HomeMy WebLinkAboutCT 14-11; CARLSBAD BOAT CLUB & RESORT; DRAINAGE STUDY; 2006-12-31CARLSBAD BOAT CLUB
DRAINAGE STUDY
~0~~ C-2-~-oG
RcibertD.Dentino RCE #45629 Exp. 12/31/06
EXCEL ENGINEERING
440 State Place
Escondido, CA 92029
(760) 745-8118
DEC 1 9 2014
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TABLE OF CONTENTS
Summary ............................................................................................................................... .
Vicinity Map ......................................................................................................................... .
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2
1111 APPENDICES ..
San Diego County Isopluvial Chart 100-Year, 6-Hour ................................................... A ,.
111 Tables and Charts for run-off coefficients and times of concentration ................................. B
... On-site Detention Calculations .............................................................................. C
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Existing Condition Hydro logic Calculations for the 100-Year Storm Event ............................... D
Developed Condition Hydro logic Calculations for the 100-Y ear Storm Event ........................... E
Hydraulic Calculations .................................................................................................................. F
85th Percentile Calculations ........................................................................................................... G
Hydrology Map .......................................................................................... Pocket
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HYDROLOGY
Summary
This 1.02-acre project (APN 206-200.06) is located on the south side of Adams Street, east of the
intersection with Highland Drive in the City of Carlsbad. Topographically the site slopes to the
south towards the Agua Hedionda Lagoon. Very little runoff enters the site from the adjacent
property to the west.
Existing Condition
This project is adjacent and north of the Agua Hedionda Lagoon, which serves a final repository
of an enormous drainage basin that serves parts San Diego North County, including Carlsbad and
San Marcos. The final step after the Agua Hedionda Lagoon is the Pacific Ocean .
The current site is approximately 57% impervious. Using table 3-1, in Appendix B, a prorated C
value of 0.67 is obtained for soil type D and an impervious percentage of 57% .
The current storm waters are partly absorbed onsite and the remainder flow southerly towards the
Agua Hedionda Lagoon. There currently exists a large residential structure that serves as the Boat
Club's meeting and administrative facilities. The parcel is lightly vegetated and a large portion of
the site is paved with very weathered asphalt. There are no storm drain facilities on-site and the
run-off from storm events sheet flows into the beach at the south end of the property and into the
Lagoon. The current site generates approximately 3 .94 cfs in a 100-year storm event.
Developed Condition
The existing residence/boat dub structure is to be removed. fu its place will be a new 3 story boat
club and time share with under ground parking for vehicles and small boats: Three floors will be
visible from the Lagoon and only one floor will be visible from Adams Street. The site will be
accessed from Adams Street via a driveway, which starts out at 5% and at its steepest point
reaches 19%.
The proposed site is approximately 63% impervious. Using table 3-1, in Appendix B, a prorated
C value of0.70 is obtained for soil type D and an impervious percentage of 63%.
The runoff generated by a 100-year storm event has been calculated to be approximately 4.25 cfs,
an increase of .31 cfs. This runoff will be collected in an on-site storm drain system and allowed
to infiltrate and to settle debris & hydrocarbons before discharging into the Agua Hedionda
Lagoon. Additionally the project will be detaining the additional 0.31 cfs, generated by the new
development, before treating it and discharging into the Agua Hedionda Lagoon
Watershed
• The watersheds were analyzed using the 2003 San Diego County Hydrology Manual. ..
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Pre-Development
Pre-development Condition, as described in the Hydrology Calculations, is 0.90 acres and
contributes 3.94 cfs (100-year) in pre-development conditions. This runoff drains directly to the
Agua Hedionda Lagoon
Post-Development
Area "A" (Hydrology Map, Pre-development Conditions), as described in the Hydrology
Calculations, is 0.13 acres and contributes 0.58 cfs (100-year) in post-developed conditions. This
runoff drains directly to the proposed curb inlet located on the west side of the driveway .
Area "B", as described in the Hydrology Calculations, is .08 acres and contributes 0.38 cfs (100-
year) in the post-developed condition. This runoff drains directly to the proposed curb inlet
located on the east side of the driveway .
Area "C" is .11 acres and contributes .35 cfs (100-year) in the post-developed condition. This
runoff drains directly to the proposed curb inlet located at the end of the driveway.
Area "D" is .18 acres and contributes 0.83 cfs (100-year) in the post-developed condition. This
runoff is flow southerly along the east property line and onto and into the Agua Hedionda
Lagoon. This runoff passes through pedestrian concrete walkways and boat ramp area.
