flow width (from curb towards crown)= 8.177(Ft.)
Process from Point/Station 150.000 to Point/Station 160.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 351.000(Ft.)
End of street segment elevation = 346.200(Ft.)
Length of street segment = 290.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020
street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500(ln.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 2.471(CFS)
Depth of flow = 0.279(Ft.), Average velocity = 2.687(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 9.210(Ft.)
Flow vel9city = 2.69(Ft/s)
Travel time = 1.80 min. TC = 10.21 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400Sub-Area C value = 0.570
Rainfall intensity = 3.159(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.992
Subarea runoff = 1.378(CFS) for 0.880(Ac.)
Total runoff = 3.133(CFS) Total area = 1.740(Ac.)
Street flow at end of street = 3.133(CFS)
Half street flow at end of street = 3.133(CFS)
Depth of flow = 0.298(Ft.), Average velocity = 2.843(Ft/s)
Flow width (from curb towards crown)= 10.152(Ft.)
Page 11 of 14
10 yr Developed Flows
Process from Point/Station 150.000 to Point/Station 160.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main Stream number: 2 in normal stream number 2
Stream flow area = 1.740(Ac.)
Runoff from this stream = 3.133(CFS)
Time of concentration = 10.21 min.Rainfall intensity = 3.159(In/Hr)Summary of stream data:
Stream
No.
Flow rate
CCFS)
TC
(min)
Rainfall intensity
(in/Hr)
12
Qmax(l)
Qmax(2)
1.928
3.133
1.000 *
0.770 *
1.000 *
1.000 *
15.30
10.21
000
000
0.667 *
1.000 *
2.433
3.159
1.928) +
3.133) +
1.928) +
3.133) +
4.340
4.419
Total of 2 streams to confluence:Flow rates before confluence point:
1.928 3.133Maximum flow rates at confluence using above data:
4.340 4.419
Area of streams before confluence:
1.390 1.740
Results of confluence:
T9tal flow rate = 4.419(CFS)
Time of concentration = 10.208 min.
Effective stream area after confluence = 3.130(Ac.)
Process from Point/station 160.000 to Point/Station 180.000
**** PIPEFLOW TRAVEL TIME (user specified size) ****
upstream point/station elevation = 334. 700 (Ft.)
Downstream point/station elevation = 331.400(Ft.)
Pipe length = 66.00(Ft.) Manning's N = 0.014
NO. of pipes = 1 Required pipe flow = 4.419(CFS)
Given pipe size = 18.00(In.)
Calculated individual pipe flow = 4.419(CFS)
Normal flow depth in pipe = 5. 50 (in.)
Flow top width inside pipe = 16. 58 (In.)
Critical Depth = 9. 67 (in.)
Pipe flow velocity = 9.67(Ft/s)
Travel time through pipe = 0.11 min.
Time of concentration (TC) = 10.32 min.
Process from Point/Station 160.000 to Point/Station 180.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main Stream number: 2 in normal stream number 1
Stream flow area = 3.130(Ac.)
Runoff from this stream = 4.419(CFS)
Time of concentration = 10.32 min.
Rainfall intensity = 3.137(ln/Hr)
Page 12 of 14
10 yr Developed Flows
Process from Point/Station 170.000 to Point/station 180.000
**** USER DEFINED FLOW INFORMATION AT A POINT ****
000
000
000
000
Decimal fraction soil group A
Decimal fraction soil group BDecimal fraction soil group C
Decimal fraction soil group D
[MEDIUM DENSITY RESIDENTIAL
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C value = 0.570
Rainfall intensity (I) =
user specified values are as follows:
TC = 13.00 min. Rain intensity =
Total area = 68.400(Ac.) Total
2.703(ln/Hr) for a 10.0 year storm
2.70(In/Hr)
runoff = 98.000CCFS)
Process from Point/Station 170.000 to Point/Station 180.000
**** PIPEFLOW TRAVEL TIME (user specified size) ****
upstream point/station elevation = 347.200(Ft.)
Downstream point/station elevation = 329.800(Ft.)
Pipe length = 535.00(Ft.) Manning's N = 0.014
NO. of pipes = 1 Required pipe flow = 98.000(CFS)
Given pipe size = 48.00(ln.)
Calculated individual pipe flow = 98.000(CFS)
Normal flow depth in pipe = 21.33(in.)
Flow top width inside pipe = 47.70(in.)
Critical Depth = 36.00(ln.)
Pipe flow velocity = 18.16(Ft/s)
Travel time through pipe = 0.49 min.
Time of concentration (TC) = 13.49 min.
Process from Point/Station 170.000 to Point/Station 180.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main stream number: 2 in normal stream number 2
stream flow area = 68.400(AC.)
Runoff from this stream = 98.000(CFS)
Time of concentration = 13.49 min.
Rainfall intensity = 2.639(ln/Hr)
Summary of stream data:
streamNO.Flow rate
(CFS)
TC(mi n)Rainfall intensity(in/Hr)
1
2Qmax(l)
4.41998.000
Qmax(2) =
000000
0.841
1.000
10.32
13.49
1.000
0.765
1.000 *
1.000 *
3.137
2.639
4.419) +98.000) +
4.419) +98.000) +
79.397
101.718
Total of 2 streams to confluence:
Flow rates before confluence point:
4.419 98.000
Maximum flow rates at confluence using above data:
79.397 101.718
Area of streams before confluence:
3.130 68.400
Results of confluence:Tptal flow rate = 101.718(CFS)Time of concentration = 13.491 min.
Effective stream area after confluence = 71.530(AC.)
Page 13 of 14
10 yr Developed Flows
Process from Point/Station 180.000 to Point/Station 190.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
upstream point/station elevation = 329. 800 (Ft.)Downstream point/station elevation = 329. 100 (Ft.)Pipe length = 74.00(Ft.) Manning's N = 0.014
NO. of pipes = 1 Required pipe flow = 101.718(CFS)Given pipe size = 48.00(ln.)Calculated individual pipe flow = 101.718(CFS)Normal flow depth in pipe = 32. 02 (in.)Flow top width inside pipe = 45.24(ln.)Critical Depth = 36.64(ln.)
Pipe flow velocity = 11.43(Ft/s)Travel time through pipe = 0.11 mi n.Time of concentration (TC) = 13.60 min.
Process from Point/Station 180.000 to Point/Station 190.000
**** CONFLUENCE OF MAIN STREAMS ****
The following data inside Main stream is listed:
In Main Stream number: 2
stream flow area = 71. 530 (AC.)
Runoff from this stream = 101.718(CFS)
Time of concentration = 13.60 min.
Rainfall intensity = 2.626(ln/Hr)
Summary of stream data:
Stream Flow rate TC Rainfall intensity
NO. CCFS) (min) (in/Hr)
1 7.327 15.83 2.381
2 101.718 13.60 2.626Qmax(l) =1.000 * 1.000 * 7.327) +
0.907 * 1.000 * 101.718) + = 99.556
Qmax(2) =
1.000 * 0.859 * 7.327) +1.000 * 1.000 * 101.718) + = 108.013
Total of 2 main streams to confluence:
Flow rates before confluence point:
7.327 101.718
Maximum flow rates at confluence using above data:99.556 108.013Area of streams before confluence:5.320 71.530
Results of confluence:
T9tal flow rate = 108.013(CFS)Time of concentration = 13.599 min.Effective stream area after confluence = 76.850(Ac.)
Process from Point/Station 190.000 to Point/Station 200.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
Upstream point/station elevation = 329. 100 (Ft.)Downstream point/station elevation = 328. 300 (Ft.)Pipe length = 79.00(Ft.) Manning's N = 0.014NO. of pipes = 1 Required pipe flow = 108.013(CFS)
Given pipe size = 48.00(ln.)Calculated individual pipe flow = 108.013(CFS)Normal flow depth in pipe = 32. 63 (in.)Flow top width inside pipe = 44.79(ln.)Critical Depth = 37. 73 (in.)
Pipe flow velocity = 11.88(Ft/s)Travel time through pipe = 0.11 min.Time of concentration (TC) = 13.71 min.End of computations, total study area = 76.850 (Ac.)
Page 14 of 14
100 yr Developed Flows
San Diego County Rational Hydrology program
CIVILCADD/CIVILDESIGN Engineering software,(c)1991-2004 Version 7.4
Rational method hydrology program based on
San Diego County Flood Control Division 2003 hydrology manual
Rational Hydrology study Date: 10/04/07
JN DRHH0030 - LA COSTA RIDGE
DAVID EVANS AND ASSOCIATES, INC.
DEVELOPED FLOWS TO EXISTING PIPE - 1/17/06, REV 10/04/07
P:\D\DRHH0030\600lNFO\EC\HYDROLOGY\DEV2
********* Hydrology Study Control information **********
Program License serial Number 4009
Rational hydrology study storm event year is 100.0
English (in-lb) input data Units used
Map data precipitation entered:
6 hour, precipitation(inches) = 2.800
24 hour precipitation(inches) = 5.125
P6/P24 = 54.6%
San Diego hydrology manual 'C' values used
+++++++++++++4
Process from Point/Station 10.000 to Point/Station 20.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ](General commercial )
Impervious value, Ai = 0.850
Sub-Area c Value = 0.820
initial subarea total flow distance = 100.000(Ft.)
Highest elevation = 388.000(Ft.)
Lowest elevation = 377.000(Ft.)
Elevation difference = 11.000(Ft.) slope = 11.000 %
Top of Initial Area Slope adjusted by user to 1.000 %
Bottom of initial Area slope adjusted by user to 1.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 60.00 (Ft)
for the top area slope value of 1.00 %, in a development type of
General commercial
In Accordance with Figure 3-3
initial Area Time of Concentration = 3.90 minutes
TC = [1.8*(l.l-c)*distance(Ft.)A.5)/(% slopeA(l/3)]
TC = [1.8*(1.1-0.8200)*( 60.000A.5)/( 1.000A(l/3)]= 3.90
The initial area total distance of 100.00 (Ft.) entered leaves a
remaining distance of 40.00 (Ft.)
using Figure 3-4, the travel time for this distance is 0.79 minutes
for a distance of 40.00 (Ft.) and a slope of 1.00 %
with an elevation difference of 0.40(Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)
0.787 Minutes
Tt=[(11.9*0.0076A3)/( 0.40)]A.385= 0.79
Total initial area Ti = 3.90 minutes from Figure 3-3 formula plus
0.79 minutes from the Figure 3-4 formula = 4.69 minutes
Rainfall intensity (I) = 7.687(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is C = 0.820
Subarea runoff = 0.441(CFS)
Total initial stream area = 0.070(Ac.)
Page 1 of 14
100 yr Developed Flows
Process from Point/Station 20.000 to Point/Station 30.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 377.000(Ft.)
End of street segment elevation = 365.000(Ft.)
Length of street segment = 190.000(Ft.)
Height of curb above gutter flow/line = 6.0(m.)
width of half street (curb to crown) = 18.000(Ft.) .
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10. 000 (Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)
Gutter hike from flowline = 1.500(In.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 0.744(CFS)
Depth of flow = 0.169(Ft.), Average velocity = 3.549(Ft/s)
streetflow hydraulics at midpoint or street travel:
Halfstreet flow width = 3.719(Ft.)
Flow velocity = 3.55(Ft/s)
Travel time = 0.89 mi n. TC = 5.58 mi n.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(General Commercial )
impervious value, Ai = 0.850
sub-Area c value = 0.820
Rainfall intensity = 6.870(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.820 CA = 0.164
Subarea runoff = 0.685(CFS) for 0.130(Ac.)
Total runoff = 1.127(CFS) Total area = 0.200 (Ac.)
Street flow at end of street = 1.127(CFS)
Half street flow at end of street = 1.127(CFS)
Depth 9f flow = 0.190(Ft.), Average velocity = 3.813(Ft/s)
Flow width (from curb towards crown)= 4.736(Ft.)
process from Point/Station 30.000 to point/station 40.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 365.000(Ft.)