Subsequently no hydrocarbons or pollution is picked up in its flow.
Area "E" is .11 acres and contributes 0.48 cfs (100-year) in the post-developed condition. This
will across the club house patio area and onto the beach. More than 50% of the square footage of
area "E" is the beach it's self. This area contributes the least to any possible poliution of the
Agua Hedionda Lagoon.
Area "F" is 0.29 acres and contributes 1.65 cfs (100-year) in the post-developed condition. This
runoff will flow to roof drains and to the storm drain system located in the driveway on the west
side of the project. Tiris water then confluences with the runoff from areas "A", "B" and "C" and
will be processed through a detention facility before any discharge into the Agua Hedionda
Lagoon .
All runoff from this project will ultimately proceed southerly and into the Agua Hedionda
Lagoon. According to the 1998 303d list published by the San Diego Regional Water Quality
Control Board, the Agua Hedionda Lagoon is an "impaired water body". Pre-and post-
construction BMPs are mentioned in the Water Quality Technical Report for this project and will
be detailed in the project's future SWPPP .
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VICINITY MAP
Not to Scale
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APPENDIX A
County of San Diego
2003 Isopluvials
100-Y ear Rainfall Event -6 Hour & 24 Hour
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County of San Diego
Hydrology Manual
Rainfall Isopluvia/s
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County of San Diego
Hydrology Manual
Rainfa/l lsop/wials
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APPENDIXB
Tables and Charts for run-off coefficients and times of concentration
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San Diego County Hydrology Manual
Date: June 2003
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Table 3-1
RUNOFF COEFFICIENTS FOR URBAN AREAS
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Section:
Page:
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6 of26
Land Use I Runoff Coefficient "C"
Soil T~e
NRCS Elements Coun Elements ¾IMPER. A B C D
Undisturbed Natural Terrain (Natural) Permanent Open Space 0* 0.20 0.25 0.30 0.35
Low Density Residential (LDR) Residential, 1.0 DU/A or less 10 0.27 0.32 0.36 0.41
Low Density Residential (I.DR) Residential, 2.0 DU/Aor less 20 0.34 0.38 0.42 0.46
Low Density Residential (LDR) Residential, 2.9 DU/A or less 25 0.38 0.41 0.45 0.49
Medium Density Residential (MDR) Residential, 4.3 DU/A or less 30 0.41 0.45 0.48 0.52
Medium Density Residential (MDR) Residential, 7.3 DU/A or less 40 0.48 0.51 0.54 0.57
Medium Density Residential (MDR) Residential, 10.9 DU/A or less 45 0.52 0.54 0.57 0.60
Medium Density Residential (MDR) Residential, 14.5 DU/A or less 50 0.55 o.58. 0.60 0.63
High Density Residential (HDR) Residential, 24.0 DU/A or less 65 0.66 0.67 0.69 0.71
High Density Residential (HDR) Residential, 43.0 DU/A or less 80 0.76 0.77 0.78 0.79
CommerciaVIndustrial (N. Com) Neighborhood Commercial 80 0.76 0.77 0.78 0.79
CommerciaVIndustrial (G. Com) General Commercial 85 0.80 0.80 0.81 0.82
· CommerciaVIndustrial (O.P. Com) Office Professional/Commercial 90 0.83 0.84 0.84 0.85
CommerciaVIndustrial (Limited I.) Limited Industrial 90 0.83 0.84 0.84 0.85
CommerciaVIndustrial (General I.) General Industrial 95 0.87 0.87 0.87 0.87
*The values associated with 0% impervious may be used.fqr direct calculation of the runoff coefficient as described in Section 3.1.2 (representing the pervious runoff
coefficient, Cp, for the soil type}, or for areas that will remain undisturbed in perpetuity. Justificatioq must be given that the area will remain natural forever (e.g., the area
is located in Cleveland National Forest). ·
DU/A= dwelling units per acre
NRCS = National Resources Conservation Service
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San Diego County Hydrology Manual
Date: June 2003
Section:
Page:
3
12 of26
Note that the Initial Time of Concentration should be reflective of the general land-use at the
upstream end of a drainage basin. A single lot with an area of two or less acres does not have
a significant effect where the drainage basin area is 20 to 600 acres .
Table 3-2 provides limits of the length (Maximum Length (LM)) of sheet flow to be used in
hydrology studies. Initial Ti values based on average C values for the Land Use Element are
also included. These values can be used in planning and design applications as described
below. Exceptions may be approved by the "Regulating Agency" when submitted with a
detailed study .