End of street segment elevation = 358.000(Ft.)Length of street segment = 200.000(Ft.)Height of curb above gutter flowline = 6.0(in.)width of half street (curb to crown) = 18.000(Ft.)Distance from crown to crossfall grade break = 16.500(Ft.)Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500(ln.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.676(CFS)
Depth of flow = 0.228(Ft.), Average velocity = 3.279(Ft/s)streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 6.631(Ft.)
Flow velocity = 3.28(Ft/s)
Travel time = 1.02 mi n. TC = 6.60 min.
Page 2 of 14
100 yr Developed Flows
Adding area flow to streetDecimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
Impervious value, Ai = 0.400Sub-Area C Value = 0.570
Rainfall intensity = 6.168(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.664 CA = 0.352Subarea runoff = 1.045(CFS) for 0.330(Ac.)Total runoff = 2.172(CFS) Total area = 0.530(Ac.)Street flow at end of street = 2.172(CFS)
Half street flow at end of street = 2.172(CFS)
Depth of flow = 0.244(Ft.), Average velocity = 3.476(Ft/s)
Flow width (from curb towards crown)= 7. 439 (Ft.)
Process from Point/Station
**** SUBAREA FLOW ADDITION ****
35.000 to Point/station 40.000
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C value = 0.570
Time of concentration = 6.60 mi n.
Rainfall intensity = 6.168(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.616 CA = 0.671Subarea runoff = 1.969(CFS) for 0.560(Ac.)
Total runoff = 4.140(CFS) Total area = 1.090(Ac.)
Process from Point/Station 40.000 to Point/Station 90.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 358.000(Ft.)
End of street segment elevation = 346.100(Ft.)Length of street segment = 460.000(Ft.)Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16. 500 (Ft.)Slope from gutter to grade break (v/hz) = 0.020slope from grade break to crown (v/hz) = 0.020Street flow is on [1] side(s) of the streetDistance from curb to property line = 10.000(Ft.)Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)Gutter hike from flowline = 1.500(In.)
Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street =
Depth of flow = 0.333 (Ft.), Average velocity =
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 11.911(Ft.)
Flow vel9city = 3.91(Ft/s)
5.827(CFS)
3.911(Ft/s)
Travel time = 1.96 mi n. TC =
Adding area flow t9 street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL
8.56 min.
Page 3 of 14
100 yr Developed Flows
(7.3 DU/A or Less )Impervious value, Ai = 0.400
sub-Area c value = 0.570Rainfall intensity = 5.215(in/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area(Q=KCIA) is C = 0.591 CA = 1.429Subarea runoff = 3.314(CFS) for 1.330(Ac.)
Total runoff = 7.455(CFS) Total area = 2.420(AC.)
Street flow at end of street = 7.455(CFS)
Half street flow at end of street = 7.455(CFS)
Depth of flow = 0.358(Ft.), Average velocity = 4.152(Ft/s)
Flow width (from curb towards crown)= 13. 130 (Ft.)
Process from Point/Station 40.000 to Point/Station 90.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main stream number: 1 in normal stream number 1
Stream flow area = 2.420(Ac.)
Runoff from this stream = 7.455(CFS)
Time of concentration = • 8.56 mi n.Rainfall intensity = 5.215(ln/Hr)
Process from Point/Station 50.000 to Point/Station 60.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group c = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
Impervious value, Ai = 0.400Sub-Area C value = 0.570initial subarea total flow distance = 180.000(Ft.)
Highest elevation = 354.700(Ft.)
Lowest elevation = 352.300(Ft.)
Elevation difference = 2.400(Ft.) Slope = 1.333 %Top of initial Area Slope adjusted by User to 1.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 65.00 (Ft)
for the top area slope value of 1.00 %, in a development type of
7.3 DU/A or Less
in Accordance with Figure 3-3initial Area Time of Concentration = 7.69 minutesTC = [1.8*(l.l-c)*distance(Ft.)A.5)/(% slopeA(l/3)]
TC = [1.8*(1.1-0.5700)*( 65.000A.5)/( 1.00QA(l/3)]= 7.69Rainfall intensity (I) = 5.588(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is c = 0.570Subarea runoff = 0.796(CFS)
Total initial stream area = 0.2 50 (AC.)
Process from Point/Station 60.000 to Point/Station 70.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 352. 300 (Ft.)
End of street segment elevation = 352.000(Ft.)
Length of street segment = 180.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)Slope from curb to property line (v/hz) = 0.025Gutter width = 1.500(Ft.)
Page 4 of 14
100 yr Developed Flows
Gutter hike from flowline = 1.500 (In.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street = 1.255(CFS)
Depth of flow = 0.318 (Ft.), Average velocity = 0.954(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 11.155(Ft.)Flow ve^city = 0.95(Ft/s)
Travel time = 3.14 mi n. TC = 10.84 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ](7.3 DU/A or Less )impervious value, Ai = 0.400
Sub-Area C value = 0.570
Rainfall intensity = 4.480(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.370Subarea runoff = 0.863(CFS) for 0.400(Ac.)Total runoff = 1.660(CFS) Total area = 0.650 (AC.)street flow at end of street = 1.660(CFS)Half street flow at end of street = 1.660(CFS)Depth of flow = 0.344(Ft.), Average velocity = 1.021(Ft/s)Flow width (from curb towards crown)= 12.468(Ft.)
Process from Point/Station 70.000 to Point/Station 80.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 352.000(Ft.)
End of street segment elevation = 350. 000 (Ft.)
Length of street segment = 178.000(Ft.)
Height of curb above gutter flowline = 6.0(In.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020Slope from grade break to crown (v/hz) = 0.020Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)Gutter hike from flowline = 1.500 (in.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street == 2.684(CFS)Depth of flow = 0.301(Ft.), Average velocity = 2.365(Ft/s)Streetflow hydraulics at midpoint of street travel:Halfstreet flow width = 10. 314 (Ft.)Flow velocity = 2.36(Ft/s)Travel time = 1.25 min. TC = 12.09 min.Adding area flow to streetDecimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )impervious value, Ai = 0.400Sub-Area C Value = 0.570Rainfall intensity = 4.174(ln/Hr) for a 100.0 year stormEffective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.872
Subarea runoff = 1.980(CFS) for 0.880(Ac.)
Total runoff = 3.640(CFS) Total area = 1.5 30 (AC.)
street flow at end of street = 3.640(CFS)
Half street flow at end of street = 3.640(CFS)
Page 5 of 14
100 yr Developed Flows
Depth 9f flow = 0.328(Ft.), Average velocity = 2.544(Ft/s)
Flow width (from curb towards crown)= 11.659(Ft.)
Process from Point/Station 80.000 to Point/Station 90.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 350.000(Ft.)
End of street segment elevation = 346.100(Ft.)
Length of street segment = 412.000(Ft.)
Height of curb above gutter flowline = 6.0 (In.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)Gutter hike from flowline = 1.500 (in.)Manning's N in gutter =• 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 4.697(CFS)
Depth of flow = 0.362(Ft.), Average velocity = 2.537(Ft/s)
streetflow hydraulics at midpoint of street travel:Half street flow width = 13. 343 (Ft.)
Flow vel9city = 2.54(Ft/s)
Travel time = 2.71 mi n. TC = 14.80 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C Value = 0.570
Rainfall intensity = 3.664(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 1.556
Subarea runoff = 2.062(CFS) for 1.200(Ac.)
Total runoff = 5.702(CFS) Total area = 2.730(Ac.)
Street flow at end of street = 5.702(CFS)
Half street flow at end of street = 5.702(CFS)
Depth 9f flow = 0.383(Ft.), Average velocity = 2.660(Ft/s)
Flow width (from curb towards crown)= 14.396(Ft.)
Process from Point/Station 80.000 to Point/Station 90.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main stream number: 1 in normal stream number 2
Stream flow area = 2. 730 (AC.)
Runoff from this stream = 5.702(CFS)
Time of concentration = 14.80 min.
Rainfall intensity = 3.664(ln/Hr)Summary of stream data:
Stream Flow rate TC Rainfall intensity
NO. (CFS) (min) (In/Hr)
1 7.455 8.56 5.2152 5.702 14.80 3.664Qmax(l) =1.000 * 1.000 * 7.455) +
1.000 * 0.579 * 5.702) + = 10.753Qmax(2) =
0.703 * 1.000 * 7.455) +
Page 6 of 14
100 yr Developed Flows
1.000 * 1.000 * 5.702) + = 10.939
Total of 2 streams to confluence:
Flow rates before confluence point:
7.455 5.702Maximum flow rates at confluence using above data:
10.753 10.939
Area of streams before confluence:
2.420 2.730
Results of confluence:
T9tal flow rate = 10.939(CFS)
Time of concentration = 14.797 min.
Effective stream area after confluence = 5.150(Ac.)
Process from Point/station 90.000 to Point/station 92.000
**** IMPROVED CHANNEL TRAVEL TIME ****
Upstream point elevation = 346.100(Ft.)Downstream point elevation = 343.500(Ft.)
Channel length thru subarea = 80.000(Ft.)channel base width = 4.000(Ft.)slope or 'z1 of left channel bank = 3.000slope or 'z1 of right channel bank = 3.000Estimated mean flow rate at midpoint of channel = 11.079(CFS)Manning's 'N' =0.025Maximum depth of channel = 2.000(Ft.)Flow(q) thru subarea = 11.079(CFS)Depth of flow = 0.414(Ft.), Average velocity = 5.098(Ft/s)Channel flow top width = 6.487(Ft.)Flow ve^city = 5.10(Ft/s)Travel time = 0.26 min.Time of concentration = 15.06 min.Critical depth = 0.539(Ft.)Adding area flow to channel
Decimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(4.3 DU/A or Less )
Impervious value, Ai = 0.300
Sub-Area C Value = 0.520
Rainfall intensity = 3.623(m/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.578 CA = 3.074
Subarea runoff = 0.197(CFS) for 0.170(Ac.)
Total runoff = 11.137(CFS) Total area = 5.320(Ac.)
Depth of flow = 0.416(Ft.), Average velocity = 5.107(Ft/s)
Critical depth = 0.539(Ft.)
Process from Point/Station 92.000 to Point/Station 190.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
Upstream point/station elevation = 335. 500 (Ft.)Downstream point/station elevation = 329. 100 (Ft.)Pipe length = 35.00(Ft.) Manning's N = 0.014No. of pipes = 1 Required pipe flow = 11.137(CFS)
Given pipe size = 18. 00 (In.)calculated individual pipe flow = 11.137(CFS)Normal flow depth in pipe = 6. 3 5 (In.)Flow top width inside pipe = 17.20(ln.)
Critical Depth = 15.31(ln.)Pipe flow velocity = 19.98(Ft/s)Travel time through pipe = 0.03 min.Time of concentration (TC) = 15.09 min.
Page 7 of 14
100 yr Developed Flows
Process from Point/Station 92.000 to Point/Station 190.000
**** CONFLUENCE OF MAIN STREAMS ****
The following data inside Main stream is listed:
in Main stream number: 1
Stream flow area = 5.320(Ac.)
Runoff from this stream = 11.137(CFS)
Time of concentration = 15.09 mi n.
Rainfall intensity = 3.618(In/Hr)
Program is now starting with Main Stream No. 2
Process from Point/station 100.000 to Point/Station 110.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C Value = 0.570
initial subarea total flow distance = 100. 000 (Ft.)
Highest elevation = 355.200(Ft.)
Lowest elevation = 353.000(Ft.)
Elevation difference = 2.200(Ft.) Slope = 2.200 %
Top of initial Area Slope adjusted by user to 0.500 %
Bottom of Initial Area Slope adjusted by user to 0.500 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 50.00 (Ft)
for the top area slope value of 0.50 %, in a development type of
7.3 DU/A or Lessin Accordance with Figure 3-3
Initial Area Time of concentration = 8.50 minutes
TC = [1.8*(l.l-C)*distance(Ft.)A.5)/(% slopeA(l/3)]
TC = [1.8*(1.1-0.5700)*( 50.000A.5)/( 0. 50QA(l/3)]= 8.50
The initial area total distance of 100.00 (Ft.) entered leaves a
remaining distance of 50.00 (Ft.)
Using Figure 3-4, the travel time for this distance is 1.22 minutes
for a distance of 50.00 (Ft.) and a slope of 0.50 %
with an elevation difference of 0.25(Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A. 385 *60(min/hr)
1.221 Minutes
Tt=[(11.9*0.0095A3)/( 0.25)]A.385= 1.22
Total initial area Ti = 8.50 minutes from Figure 3-3 formula plus
1.22 minutes from the Figure 3-4 formula = 9.72 minutes
Rainfall intensity (I) = 4.805(ln/Hr) for a 100.0 year stormEffective runoff coefficient used for area (Q=KCIA) is c = 0.570
Subarea runoff = 0.301(CFS)
Total initial stream area = 0.110 (AC.)
Process from Point/Station 110.000 to Point/Station 120.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 353.000(Ft.)
End of street segment elevation = 351.500(Ft.)
Length of street segment = 151.000(Ft.)
Height of curb above gutter flowline = 6.0(In.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500 (In.)
Page 8 of 14
100 yr Developed Flows
Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150Manning's N from grade break to crown = 0.0150Estimated mean flow rate at midpoint of street = 0.832(CFS)Depth of flow = 0.223(Ft.), Average velocity = 1.720(Ft/s)streetflow hydraulics at midpoint of street travel:Halfstreet flow width = 6.423(Ft.)Flow velocity = 1.72(Ft/s)Travel time = 1.46 min. TC = 11.18 min.Adding area flow t9 streetDecimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
Impervious value, Ai = 0.400
Sub-Area C Value = 0.570
Rainfall intensity = 4.389(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.296Subarea runoff = l.OOO(CFS) for 0.410(AC.)
Total runoff = 1.301(CFS) Total area = 0.520(AC.)Street flow at end of street = 1.301(CFS)Half street flow at end of street = 1.301(CFS)Depth of flow = 0.252(Ft.), Average velocity = 1.903(Ft/s)Flow width (from curb towards crown)= 7.827(Ft.)
+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++
Process from Point/station 120.000 to Point/Station 160.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 351.500(Ft.)
End of street segment elevation = 346.200(Ft.)
Length of street segment = 485.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)Slope from curb to property line (v/hz) = 0.025Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500(in.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 2.138(CFS)
Depth of flow = 0.284(Ft.), Average velocity = 2.216(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 9.452(Ft.)
Flow vel9city = 2.22(Ft/s)
Travel time = 3.65 min. TC = 14.83 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
Impervious value, Ai = 0.400
Sub-Area C Value = 0.570
Rainfall intensity = 3.659(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.792
Subarea runoff = 1.598(CFS) for 0.870(Ac.)
Total runoff = 2.899(CFS) Total area = 1.390(AC.)
Street flow at end of street = 2.899(CFS)
Half street flow at end of street = 2.899(CFS)
Depth of flow = 0.309(Ft.), Average velocity = 2.383(Ft/s)
Flow width (from curb towards crown)= 10.701(Ft.)
Page 9 of 14
100 yr Developed Flows
Process from Point/Station 120.000 to Point/Station 160.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main stream number: 2 in normal stream number 1
Stream flow area = 1.390(AC.)
Runoff from this stream = 2.899(CFS)
Time of concentration = 14.83 mi n.
Rainfall intensity = 3.659(ln/Hr)
Process from Point/Station 130.000 to Point/Station 140.000
**** INITIAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DLJ/A or Less )
Impervious value, Ai = 0.400
Sub-Area C value = 0.570
initial subarea total flow distance = 100. 000 (Ft.)
Highest elevation = 355.600(Ft.)
Lowest elevation = 353.400(Ft.)
Elevation difference = 2.200(Ft.) Slope = 2.200 %
Top of initial Area Slope adjusted by user to 2.000 %
Bottom of initial Area Slope adjusted by User to 2.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 80.00 (Ft)
for the top area slope value of 2.00 %, in a development type of
7.3 DU/A or Less
in Accordance with Figure 3-3
Initial Area Time of concentration = 6.77 minutes
TC = [1.8*(l.l-C)*distance(Ft.)A.5)/(% slopeA(l/3)]
TC = [1.8*(1.1-0.5700)*( 80.000A.5)/( 2.000A(l/3)]= 6.77
The initial area total distance of 100.00 (Ft.) entered leaves a
remaining distance of 20.00 (Ft.)
Using Figure 3-4, the travel time for this distance is 0.35 minutes
f9r a distance of 20.00 (Ft.) and a slope of 2.00 %
with an elevation difference of 0.40(Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)
0.354 Minutes
Tt=[(11.9*0.0038A3)/( 0.40)]A.385= 0.35
Total initial area Ti = 6.77 minutes from Figure 3-3 formula plus
0.35 minutes from the Figure 3-4 formula = 7.13 minutes
Rainfall intensity (I) = 5.870(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is c = 0.570Subarea runoff = 0.402(CFS)Total initial stream area = 0.120 (AC.)
Process from Point/Station 140.000 to Point/Station 150.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 353.400(Ft.)
End of street segment elevation = 351.000(Ft.)Length of street segment = 163.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)Width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500(in.)
Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150
Page 10 of 14
100 yr Developed Flows
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.539(CFS)
Depth of flow = 0.250(Ft.), Average velocity = 2.301(Ft/s)
streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 7.730(Ft.)
Flow velocity = 2.30(Ft/s)
Travel time = 1.18 min. TC = 8.31 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
Impervious value, Ai = 0.400
Sub-Area c value = 0.570
Rainfall intensity = 5.317(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.490
Subarea runoff = 2.205(CFS) for 0.740(Ac.)
Total runoff = 2.607(CFS) Total area = 0.860(Ac.)
street flow at end of street = 2.607(CFS)
Half street flow at end of street = 2.607(CFS)
Depth 9f flow = 0.288(Ft.), Average velocity = 2.603(Ft/s)Flow width (from curb towards crown)= 9.645(Ft.)
Process from Point/Station 150.000 to Point/Station 160.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 351.000(Ft.)
End of street segment elevation = 346.200(Ft.)Length of street segment = 290.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)Gutter hike from flowline = 1.500(in.)Manning's N in gutter = 0.0150Manning's N from gutter to grade break = 0.0150Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 3.689(CFS)
Depth of flow = 0.312(Ft.), Average velocity = 2.957(Ft/s)
Streetflow hydraulics at midpoint of street travel:Halfstreet flow width = 10.846(Ft.)
Flow velocity = 2.96(Ft/s)Travel time = 1.63 min. TC = 9.94 min.
Adding area flow t9 streetDecimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C Value = 0.570
Rainfall intensity = 4.736(In/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.570 CA = 0.992
Subarea runoff = 2.090(CFS) for 0.880(Ac.)
Total runoff = 4.697(CFS) Total area = 1.740(Ac.)Street flow at end of street = 4.697(CFS)
Half street flow at end of street = 4.697(CFS)
Depth 9f flow = 0.334(Ft.), Average velocity = 3.134(Ft/s)
Flow width (from curb towards crown)= 11.947(Ft.)
Page 11 of 14
100 yr Developed Flows
Process from Point/station 150.000 to Point/Station 160.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main stream number: 2 in normal stream number 2
Stream flow area = 1.740(Ac.)
Runoff from this stream = 4.697(CFS)
Time of C9ncentration = 9.94 min.Rainfall intensity = 4.736(ln/Hr)
Summary of stream data:
Stream
No.
Flow rate
(CFS)
TC
(min)
Rainfall intensity
(in/Hr)
1
2
Qmax(l)
Qmax(2)
2.899
4.697
" 1.000
0.773
14.83
9.94
1.000 *
1.000 *
000
000
0.670
1.000
3.659
4.736
2.899) +
4.697) +
2.899) +
4.697) +
6.528
6.640
Total of 2 streams to confluence:
Flow rates before confluence point:
2.899 4.697
Maximum flow rates at confluence using above data:
6.528 6.640Area of streams before confluence:
1.390 1.740
Results of confluence:
T9tal flow rate = 6.640(CFS)
Time of concentration = 9.941 min.Effective stream area after confluence =3.130CAC.)
Process from Point/Station 160.000 to Point/Station 180.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
Upstream point/station elevation = 334.700(Ft.)
Downstream point/station elevation = 331.400(Ft.)Pipe length = 66.00(Ft.) Manning's N = 0.014No. of pipes = 1 Required pipe flow = 6. 640 (CFS)Given pipe size = 18.00(In.)Calculated individual pipe flow = 6. 640 (CFS)Normal flow depth in pipe = 6.81(ln.)Flow top width inside pipe = 17.46(ln.)
Critical Depth = 11. 97 (in.)Pipe flow velocity = 10.83(Ft/s)Travel time through pipe = 0.10 min.Time of concentration (TC) = 10.04 min.
Process from Point/station 160.000 to point/station 180.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main Stream number: 2 in normal stream number 1Stream flow area = 3. 130 (Ac.)Runoff from this stream = 6.640(CFS)Time of concentration = 10.04 min.Rainfall intensity = 4.705(ln/Hr)
Page 12 of 14
100 yr Developed Flows
Process from Point/station 170.000 to Point/station 180.000
**** USER DEFINED FLOW INFORMATION AT A POINT ****
Decimal fraction soil group A = 0.000Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000Decimal fraction soil group D = 1.000
[MEDIUM DENSITY RESIDENTIAL ]
(7.3 DU/A or Less )
impervious value, Ai = 0.400
Sub-Area C value = 0.570Rainfall intensity (I) = 3.983(ln/Hr) for a 100.0 year stormUser specified values are as follows:TC = 13.00 min. Rain intensity = 3.98(ln/Hr)
Total area = 68.400(Ac.) Total runoff = 154.000(CFS)
Process from Point/Station 170.000 to Point/station 180.000**** 'PIPEFLOW TRAVEL TIME (user specified size) ****
Upstream point/station elevation = 347. 200 (Ft.)Downstream point/station elevation = 329.800(Ft.)Pipe length = 535.00(Ft.) Manning's N = 0.014No. of pipes = 1 Required pipe flow = 154.000(CFS)Given pipe size = 48. 00 (in.)Calculated individual pipe flow = 154.000(CFS)Normal flow depth in pipe = 27.91(ln.)Flow top width inside pipe = 47.36(ln.)
Critical Depth = 43.52(ln.)Pipe flow velocity = 20.31(Ft/s)Travel time through pipe = 0.44 min.Time of concentration (TC) = 13.44 min.
Process from Point/Station 170.000 to Point/station 180.000
**** CONFLUENCE OF MINOR STREAMS ****
Along Main Stream number: 2 in normal stream number 2
Stream flow area = 68.400(AC.)
Runoff from this stream = 154.000(CFS)
Time of concentration = 13.44 min.
Rainfall intensity = 3.899(ln/Hr)
Summary of stream data:
Stream Flow rate TC Rainfall intensity
No. (CFS) (min) (In/Hr)
1 6.640 10.04 4.705
2 154.000 13.44 3.899
Qmax(l) =
1.000 * 1.000 * 6.640) +
1.000 * 0.747 * 154.000) + = 121.724
Qmax(2) =
0.829 * 1.000 * 6.640) +
1.000 * 1.000 * 154.000) + = 159.503
Total of 2 streams to confluence:
Flow rates before confluence point:
6.640 154.000
Maximum flow rates at confluence using above data:
121.724 159.503
Area of streams before confluence:
3.130 68.400
Results of confluence:
T9tal flow rate = 159.503(CFS)
Time of concentration = 13.439 min.
Effective stream area after confluence = 71.530(AC.)
Page 13 of 14
100 yr Developed Flows
Process from Point/Station 180.000 to Point/Station 190.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
upstream point/station elevation = 329.800(Ft.)Downstream point/station elevation = 329.100(Ft.)Pipe length = 74.00(Ft.) Manning's N = 0.014No. of pipes = 1 Required pipe flow = 159.503(CFS)Given pipe size = 48.00(ln.)
NOTE: Normal flow is pressure flow in user selected pipe size.The approximate hydraulic grade line above the pipe invert is4.110(Ft.) at the headworks or inlet of the pipe(s)Pipe friction loss = 1.058 (Ft.)Minor friction loss = 3.753(Ft.) K-factor = 1.50Pipe flow velocity = 12.69(Ft/s)
Travel time through pipe = 0.10 mi n.Time of concentration (TC) = 13.54 mi n.
Process from Point/station 180.000 to Point/station 190.000
**** CONFLUENCE OF MAIN STREAMS ****
The f9l lowing data inside Main stream is listed:
in Main Stream number: 2Stream flow area = 71.530(Ac.)
Runoff from this stream = 159.503(CFS)Time of concentration = 13.54 min.
Rainfall intensity = 3.881(ln/Hr)
Summary of stream data:
Stream Flow rate TC Rainfall Intensity
No. CCFS) (min) (in/Hr)
1 11.137 15.09 3.618
2 159.503 13.54 3.881
Qmax(l) =
1.000 * 1.000 * 11.137) +0.932 * 1.000 * 159.503) + = 159.858
Qmax(2) =1.000 * 0.897 * 11.137) +1.000 * 1.000 * 159.503) + = 169.494
Total of 2 main streams to confluence:
Flow rates before confluence point:
11.137 159.503
Maximum flow rates at confluence using above data:
159.858 169.494Area of streams before confluence:
5.320 71.530Results of confluence:Total flow rate = 169.494(CFS)Time of concentration = 13.536 min.Effective stream area after confluence = 76.850(Ac.)
Process from Point/Station 190.000 to Point/Station 200.000**** PIPEFLOW TRAVEL TIME (user specified size) ****
Upstream point/station elevation = 329.100(Ft.)Downstream point/station elevation = 328.300(Ft.)
Pipe length = 79.00(Ft.) Manning's N = 0.014NO. of pipes = 1 Required pipe flow = 169.494(CFS)Given pipe size = 48.00(In.)
NOTE: Normal flow is pressure flow in user selected pipe size.The approximate hydraulic grade line above the pipe invert is4.713(Ft.) at the headworks or inlet of the pipe(s)Pipe friction loss = 1.275 (Ft.)Minor friction loss = 4.237(Ft.) K-factor = 1.50
Pipe flow velocity = 13.49(Ft/s)Travel time through pipe = 0.10 min.Time of concentration (TC) = 13.63 min.End of computations, total study area = 76.850 (Ac.)
Page 14 of 14
10 yr Flows to Exist CB - Corintia St.
San Diego County Rational Hydrology Program
CIVILCADD/CIVILDESIGN Engineering Software, (c) 1991-2004 Version 7.4
Rational method hydrology program based on
San Diego county Flood Control Division 2003 hydrology manual
Rational Hydrology study Date: 10/04/07
3N DRHH0030 - LA COSTA RIDGE
DAVID EVANS AND ASSOCIATES, INC.
FLOWS TO EXISTING CB ON CORINTIA - 1/30/07, REV. 10/04/07
P : \D\DRHH0030\600lNFO\EC\HYDROLOGY\DEVCBSTl
*********Hydrology Study Control information **********
Program License serial Number 4009
Rational hydrology study storm event year is
English (in-lb) input data units used
Map data precipitation entered:
6 hour, precipitation (inches) = 1.900
24 hour precipitation(inches) = 3.250
P6/P24 = 58.5%
San Diego hydrology manual 'c1 values used
10.0
Process from Point/Station 320.000 to Point/Station 330.000
**** jNrriAL AREA EVALUATION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(General Commercial )impervious value, Ai = 0.850
Sub-Area C value = 0.820
Initial subarea total flow distance = 180.000(Ft.)
Highest elevation = 363. 000 (Ft.)
Lowest elevation = 360.800(Ft.)
Elevation difference = 2.200(Ft.) Slope = 1.222 %
Top of initial Area Slope adjusted by user to 1.000 %
Bottom of Initial Area Slope adjusted by User to 1.000 %INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 60.00 (Ft)
for the top area slope value of 1.00 %, in a development type of
General Commercial
in Accordance with Figure 3-3
initial Area Time of Concentration = 3.90 minutes
TC = [1.8*(l.l-c)*distance(Ft.)A.5)/(% slopeA(l/3)]
TC = [1. 8* (1.1-0. 8200) *( 60.000A.5)/( 1.000A(l/3)]= 3.90
The initial area total distance of 180.00 (Ft.) entered leaves a
remaining distance of 120.00 (Ft.)
Using Figure 3-4, the travel time for this distance is 1.83 minutes
f9r a distance of 120.00 (Ft.) and a slope of 1.00 %
with an elevation difference of 1.20(Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)
1.835 Minutes
Tt=[(11.9*0.0227A3)/( 1.20)]A.385= 1.83
Total initial area Ti = 3.90 minutes from Figure 3-3 formula plus
1.83 minutes from the Figure 3-4 formula = 5.74 minutes
Rainfall intensity (I) = 4.580(In/Hr) for a 10.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is c = 0.820Subarea runoff = 0.601(CFS)
Total initial stream area = 0.160 (AC.)
Page 1 of3
10 yr Flows to Exist CB - Corintia St.
+++++++++++4
Process from Point/Station 330.000 to Point/Station 340.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 360.800(Ft.)
End of street segment elevation = 359.500(Ft.)
Length of street segment = 170.000(Ft.)
Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)Slope from gutter to grade break (v/hz) = 0.020Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500 (Ft.)Gutter hike from flowline = 1.500 (in.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = O.SOl(CFS)
Depth of flow = 0.229(Ft.), Average velocity = 1.540(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 6.698(Ft.)
Flow vel9city = 1.54(Ft/s)
Travel time = 1.84 mi n. TC = 7.58 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(General commercial )
Impervious value, Ai = 0.850
Sub-Area c value = 0.820
Rainfall intensity = 3.828(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.820 CA = 0.238
Subarea runoff = 0.309(CFS) for 0.130(Ac.)
Total runoff = 0.910(CFS) Total area = 0.290(Ac.)
Street flow at end of street = 0.910(CFS)
Half street flow at end of street = 0.910(CFS)
Depth 9f flow = 0.237(Ft.), Average velocity = 1.585(Ft/s)
Flow width (from curb towards crown)= 7.092(Ft.)
Process from point/station 340.000 to Point/Station 350.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 359.500(Ft.)
End of street segment elevation = 347.000(Ft.)
Length of street segment = 421.250(Ft.)
Height of curb above gutter flowline = 6.0(in.)
Width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
Slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)Slope from curb to property line (v/hz) = 0.020
Gutter width = 1.500 (Ft.)
Gutter hike from flowline = 1.500 (in.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.367(CFS)
Depth of flow = 0.220(Ft.), Average velocity = 2.940(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 6.274(Ft.)
Page 2 of 3
10 yr Flows to Exist CB - Corintia St.
TC =
0.000
0.000
.000
.000
0.
1.
9.97 min.
]
Flow ve^city = 2.94(Ft/s)Travel time = 2.39 mi n.
Adding area flow to street
Decimal fraction soil group A
Decimal fraction soil group B
Decimal fraction soil group c =
Decimal fraction soil group D =[COMMERCIAL area type
(Neighborhod commercial )
Impervious value, Ai = 0.800
Sub-Area C Value = 0.790
Rainfall intensity = 3.208(ln/Hr) for a 10.0 year stormEffective runoff coefficient used for total area(Q=KCIA) is C = 0.803 CA = 0.538Subarea runoff = 0.816(CFS) for 0.380(Ac.)
Total runoff = 1.726(CFS) Total area = 0.670(Ac.)street flow at end of street = 1.726(CFS)
Half street flow at end of street = 1.726(CFS)
Depth of flow = 0.234(Ft.), Average velocity = 3.096(Ft/s)
Flow width (from curb towards crown)= 6.973(Ft.)
Process from Point/Station 345.000 to Point/Station 350.000
**** SUBAREA FLOW ADDITION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(Neighborhod commercial )
impervious value, Ai = 0.800
Sub-Area C value = 0.790
Time of C9ncentration = 9.97 min.
Rainfall intensity = 3.208(ln/Hr) for a 10.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.797 CA = 1.044Subarea runoff = 1.622(CFS) for 0.640 (AC.)Total runoff = 3.348(CFS) Total area = 1.310 (Ac.)
End of computations, total study area = 1.310 (AC.)
Page 3 of3
100 yr Flows to Exist CB - Corintia St.
san Diego County Rational Hydrology Program
CIVILCADD/CIVILDESIGN Engineering software,(c)1991-2004 version 7.4
Rational method hydrology program based onSan Diego county Flood Control Division 2003 hydrology manual
Rational Hydrology Study Date: 10/04/07
JN DRHH0030 - LA COSTA RIDGE
DAVID EVANS AND ASSOCIATES, INC.
FLOWS TO EXISTING CB ON CORINTIA - 1/30/07, REV. 10/04/07
P:\D\DRHH0030\600lNFO\EC\HYDROLOGY\DEVCBSTl
*********Hydrology Study Control information **********
Program License Serial Number 4009
Rational hydrology study storm event year is
English (in-lb) input data Units used
Map data precipitation entered:
6 hour, precipitation(inches) = 2.800
24 hour precipitation(inches) = 5.125
P6/P24 = 54.6%
san Diego hydrology manual 'c' values used
100.0
++++++++++++++++++++++++++HProcess from point/station
**** INITIAL AREA EVALUATION
320.000 to Point/Station
****
330.000
= 180.000(Ft.)
1.222
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(General commercial )
Impervious value, Ai = 0.850
sub-Area c value = 0.820
initial subarea total flow distance
Highest elevation = 363.000(Ft.)
Lowest elevation = 360.800(Ft.)
Elevation difference = 2.200(Ft.) slope =
Top of initial Area slope adjusted by user to 1.000 %
Bottom of initial Area slope adjusted by user to 1.000 %
INITIAL AREA TIME OF CONCENTRATION CALCULATIONS:
The maximum overland flow distance is 60.00 (Ft)
for the top area slope value of 1.00 %, in a development type of
General Commercial
in Accordance with Figure 3-3
initial Area Time of Concentration = 3.90 minutes
TC = [1.8*(l.l-c)*distance(Ft.)A.5)/(% slopeA(i/3)]
TC = [1.8*(1.1-0.8200)*( 60.000A.5)/( 1.000A(l/3)]= 3.90
The initial area total distance of 180.00 (Ft.) entered leaves a
remaining distance of 120.00 (Ft.)
using Figure 3-4, the travel time for this distance is 1.83 minutes
for a distance of 120.00 (Ft.) and a slope of 1.00 %
with an elevation difference of 1.20(Ft.) from the end of the top area
Tt = [11.9*length(Mi)A3)/(elevation change(Ft.))]A.385 *60(min/hr)
1.835 Minutes
Tt=[(11.9*0.0227A3)/( 1.20)]A.385= 1.83
Total initial area Ti = 3.90 minutes from Figure 3-3 formula plus
1.83 minutes from the Figure 3-4 formula = 5.74 minutes
Rainfall intensity (I) = 6.750(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for area (Q=KCIA) is C = 0.820
Subarea runoff = 0.886(CFS)
Total initial stream area = 0.160(AC.)
Page 1 of 3
100 yr Flows to Exist CB - Corintia St.
Process from Point/Station 330.000 to Point/Station 340.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 360.800(Ft.)
End of street segment elevation = 359.500(Ft.)Length of street segment = 170.000(Ft.)Height of curb above gutter flowline = 6.0(ln.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020street flow is on [1] side(s) of the streetDistance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.025
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500(In.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 1.154(CFS)
Depth of flow = 0.252(Ft.), Average velocity = 1.673(Ft/s)
Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 7.862(Ft.)Flow vel9city = 1.67(Ft/s)Travel time = 1.69 min. TC = 7.43 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000[COMMERCIAL area type ]
(General commercial )
Impervious value, Ai = 0.850
Sub-Area c Value = 0.820
Rainfall intensity = 5.713(In/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.820 CA = 0.238Subarea runoff = 0.473(CFS) for 0.130(Ac.)
Total runoff = 1.359(CFS) Total area = 0.290(Ac.)
street flow at end of street = 1.359(CFS)
Half street flow at end of street = 1.359(CFS)
Depth of flow = 0.264(Ft.), Average velocity = 1.738(Ft/s)
Flow width (from curb towards crown)= 8.429(Ft.)
Process from Point/Station 340.000 to Point/Station 350.000
**** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION ****
Top of street segment elevation = 359.500(Ft.)
End of street segment elevation = 347.000(Ft.)
Length of street segment = 421.250(Ft.)
Height of curb above gutter flowline = 6.0(in.)
width of half street (curb to crown) = 18.000(Ft.)
Distance from crown to crossfall grade break = 16.500(Ft.)
Slope from gutter to grade break (v/hz) = 0.020
slope from grade break to crown (v/hz) = 0.020
Street flow is on [1] side(s) of the street
Distance from curb to property line = 10.000(Ft.)
Slope from curb to property line (v/hz) = 0.020
Gutter width = 1.500(Ft.)
Gutter hike from flowline = 1.500(In.)
Manning's N in gutter = 0.0150
Manning's N from gutter to grade break = 0.0150
Manning's N from grade break to crown = 0.0150
Estimated mean flow rate at midpoint of street = 2.015(CFS)
Depth of flow = 0.244(Ft.), Average velocity = 3.207(Ft/s)Streetflow hydraulics at midpoint of street travel:
Halfstreet flow width = 7.465(Ft.)
Page 2 of 3
100 yr Flows to Exist CB - Corintia St.
Flow ve^city = 3.21(Ft/s)
Travel time = 2.19 min. TC = 9.62 min.
Adding area flow to street
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group C = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(Neighborhod commercial )
impervious value, Ai = 0.800
sub-Area C Value = 0.790
Rainfall intensity = 4.837(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.803 CA = 0.538
Subarea runoff = 1.244(CFS) for 0.380(Ac.)
Total runoff = 2.602(CFS) Total area = 0.670(Ac.)
Street flow at end of street = 2.602(CFS)
Half street flow at end of street = 2.602(CFS)
Depth of flow = 0.262(Ft.), Average velocity = 3.401(Ft/s)
Flow width (from curb towards crown)= 8.329(Ft.)
Process from Point/Station 345.000 to Point/Station 350.000
**** SUBAREA FLOW ADDITION ****
Decimal fraction soil group A = 0.000
Decimal fraction soil group B = 0.000
Decimal fraction soil group c = 0.000
Decimal fraction soil group D = 1.000
[COMMERCIAL area type ]
(Neighborhod Commercial )
impervious value, Ai = 0.800
Sub-Area C value = 0.790
Time of concentration = 9.62 min.
Rainfall intensity = 4.837(ln/Hr) for a 100.0 year storm
Effective runoff coefficient used for total area
(Q=KCIA) is C = 0.797 CA = 1.044
Subarea runoff = 2.445(CFS) for 0.640(Ac.)Total runoff = 5.048(CFS) Total area = 1.310(Ac.)End of computations, total study area = 1.310 (AC.)
Page 3 of3
CATCH BASIN CALCULATIONS
JJurb Inlet In Sag - Node 160
Project Description
Solve For
input Data
Discharge
Gutter Width
Gutter Cross Slope
Road Cross Slope
Curb Opening Length
Opening Height
Curb Throat Type
Local Depression
Local Depression Width
Throat Incline Angle
Results ,'. ,,j. '.
Spread
Depth
Gutter Depression
Total Depression
Spread
Horizontal
6.64 ffVs
1.50 ft
0.1031 ft/ft
0.0200 ft/ft
7.00 ft
10.00 in
2.50 in
1.50 ft
90.00 degrees
22.29 ft
0.57 ft
1.50 in
4.00 in
Bentley Systems, Inc. Haestad Methods Solution Center Bentley FlowMaster [08.01.066.00]
10/4/2007 4:47:47 PM 27 Siemens Company Drive Suite 200 W Watertown, CT 06795 USA +1 -203-755-1666 Page 1 of 1
Trapezoidal Channel - (Swale) Node 90
Project Description
Friction Method
Solve For
Input Data"
Roughness Coefficient
Channel Slope
Left Side Slope
Right Side Slope
Bottom Width
Discharge
Results J; • ''•
Normal Depth
Flow Area
Wetted Perimeter
Top Width
Critical Depth
Critical Slope
Velocity
Velocity Head
Specific Energy
Froude Number
Flow Type
GVF input Data
Downstream Depth
Length
Number Of Steps
GVF Output Data
Upstream Depth
Profile Description
Profile Headless
Downstream Velocity
Upstream Velocity
Normal Depth
Critical Depth
Channel Slope
Critical Slope
Manning Formula
Normal Depth
Subcritical
0.250
0.01500 ft/ft
3.00 ft/ft (H:V)
3.00 ft/ft (H:V)
4.00 ft
11.14 ff/s
1.67 ft
14.99 ft2
14.54 ft
14.00 ft
0.54 ft
1.25648 ft/ft
0.74 ft/s
0.01 ft
1.67 ft
0.13
0.00 ft
0.00 ft
0
0.00 ft
0.00 ft
Infinity ft/s
Infinity ft/s
1.67 ft
0.54 ft
0.01500 ft/ft
1.25648 ft/ft
10/4/2007 4:49:59 PM
Bentley Systems, Inc. Haestad Methods Solution Center Bentley Flow/Master [08.01.066.00]
27 Siemens Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 Page 1 of 1
Ditch Inlet In Sag - Node 92
Project Description
Solve For
Input Data
Discharge
Left Side Slope
Right Side Slope
Bottom Width
Grate Width
Grate Length
Local Depression
Local Depression Width
Grate Type
Clogging
Results
Spread
Depth
Wetted Perimeter
Top Width
Open Grate Area
Active Grate Weir Length
Spread
P-50mm(P-1-7/8")
11.14 ft3/s
3.00 ft/ft (H:V)
3.00 ft/ft (H:V)
4.00 ft
3.00 ft
3.00 ft
2.00 in
2.00 ft
50.00 %
4.26 ft
0.39 ft
4.82 ft
4.26 ft
4.05 ff
9.00 ft
Bentley Systems, Inc. Haestad Methods Solution Center Bentley Flow/Master [08.01.066.00]
10/4/2007 4:51:55 PM 27 Siemens Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 Page 1 of 1
Curb Inlet In Sag - (Exist. CB) Node 350
Project Description
Solve For
Input Data .
Discharge
Gutter Width
Gutter Cross Slope
Road Cross Slope
Curb Opening Length
Opening Height
Curb Throat Type
Local Depression
Local Depression Width
Throat Incline Angle
Results, .„.'; •'', ,", '•
Spread
Depth
Gutter Depression
Total Depression
Spread
Horizontal
2.60 ft3/s
1.50 ft
0.1031 ft/ft
0.0200 ft/ft
3.00 ft
10.00 in
2.50 in
1.50 ft
90.00 degrees
17.00 ft
0.46 ft
1.50 in
4.00 in
Bentley Systems, Inc. Haestad Methods Solution Center Bentley FlowMaster [08.01.066.00]
10/4/2007 4:53:46 PM 27 Siemens Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 Page 1 of 1
STORM DRAIN HYDRAULIC
CALCULATIONS
r
4--• 4-4 -1+48,10<-E< UOO-*-7-K> 4-.4 j~ .
BOSOK GROUND «--—r- T f—r~ :• ~r
-i—iQMX!--160,SCFS--
'• Vmo»= llSFPSi
——; -!- -0100- I54J) CFS ?-«-/---Vm<a= 12.3 FPSH-0100- t54.0:CFS
i Vmoxi 28.7 FPS 0100=717 .8 CFS!—r-i—i —<•—j--! i—I
i . i i I i I i _j_rrrr FT4' r
j—I—r~1—T'OHP--7J8-CFS*-445.BS__j_4_r L_i
H-H-4-332-
—H-00 ---—. -—- --5+00 - -— '—6+00 1+00 ~" "" r+oo"
LAT A-l LAT A-2
(PRIVATE STORM DRAIN) (PRIVATE STORM DRAIN)
FILOLI CIRCLE
BENCH MARK
DESCRIPTION: K-302. A STD. DISK STAMPED K 302 1935.
SET IN THE TOP OF A CONCRETE POST.
LOCATION: LIES 8.5' EASTERLY OF EASTERN BERM UNE
ON RANCHO SANTA FE ROAD. 133' NORTHERLY
OF ELECTRIC TRANSMISSION UNE POLE MARKED
TL230I1- AND TL13825-
RECORDED:
ELEVATION: 533.39 DATUM: NGVD 1929
"AS BUILT"
DAVID EVANS
AND ASSOCIATES INC
800 N. Haven Avenue. Suite 300
Ontano California 91 764
Phone: 909.481.5750
Fajc 909.481.5757
ENGINEERING DEPARTMENT
GRADING. EBOSION CONTROL AND STORM DBAIM PIAKS fOK
LA COSTA RIDGE
NEIGHBORHOOD 2.6
STORM DRAIN LINE A
VALLECITOS WATER DISTRICT
(FOR GRADING PURPOSES ONLY)
REVISION DESCRIPTIONVALLECITOS WATER DISTRICT
A.WSW
Tl JN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
T2 LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
T3 [P:\DRHH0030\0600INFO\EC\WSPGW\A.WSW]
SO -880.00 328.20 24 332.000
TS -855.00 328.30 24 .013
R -854.88 328.33 4 .013
WX -854.88 328.33 4 .013
R -775.59 329.06 4 .013
3X -771.42 329.10 4 11 .014 11.14 331.10
R:x
R
R
R
R
R
R
R
R
R
R
JX
R
SH
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
CD
PTS
PTS
PTS
Q
-700
-696
-661
-506
-502
-303
-299
-207
-165
-148
-144
-101
-97
-0
-0
1 4
2 4
3 4
4 4
5 4
6 4
7 4
8 4
9 4
11 4
12 4
13 4
14 4
15 4
16 4
17 4
18 4
19 4
20 2
21 2
22 2
23 2
24 5
25 5
26 5
24 4
25 3
26 3
.38 329.75
.21 329.81
.51 330.11
.85 331.54
.68 331.58
.94 333.41
.77 333.45
.44 342.94
.91 347.21
.44 349.13
.27 349.16
.27 349.72
.10 350.05
.00 353.50
.00 353.50
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
1 .000
0 .000
0 .000
0 .000
0 .000
0 .000
0 .000
0 .000
.000 1.000
.000 1.000
.000 1.000
154.000 .0
4
4 2
4
4
4
4
4
4
4
4
4
4
4 1
4
4
0.010
2.000
3.000
4.000
5.000
6.000
7.000
8.000
9.000
1.500
2.500
3.500
4.500
5.500
6.500
7.500
8.500
9.500
8.500
6.000
5.000
2.000
4.500
50.000
10.000
2.000
.013
.014 6
.013
.013
.013
.013
.014
.014
.013
.013
.013
.013
.014 0
.013
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
10.000
10.000
10.000
10.000
.000
.000
10.000
.000100
.000 20
.000 4
.64
.01
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
-22
333.50
-22
48
350.06
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000 .000 .000
.000 .000 .000
.000 .000 .000
.000 .000 .000
.000 .000 .000
.000 .000 .000
.000
.000
.000
.000
.000
50.00
.926
32.00
.926
.000
.000
.000
.000
.984
.000
.000
.000
.000
90.00
.000
.000
.000
.000
.000
.000
.000
0
.000
.000
.000
.000
.000
.000
.000
.000
0.000
0.000
0.000
0.000
0.000
0.000
0.000
0
0
0
0
.00
0
.00
0
01
01
0
0
01
0
-90.00
0.000
.000
.000
.000
.000
.000
.000
0
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000150.000 1.000
1.000
1.000
Page 1
FILE: a.WSW w s p G w - CIVILDESIGN version 14.05
Program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
UN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600lNFO\EC\WSPGW\A.WSW]
PAGE 1
Date:10- 5-2007 Time:11:39:58
************************************************************************************************************************** ********
station
L/Elem*********
-880.000
invert
Elev
Ch Slope*********
328.200
Depth
(FT)
********
3.800
waterElev
*********
332.000
Q
(CFS)
*********
vel velCFPS) Head_ i _
SF Ave******* i *******
171.79 .33 .00i i
EnergyGrd.El.
HF*********
332.00
SuperElev
SE Dpth*******
.00
Critical
Depth
Froude N********
.58
Flow Topwi dth
Norm Dp********
150.00
Height/Di a . - FT
"N"*******
Base wtor I.D.
x-Fall*******
24
ZL
ZR* * * * *
No Wth
Prs/Pip
Type Ch*******
0 .0
TRANS STR .0040 .0000 .00 3.80 .03. .013 IR-OPEN
1 1
-855.000 328.300 3.701 332.001 171.79 .34 .00 332.00 .00 .58 150.00 24 0 .0
-
-855.000
.120
-854.880
-
328.300
.2500
328.330
i
3.576 331.876
3.736 332.066
_i_ _|_
171.79 14.49 3.26
_ - 1 - - 1 - -
.0125
171.79 14.07 3.07_ i _
-
335.14
.00
335.14
-
.00
3.58
.00
3.74
1.16
3.74
-
2.46
1.33
1.99
4.000 .000
.013
4.000
.00
.000
-
.00
.00
.00
-
1 .0
PIPE
0 .0
WALL EXIT
1-854.880 328.330 3.736 332.066 171.79 14.07 3.07 335.14 .00 3.74 1.99 4.000 .000 .00 1 .0------1----i- ----
24.339 .0092 .0130 .32 3.74 1.00 4.00 .013 .00 .00 PIPEi
-830.541
54.951
328.554
.0092
4.000 332.554 171.79 13.67 2.90_ i _
.0140
335.46
.77
.00 3.74_ i _
4.00 .00
.00
4.00
4.000
.013
.000
.00
.00
.00
1 .0
PIPE
-775. 5901 329. 0601 4.28o' 333. 34o' 171.79' 13.67 2.9o' 336.24 ' .00 ' 3.74 ' .00 ' 4.000 ' .OOo' .00 ' 1 .0------1- -1--1------
JUNCT STR .0096 .0155 .06 .00 .00 .014 .00 .00 PIPE
1 1 1 1
-771.420 329.100 4.922 334.022 160.65 12.78 2.54 336.56 .00 3.67 .00 4.000 .000 .00 1 .0-----_ 1 _-1----1---
71.040 .0091 .0125 .89 .00 .00 4.00 .013 .00 .00 PIPE
1 III
-700.380 329.750 5.416 335.166 160.65 12.78 2.54 337.70 .00 3.67 .00 4.000 .000 .00 1 .0
-1--1--1- -1-----1--__
JUNCT STR .0144 .0139 .06 .00 .00 .014 .00 .00 PIPE
1 1 1
-696.210 329.810 5.796 335.606 154.01 12.26 2.33 337.94 .00 3.63 .00 4.000 .000 .00 1 .0--1- -1--1- -1---------
34.700 .0086 .0115 .40 .00 .00 4.00 .013 .00 .00 PIPE
FILE: a.WSW W S P G W - CIVILDESIGN Version 14.05
Program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
JN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600INFO\EC\WSPGW\A.WSW]
PAGE 2
Date:10- 5-2007 Time:11:39:58
Sr * * ft * * * ft * * * * * *
Station
L/Elem
* * * * -ti * * * *
-661.510
154.660
-506.850
4.170
-502.680
130.094
-372.586
invert
Elev
Ch slope*********
330.110
.0092
331.540
.0096
331.580
.0092
332.778
HYDRAULIC JUMP1
-372.586 332.778_ i
6.359
-366.227
21.772
-344.455
.0092
332.836
.0092
333.037
20.7441 .0092
-323.712 333.228
- 1 -
19.772 .0092
-303.940
Depth
(FT)
********
6.130
6.478
6.603
6.899
2.031
2.015
1.941
1.871
333.410 1.804i
waterElev
*********
336.240
338.018
338.183
339.677
334.809
334.852
334.978
335.099
Q
(CFS)
*********
154.01
154.01
154.01
154.01
Vel Vel
(FPS) Head_ i _
SF Ave******* i *******
12.26 2.33_ _ 1 _ _
.0115
12.26 2.33
-1-
.0115
12.26 2.33_ i _ _
.0115
12.26 2.33_ i _
Energy
Grd.El.
HF*********
338.57
1.78
340.35
.05
340.52
1.50
342.01__ _ ( _ __
1 1
154.01 24.03 8.97 343.78
154.01
154.01
154.01
.0442
24.27 9.15_ i _ _
.0478
25.46 10.06
_ - 1 -
.0543
26.70 11.07i
.06181 i
335.214 154.01 28.00 12.18i i
.28
344.00
1.04
345.04
1.13
346.17
1.22
347.39
SuperElev
SE Dpth*******
.00_ _
6.13
.00
-6.48
.00_
6.60
.00_
.00_ _
2.03
.00_ _
2.02
.00
1.94
.00
1.87
.00
4.170 .0096 ' .07751 .32 ' 1.80
criticalDepth
Froude N********
3.63_ _
.00.
3.63
-
.00
3.63
-
.00
3.63_
3.63_ __
3.35
3.63 _
3.40
3.63
3.65
3.91
3.63
Flow Top
Width
Norm Dp********
Height/Di a . - FT
"N"*******
.00 4.000
_ - 1 — -
Base wtor l.D.
x-Fall*******
.000
4.00 .013 .00i
.00
4.00
.00
4.00
.00
4.00
4.00
4.00
4.00
4.00
4.00
3.99
4.00
3.98
4.000
.013
4.000
.013
4.000
.000
.00
.000
.00
.000
4.000 .000
_ _ (
.013
4.000
.013
4.000
.013
4.000
.00
.000
.00
.000
.00
.000
.013 ' .001
4.000 .000i
ZL
ZR*****
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00_
.00
.00
.00
.00
NO Wth
Prs/Pip
Type Ch
* * is * * * *
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
4.20 4.00 .014 ' .OO1 .00 'PIPE
FILE: a.WSW w S P G w - CIVILDESIGN Version 14.05
Program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
3N DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600INFO\EC\WSPGW\A.WSW]
PAGE 3
Date:10- 5-2007 Time:11:39:58
* * it * * * * *
Station
L/Elem*********
-299.770
27.701
-272.069
28.165
-243.904
20.591
-223.313
15.873
-207.440
1.021
-206.419
11.183
-195.236
9.308
-185.928
7.825
invertElev
Ch slope*********
333.450
.1028
336.297
.1028
339.192
.1028
341.309_ _
.1028
342.940_ _
.1028
343.045
.1028
344.195
.1028
345.152
.1028
-178.103 345.956
Depth
(FT)
********
1.787_
1.833
1.902
Water
Elev
*********
335.237
338.130
341.094
1.974_
2.050
2.056
2.136
2.220
2.308
343.283
-
344.990
345.101
346.331
347.372
(CFS)
*********
154.01
154.01
154.01
154.01
-
154.01
154.01
154.01
154.01
Vel vel
CFPS) Head
-1-SF Ave******* i *******
28.35 12.48_ _ 1 __ _
.0754
27.40 11.66_ _ 1 _ _
EnergyGrd.El .
HF*********
347.71
2.09
349.79
.0676 1.90
126.13 10.60 351.70_ - 1 _ _
.0595
24.91 9.64
-1-.0524
23.75 8.76
_ - 1 - -
.0421
23.65 8.69_ i _ _
.0393
22.55 7.90_ i _
1.22
Super
Elev
SE Dpth*******
.92_ _
2.71
.86
2.69
.78
2.69
352.92 .71
.83 2.69
1353.75 .00
.04
353.79
.44
354.23
.0347 .32
121.50 7.18 354.55i i
.03061 .241 i
348.264 154.01 20.50 6.53
1
354.79
2.05
.00
2.06
.00
2.14
.00
Critical
Depth
Froude N********
3.63
4.27-
3.63
4.07
3.63
3.79
3.63
3.53
3.63
3.29
3.63_
3.27
3.63_
3.04
3.63_
2. 221 2.82
.00 3.63
Flow Topwidth
Norm Dp********
3.98
1.66
3.99
1.66
4.00
1.66
4.00_ _
1.66
4.00
1.59
4.00
1.59
3.99
1.59
3.98
1.59
3.95
Height/
Di a . - FT
"N"*******
4.000
.014
4.000
Base Wt
or I.D.
X-Fall*******
.000
.00
.000_
.014 .00
14.000 .000
.014
4.000
-.014
4.000
.013
4.000
.013
4.000
.013
4.000
.013
4.000
.00
.000-
.00
.000
.00
.000
ZL
ZR* * * * *
.00_
.00
.00_
.00
.00
.00
.00
.00
.00
.00
.00
.00' .00
.000 .00
.00
.000
.00
.000
.00
.00
.00
.00
6.607 .1028 ' ' .027l' .18 ' 2.3l' 2.62 ' 1.59 ' .013 ' .Oo' .00
NO wth
Prs/Pip
Type Ch*******
1 .0_
PIPE
1 .0
-
PIPE
1 .0
PIPE
1 .0-
PIPE
1 .0_
PIPE
1 .0
-
PIPE
1 .0_
PIPE
1 .0_
PIPE
1 .0_
PIPE
FILE: a.wsw w s P G w - CIVILDESIGN Version 14.05
Program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
DN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600INFO\EC\WSPGW\A.WSW]
PAGE 4
Date:10- 5-2007 Time:11:39:58
* * * * ft * it it
station
L/Elem*********
-171.496
-5.586
invert
Elev
ch slope*********
346.636
.1028
-165.910 347.210
1.712 .1099
1-164.198 347.398_
4.076
-160.122
3.432
-156.690
2.847
-153.843
2.319
Depth
(FT)
********
2.401
-
2.500
-
2.538
- 1 -.1099
1347.846 2.646_ - 1 -
.1099
348.223
.1099
348.536
.1099
2.761
2.885_ _
-151. 5241 348. 79l' 3.019_ i i
1.796
-149.727
1.287
-148.440
-.1099
348.989
.1099
349.130
-
3.168
-
3.336
4.170 .0072
Water
Elev
*********
349.037
-
349.710
-
349.936_ _
350.492
-
QCCFS)
*********
154.01
154.01
154.01
154.01
350.984 154.01i- 1 -
1351.421 154.01_
351.810
-
352.157
-
352.466
154.01
154.01
154.01
vel Vel
(FPS) Head
SF Ave******* i *******
19.55 5.93_ i _
.0240
Energy
Grd.El.
HF*********
354.97
.13
18.64 5.39 355.10
-1- -1-.0220 .04
118.31 5.21 355.14
- — 1 — -.0203
17.46 4.73_ i _
.0181
.08
355.22
.06
16.64 4.30 355.29i i- 1 -.0161
15.87 3.91_ i _ _
.0144
-.05
355.33
.03
15.13 3.56 355.37_ _ 1 _ 1
.0129
14.43 3.23
-1-.0117
13.76 2.94i
-.02
355.39
-.02
355.40
Super
Elev
SE Dpth*******
.00
2.40
.00
2.50
.00
2.54
.00
2.65
critical
Depth
Froude N********
3.63
2.43
Flow Top
width
Norm Dp********
3.92
1.59
3.63 3.87
-1-2.25 1.56
13.63 3.85
2.18
3.63
2.02
1.56
3.79
1.56
.00 3.63 ' 3.70
2.76
.00
Height/
Dia.-FT
"N"*******
4.000
.013
4.000
.013
4.000
.013
4.000
.013
4.000
1.85 1.56 .013
1 13.63 3.59 4.000i i
2.891 1.70 ' 1.56 ' .013
I
.00 3.63_ _
3.02
.00
-3.17
.00
1.55
1.40
3.63
3.44_ _
1.56
3.25
1.56
2.98
4.000_ _
.013
4.000
.013
4.000
Base wt
or I.D.
x-Fall****** *
.000
.00
.000
.00
.000
.00
.000
.00
.000
.00
.000
.00
.000
.00
.000
.00
.000
ZL
ZR*****
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
.00
No Wth
Prs/Pip
Type Ch*******
1 .0
PIPE
1 .0
PIPE
1 .0
-PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0_ _
.0112 .05 3.34 1.25 4.00 .013 .00 .00 PIPE
FILE: a.wsw W S P G W - CIVILDESIGN Version 14.05
Program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
JN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600lNFO\EC\WSPGW\A.WSW]
PAGE 5
oate:10- 5-2007 Time:11:39:58
***** ** *
Station
L/Elem* * * ***** *
-144.270
Invert
Elev
Ch Slope*********
349.160
26.823 .0130
-117.447 349.509--
16.177 .0130
-101.270 349.720_
3UNCT STR .0791
-97.100 350.050--25.126 .0355
-71.974 350.943--21.378 .0355
-50.596 351.702
16.18l' .0355
-34.415 352.277-
12.328 .0355
-22.088 352.715--9.296 .0355
-12.792 353.045
-1-6.752 .0355
Depth
(FT)
* * * * * * * *
3.307
-
3.409
-
3.625
-
2.489
-
2.581
-
2.691
~
2.809_
2.937
-
3.077
-
water
Elev
* * *******
352.467
QCCFS)
*********
154.01
vel vel
(FPS) Head
SF Ave******* i *******
13.86 2.98i
Energy
Grd.El .
HF*********
355.45
.Olio' .30
1
352.918 154.01 13.49 2.83 355.75
-1- -I- -1- -I-.0104 .17
1
353.345 154.01 12.86 2.57 355.91i i-
i
352.539 154.00 18.73 5.45 357.99
--_ 1 _-.0217 .54
1 1
353.524 154.00 17.96 5.01 358.53
-1--1-_ _
.0194 .41i
354.393 154.00 17.13 4.55_i_ __ -1-358.95
.0172 .281355.086 154.00 16.33 4.14 359.23
--1- -1-
_
.0154 .19
355.652 154.00 15.57 3.76 359.42
-1--1- -1-.0138 .13j
356.123 154.00 14.84 3.42 359.54
--_ i _-.0124 .08
super
Elev
SE Dpth* * * * * * *
.00
3.31
.00-
3.41
4.00
4.00
.00
-2.49
.00
-2.58
.00_
2.69
.00-
2.81
.00-
2.94
.00
-3.08
Critical
Depth
Froude N********
3.63
1.28-
3.63-
1.19
3.63
1.00
3.63
-2.27
3.63
-2.11
3.63
1.95
3.63
1.79
3.63
-1.64
3.63
-1.49
Flow Top
Width
Norm Dp********
Height/Dia.-FT
"N"*******
Base wt
or I.D.
x-Fall*******
3.03 4.000 .000i i- 1 - - 1 -3.08 .013 .00
12.84 4.000 .000
-1--3.08 .013 .00
1 12.33 4.000 .000
.014 .00
3.88 4.000 .000--
2.16 .013 .00
13.83 4.000 .000
--
2.16 .013 .00i
3.75 4.000 .000
2.16 .013 ' .00
3.66 4.000 .000
---
2.16 .013 .00
3.53 4.000 .000
--
2.16 .013 .00
3.37 4.000 .000---2.16 .013 .00
ZL
ZR*****
.00
-.00
.00-.00
.00
-.00
.00-.00
.00-.00
.00_
.00
.00-.00
.00-.00
.00-.00
NO Wth
Prs/Pip
Type Ch*******
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-PIPE
1 .0_
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
FILE: a.wsw w S P G W - CIVILDESIGN Version 14.05
program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
DN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE A - 02/06/07 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600lNFO\EC\WSPGW\A.WSW]
Date:10- 5-2007
PAGE 6
Time:ll:39:58
************************************************************************************************************************** ********
station
L/Elem*********
invertElev
ch slope*********
-6.040 353.285
_ I _
Depth
(FT)
* * A * * * * *
3.232
Water
Elev
*********
356.517
Q
(CFS)
*********
vel vel(FPS) Head_ 1 _
SF Ave*******!*******
154.00 14.15 3.11
1 1
Energy
Grd.El .
HF*********
359.63
Super
Elev
SE Dpth*******
.00
criticalDepth
Froude N********
3.63
Flow Top
Width
Norm Dp******* *
3.15
Height/
oia. -FT
"N"****** *
4.000
Base wt|
or I.D. 1 ZL_
X-Fall | ZR******* 1 *****
1.000 .00i
No Wth
Prs/Pip
Type Ch*******
1 .0
4.362 .0355 .0113 .05 3.23 1.34. 2.16 .013 .00 .00 PIPE
1 1 1 1 1-1.678 353.440 3.409 356.849 154.00 13.49 2.83 359.68 .00 3.63 2.84 4.000 .000 .00 1 .0_|. -|- -|- -|- -|- -|---1---1- -1--
1.678 .0355 .0104 .02 3.41 1.19 2.16 .013 .00 .00 PIPE
1 1 1 1 1.000 353.500 3.625 357.125 154.00 12.86 2.57 359.69 .00 3.63 2.33 4.000 .000 .00 1 .0-I--I-
Al.WSW
Tl UN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
T2 LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
T3 [P:\DRHH0030\0600lNFO\EC\WSPGW\Al.WSW]so 100.
R 132.
SH 132.
CD 1 4
CD 2 4
CD 3 4
CD 4 4
CD 5 4
CD 6 4
CD 7 4
CD 8 4
CD 9 4
CD 11 4
CD 12 4
CD 13 4
CD 14 4
CD 15 4
CD 16 4
CD 17 4
CD 18 4
CD 19 4
CD 20 2
CD 21 2
CD 22 2
CD 23 2
CD 24 5
CD 25 5
CD 26 5
PTS 24 4
PTS 25 3
PTS 26 3
Q
00 330
83 335
83 335
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
0
0
0
0
0
0
0
.000
.000
.000
11.140
.08 2
.50 2
.50 2
.000 1.000
.000 2.000
.000 3.000
.000 4.000
.000 5.000
.000 6.000
.000 7.000
.000 8.000
.000 9.000
.000 1.500
.000 2.500
.000 3.500
.000 4.500
.000 5.500
.000 6.500
.000 7.500
.000 8.500
.000 9.500
.000 8.500
.000 6.000
.000 5 . 000
.000 2.000
.000
.000
.000 4.500
1.000 10.000
1.000 10.000
1.000 2.000
.0
.013
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
.000 .000
10.000 .000
10.000 .000
10.000 .000
10 . 000 . 000
.000 .000
.000 .000
10 . 000 . 000
.000 20.000
.000 20.000
.000 4.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
1.000
1.000
333.340
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
30.000
.000
.000
.000
.000
.000 .
.000 .
1.000
.000
.000
.000
.000
000
000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
0
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
Page 1
FILE: al.wsw W S P G W - CIVILDESIGN Version 14.05Program Package serial Number: 1425
WATER SURFACE PROFILE LISTING
UN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600lNFO\EC\WSPGW\Al.WSW]
Date:10- 4-2007
PAGE 1
Time: 5:40:49
****************************************************************************************************** ********
Station
L/Elem*********
100.000
4.885
104.885
InvertElev
Ch Slope*********
330.080
.1651
330.887
Depth
(FT)
********
3.260
2.465
water
Elev
*********
333.340
333.352
QCCFS)
*********
11.14
11.14
Vel VelCFPS) Head_ - 1 - -
SF AV6******* i *******
3.55 .20_ 1 _ _
.0024
3.55 .20
Energy
Grd.EI .
HF*********
333.54_ _
.01
333.55
Super
Elev
SE Dpth*******
.00
3.26
.00
CriticalDepth
Froude N********
1.20
.00
1.20
Flow Top
Wi dth
Norm Dp********
.00
.47
.00
Height/
Dia.-FT
"N"*******
2.000
.013
2.000
Base Wt
or l.D.
x-Fall*******
.000
.00
.000
ZL
ZR*****
.00
.00
.00
No wth
Prs/Pip
Type Ch*******
1 .0
PIPE
1 .0
HYDRAULIC JUMP
1 1104.885 330.887 .536 331.422 11.14 16.45 4.20 335.63 .00 1.20 1.77 2.000 .000 .00 1 .0. ---1- -1--1- -1- -1--1---1--
1.449 .1651 .0963 .14 .54 4.69 .47 .013 .00 .00 PIPE
1 1 1106.335 331.126 .541 331.667 11.14 16.21 4.08 335.75 .00 1.20 1.78 2.000 .000 .00 1 .0-----1- -1---1--1--1--
4.590 .1651 .0884 .41 .54 4.60 .47 .013 .00 .00 PIPEi
110.925 331.884
- 1 - -
.560 332.444 11.14 15.46 3.71i 336.15 .00 1.20 1.80 2 . 000 . 000 .00 1 .01
3.628 .1651 .0773 .28 .56 4.30 .47 .013 .00 .00 PIPE11114.553 332.483 .579 333.062 11.14 14.74 3.37 336.44 .00 1.20 1.81 2.000 .000 .00 1 .0__ __ __ __ __ -1- -1- -1- -- -1- -- -- --
2.943 .1651 .0677 .20 .58 4.02 .47 .013 .00 .00 PIPE1117.496 332.968 .599 333.567 11.14 14.05 3.07 336.63 .00 1.20 1.83 2.000 .000 .00 1 .0---1--_ | _-1--1-----
2.435 .1651 .0592 .14 .60 3.77 .47 .013 .00 .00 PIPE
119.931
2.044
121.976
333.370
.1651
333.708
.620
.642
333.991
334.350
11.14
11.14
13.40 2.79_ - 1 -
.0519
12.78 2.53_ i _
336.78
.11
336.88
.00
.62
.00
1.20
3.52
1.20
1.85
.47
1.87
2.000
.013
2.000
.000
.00
.000
.00
.00
.00
1 .0
PIPE
1 .0
1.7341 .1651 ' .04551 .08 ' .64' 3.30 ' .47 ' .013 ' .Oo' .00 ' PIPE
FILE: al.wsw w S P G w - CIVILDESIGN Version 14.05
Program Package serial Number: 1425
WATER SURFACE PROFILE LISTING
3N DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600lNFO\EC\WSPGW\Al.WSW]
PAGE 2
Date:10- 4-2007 Time: 5:40:49
V ***** * ***** ft * *
Station
L/Elem*********
123.709
1.481
invertElev
ch slope*********
333.994
Depth
(FT)
********
.665
.1651
1
waterElev
*********
334.659
CCFS)
*********
11.14
i
vel velCFPS) Head
SF AV6******* i *******
12.18 2.30_ i _ _
Energy
Grd.El .
HF*********
336.96
.0398 .06
1
superElev
SE Dpth*******
.00
.67
CriticalDepth
Froude N********
1.20
Flow TopWidth
Norm Dp********
1.88
3.08 .47i
125.190 334. 2391 .689' 334. 92s' 11. 14 ' 11.61 2.09' 337.02 ' .00 ' 1.20 ' 1.90
-1- -1---1- -1---1-1.278 .1651 .0349 .04 .69 2.88 .47
1 1126.469 334.450 .713 335.163 11.14 11.07 1.90 337.07 .00 1.20 1.92-----I i ---1.094 .1651 .0306 .03 .71 2.69 .47
1 1 1 1 .127.562 334.630 .739 335.369 11.14 10.56 1.73 337.10 .00 1.20 1.93---1--1- -1--1--
.950 .1651 .0268 .03 .74 2.52 .47
1 1 1 1128.513 334.787 .765 335.552 11.14 10.07 1.57 337.13 .00 1.20 1.94--1--1- -1--1--
.813 .1651 .0235 .02 .77 2.35 .47
1 1 1 1
129.326 334.921 .793 335.715 11.14 9.60 1.43 337.15 .00 1.20 1.96-----_ 1 _--1--
.700| .1651 ( .0207| .01 ( .79| 2.20 ( .47
130.025 335.037
.600' .16511
.822 335.859 11.14 9.15 1.30_ i _ _
.0181
337.16 .00
.01 ' .82i
1.20
2.05
1.97
.47
130.626 335.136 .852 335.988 11.14 8.73 1.18 337.17 .00 1.20 1.98---1--1- -1- -1- -1--1-
.513 .1651 .0159 .01 .85 1.91 .47
1 1 1
131.139 335.221 .883 336.104 11.14 8.32 1.07 337.18 .00 1.20 1.99__ __ __ __ __ - 1 - -- -- -- -- -
.428 .1651 .0140 .01 .88 1.79 .47
Height/Dia.-FT
"N"*******
2.000
.013
Base Wt
or I.D.
x-Fall*******
.000
.00
ZL
ZR*****
.00_
.00
2.000 .000 .00
-_-
.013 .00 .00
2.000 .000 .00
---
.013 .00 .00
1
2.000 .000 .00_-1-
.013 .00 .00
2.000 .000 .00
-1--
.013 .00 .00
2.000 .000 .00---
.013 .00| .00
2.000 .000_ 1 _
.013 .00
.00
.00
2.000 .000 .00
--1-.013 .00 .00
2.000 .000 .00
.013 .00 .00
No WthPrs/Pip
Type Ch
* A * * * ft *
1 .0_
PIPE
1 .0-
PIPE
1 .0-
PIPE
1 .0-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
1 .0
-
PIPE
FILE: al.wsw w s P G w - CIVILDESIGN Version 14.05
program package Serial Number: 1425
WATER SURFACE PROFILE LISTING
JN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600lNFO\EC\WSPGW\Al.WSW]
PAGE 3
Date:10- 4-2007 Time: 5:40:49
********
Station
L/Elem*********
invertElev
ch Slope*********
131.567 335.291--
.359 .1651
131.926 335.3511 _ _
.290 .1651
132.216 335.399
-.228 .1651|
132.444 335.436--
.171 .1651
132.615 335.464--
.125 .1651|
132.739 335.485
.070 .1651
132.810 335.497-_
.020 .1651
132.830 335.500
Depth
(FT)
********
.916
-
.950
-
.986
-
1.024
-
1.064-
1.105
1.149
-
1.197
waterElev
*********
(CFS)
*********
vel vel(FPS) Head_ - 1 -
SF AV6******* i *******
Energy
Grd.El.
HF*********
Super
Elev
SE Dpth*******
Critical
Depth
Froude N********
Flow Top
wi dth
Norm Dp********
336.208 11.14 7.93 .98 337.18 .00 1.20 1.99
-1-_ i _----.0123 .00 .92 1.67 .47
1336.301 11.14 7.56 .89 337.19 .00 1.20 2.00
III II 1-_!_ _!_ _!_ -J- _|- -|-
.0108 .00 .95 1.55 .47
336.385 11.14 7.21 .81 337.19 .00 1.20 2.00
--1- -1- -1- -1- -1- -1-.0095 .00 .99 1.45 .47I
336.460 11.14 6.88 .73 337.19 .00 1.20 2.00
--_ i _-i--
.0084 .00 1.02 1.35 .47
1 1
336.529 11.14 6.56 .67 337.20 .00 1.20 2.00--1- -1- -1-i -
.0074 .00 1.06 1.25 .47
336.590 11.14 6.25 .61i 337.20 .00 1.20 1.99
.00651 .00 ' l.ll' 1.16 ' .47
1 1 1336.646 11.14 5.96 .55 337.20 .00 1.20 1.98-_|_ -1- -I- -1- -1--
.0058 .00 1.15 1.08 .47
336.697
-
I 1 111.14 5.68 .50_|- _i_337.20 .00i_ 1 1.20 1.96
Height/
Dia.-FT
"N"*******
Base wt
or I.D.
x-Fall*******
ZL
ZR*****
NO Wth
Prs/Pip
Type Ch*******
2.000 .000 .00 1 .0
----
.013 .00 .00 PIPE
1 1
2.000 .000 .00 1 .0I i- 1 1.013 .00 .00 PIPE
2.000 .000 .00 1 .0----
.013 .00 .00 PIPE
2.000 .000 .00 1 .0
--1--
.013 .00 .00 PIPE
12.000 .000 .00 1 .0----
.013 .00 .00 PIPEi
2.000 .000 .00 1 .0_
.013 .00 .00 PIPE12.000 .000 .00 1 .0
--1--
.013 .00 .00 PIPE
2.000
-
.000 .00 1 .0
A2.WSW
Tl UN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
T2 LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
T3 [P:\DRHH0030\0600INFO\EC\WSPGW\A2.WSW]so 100.
R 166.
SH 166.
CD 1 4
CD 2 4
CD 3 4
CD 4 4
CD 5 4
CD 6 4
CD 7 4
CD 8 4
CD 9 4
CD 11 4
CD 12 4
CD 13 4
CD 14 4
CD 15 4
CD 16 4
CD 17 4
CD 18 4
CD 19 4
CD 20 2
CD 21 2
CD 22 2
CD 23 2
CD 24 5
CD 25 5
CD 26 5
PTS 24 4
PTS 25 3
PTS 26 3
Q
00 330.99 1145 334.72 1145 334.72 11
1 .000 1.000
1 .000 2.000
1 .000 3.0001 .000 4.000
1 .000 5.0001 .000 6.000
1 .000 7.000
1 .000 8.000
1 .000 9.000
1 .000 1.500
1 .000 2.500
1 .000 3.500
1 .000 4.5001 .000 5.5001 .000 6.500
1 .000 7.500
1 .000 8.500
1 .000 9.500
0 .000 8.500
0 .000 6.000
0 .000 5.0000 .000 2.000
0 .000
0 .0000 .000 4.500
.000 1.000 10.000
.000 1.000 10.000
.000 1.000 2.000
6.640 .0
.013
.000
.000
.000
.000.000
.000
.000
.000
.000
.000
.000
.000.000.000
.000
.000
.000
.000
10.000
10.000
10.00010.000
.000
.000
10.000
.000 20
.000 20
.000 4
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
.000
1.000
1.000
335.606
.000
.000
.000
.000.000
.000
.000
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
30.000
.000
.000
.000.000.000.000
.000
.000
.000.000
.000
.000
,000
.000
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
.000
0
.000
.000
.000
.000
.000
.000
.000.000
.000
.000
.000
.000
1.000
Page 1
FILE: A2.WSW w s P G w - CIVILDESIGN Version 14.05
Program Package serial Number: 1425
WATER SURFACE PROFILE LISTING
JN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600INFO\EC\WSPGW\A2.WSW]
PAGE 1
Date:10- 4-2007 Time: 5:41:10
ft***************** ***********
Station
L/Elem*********
100 . 000
59.766
159.766
2.231
161.997
1.064
invert
Elev
Ch Slope*********
Depth
(FT)
********
330.990 4.616
-1-.0561
1
334.345
.0561
334.470
.0561
163. 06l' 334.530_ 1
.133
163.193
HYDRAULIC
.0561
334.537
1.500
1.360
1.280
1.280
JUMP
1
163. 1931 334.5371 .755
.409
163.602
.0561
334.560 .784
.9271 .0561 i
164.529
.729
165.258
.537
334.612 .815
.0561
334.653 .847
.0561
*************************************
Water
Elev
*********
QCCFS)
**** *****
335.606 6.64
-1-
I
335.845 6.64
-1-
i
Vel Vel
(FPS) Head_ i _ _
SF AV6*******!* ******
3.76 .22
-1-.0040
3.76 .22
.0037
335.830 6.64 3.94 .24
-1- -1- -1-.0036
335.810
-
335.817_
6.64
6.64
335.292 6.64i_
335.344
-
335.427
-
335.500
-
~ -
6.64
4.13 .27_ - 1 -
.0037
4.13 .27_ 1 _1
7.45 .86_ - 1 - -
.0147
7.10 .78i
.0129
6.64
6.64
6.77 .71
.0114
6.45 .65
.0101
*******************
Energy
Grd.EI .
HF*********
Super
Elev
SE Dpth*******
335.83 .00
-1-.24 4.62
336.06
.01
336.07
.00
336.08_
.00
336.08
.00
-1.50
.00
1.36
.00_ _
1.28
.00_ _
I
336.15 .00_ _
.01
336.13_ _
.01
.76
.00
.78
336.14 .00
-1-.01 .82
336.15
.01
.00
-.85
t********************** ************* **** ********
Critical
Depth
Froude N
***** ft * *
1.00
-.00
Flow Top
Width
Norm Dp********
.00
.53
1.00 .00-1-.00 .53
1.00 .87
-1-.50 .53
1.00_
.59
1.00_
Height/
Di a . - FT
"N"* * * * * * *
1.500
.013
1.500
.013
1.500
.013
Base Wt
or I.D.
x-Fall*******
.000
.00
.000
.00
,000-.00
1.06 1.500 .000i-
.53
1.06
1.00 1.50_ i
1.70
1.00 _
1.58
1.00
-1.47
1.00
1.37
.53
1.50
.013
1.500
1.500
.013
1.500
.53 ' .013i
1.49 1.500
-1-.53 .013
1.49 1.500
-1-.53 .013
.00
.000
.000
.00
.000
.00
.000
.00
.000
.00
ZL
ZR
* * * * it
.00
.00
.00
.00
.00
.00
.00
.00
.00
NO wth
Prs/Pip
Type Ch*******
1 .0-PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
1
.00 t i .0
.00
.00
.00
.00
.00
.00
.00
PIPE
1 .0
PIPE
1 .0
PIPE
1 .0
PIPE
FILE: AZ.WSW w s P G w - CIVILDESIGN version 14.05Program Package Serial Number: 1425
WATER SURFACE PROFILE LISTING
DN DRHH0030 - LA COSTA RIDGE NEIGHBORHOOD 2.6
LINE Al - 03/06/06 BY W.D.H., REVISED 10/04/07 BY W.D.H.
[P:\DRHH0030\0600INFO\EC\WSPGW\A2.WSW]
Date:10- 4-2007
PAGE 2
Time: 5:41:10
************************************************************************************************************************** ********
Station
L/Elem*********
165.794
.368
166.163
.218
166.381
.069
invertElev
Ch Slope*********
334.683
.0561
334.704
Depth
(FT)
ft*******
.881
.917
water
Elev
*********
335.564
335.621
(CFS)
*********
6.64
6.64
.0561
1 1 1
334.716 .955 335.671 6.64
-1- -1- -1-
.0561
166.450 334.720
-1-
.997 335.717
vel vel(FPS) Head
SF Ave******* | *******
6.15 .59
_ - 1 -
.0089
5.86 .53_ _ 1 _ _
.0079
5.59 .49
.0070
6.64 5.32 .44
-1- -1-
Energy
Grd.El .
HF*********
336.15
.00
336.15
Super
Elev
SE Dpth*******
.00
.88
.00
.00 .92
1
336.16 .00
-1-
.00 .96•
336.16
critical
Depth
Froude N********
1.00
1.27 .
1.00
-
1.17
1.00
1.09
.00 1.00
-1-
Flow Top
Width
Norm Dp********
1.48
.53
1.46
-
.53
1.44
.53
1.42
Height/Di a . - FT
"N"A A ft * * * *
1.500
Base wtor I.D.
x-Fall* * * * * * *
.000
.013 ' .00
1
1.500 .000
- - 1
.013
1.500
.013
1.500
.00
.000
.00
.000
ZL
ZR*****
.00_
.00
.00_
.00
.00
.00
.00-
NO WthPrs/Pip
Type Ch*******
1 .0
-
PIPE
1 .0
PIPE
1 .0
-
PIPE
1 .0
-
RIP RAP CALCULATIONS
DAVID EVANS JN
BY
JOB DESCRIPTION ......
CALCULATION FOR ^_
DATE |p -PS --
OF HEETS
CHECKED BY ....... ......... ______ DATE .
5^ W<S- "Mr
I \ C \f",~: T~>
us CJ
8/14/06, Calculations
DAVID EVANS
ANDASSOCIATES i
JOB DESCRIPTION .
CALCULATION FOR .
JN
BY..,., DATE
SHEET OF
CHECKhO BY _ DATE .
SHEETS
* - o 484<?1 ..=,
S/l 4/06, Calculations
t i It t i i I f, t