Table 3-2
MAXIMUM OVERLAND FLOW LENGTH (LM)
& INITIAL TIME OF CONCENTRATION (T1)
Element* DU/ .5% 1% 2% 3% 5% 10%
Acre LM Ti LM Ti LM Ti LM Ti LM Ti LM Ti
Natural 50 13.2 70 12.5 85 10.9 100 10.3 100 8.7 100 6.9
LDR 1 50 12.2 70 11.5 85 10.0 100 9.5 100 8.0 100 6.4
LDR 2 50 11.3 70 10.5 85 9.2 100 8.8 100 7.4 100 5.8
LDR 2.9 50 10.7 70 10.0 85 8.8 95 8.1 100 7.0 100 5.6
MOR 4.3 50 10.2 70 9.6 80 8.1 95 7.8 100 6.7 100 5.3
MDR 7.3 50 9.2 65 8.4 80 7.4 95 7.0 100 6.0 100 4.8
MOR 10.9 50 8.7 65 7.9 80 6.9 90 6.4 100 5.7 100 4.5
MOR 14.5 50 8.2 65 7.4 80 6.5 90 6.0 100 5.4 100 4.3
HDR 24 50 6.7 65 6.1 75 5.1 90 4.9 95 4.3 100 3.5
HOR 43 50 5.3 65 4.7 75 4.0 85 3.8 95 3.4 100 2.7
N.Com 50 5.3 60 4.5 75 4.0 85 3.8 95 3.4 100 2.7
G.Com 50 4.7 60 4.1 75 3.6 85 3.4 90 2.9 100 2.4
O.P./Com 50 4.2 60 3.7 70 3.1 80 2.9 90 2.6 100 2.2
Limited I. 50 4.2 60 3.7 70 3.1 80 2.9 90 2.6 100 2.2
General I. 50 3.7 60 3.2 70 2.7 80 2.6 90 2.3 100 1.9
*See Table 3-1 for more detailed description
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APPENDIXC
Detention Facilities Calculations
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Required Detention:
The required retention for the site was determined from the San Diego County Hydrology
manual formula for volume as follows:
Where:
Volume = C*P6* A
Volume= volume of runoff (acre-inches)
P6 = 6-hour precipitation (inches)
C = delta of runoff coefficient
A = area of watershed
Volume= 0.03(2.8)(0.90) = 0.0756 acre-inches
Volume= 276 cubic feet of required detention .
Check of 85th Percentile rainfall volume:
=2.8
=0.03
=0.90
The 85th percentile volume (see 85th percentile calculations) has been calculated as follows:
Q=0.64 cfs
Duration of 10 minutes
Volume=Q*D
Volume=(0.64cfs)*(10 min)(60 sec)
V=384 cubic feet
Volume = 384 cubic feet of required detention .
,,,,. Using four 20-foot long, 30-inch CMP for storage. -Area of30-inch CMP = 4.91 square feet ...
..., A 20-foot section will yield 98 cubic feet
.., Four 20 foot sections will provide 392 cubic feet, which is more than what is required. We will
• have 1.02% storage capacity for detention .
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APPENDIXD
Pre-developed Hydro logic Calculations for the 100-Y ear Storm Event Onsite
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RATIONAL METHOD HYDROLOGY COMPUTER PROGRAM PACKAGE
Reference: SAN DIEGO COUNTY FLOOD CONTROL DISTRICT
2003 HYDROLOGY MANUAL
(c) Copyright 1982-2003 Advanced Engineering Software (aes)
Ver. 1.5A Release Date: 01/01/04 License ID 1462
FILE NAME: CBC.DAT
TIME/DATE OF STUDY: 16:22 5/18/2006
USER SPECIFIED HYDROLOGY AND HYDRAULIC MODEL INFORMATION:
2003 SAN DIEGO MANUAL CRITERIA
USER SPECIFIED STORM EVENT(YEAR) = 100.00
6-HOUR DURATION PRECIPITATION (INCHES) = 2.800
SPECIFIED MINIMUM PIPE SIZE(INCH) = 10.00
SPECIFIED PERCENT OF GRADIENTS(DECIMAL) TO USE FOR FRICTION SLOPE
SAN DIEGO HYDROLOGY MANUAL "C"-VALUES USED
NOTE: ONLY PEAK CONFLUENCE VALUES CONSIDERED
. 95
****************************************************************************
FLOW PROCESS FROM NODE 1. 00 TO NODE 2.00 IS CODE= 22
. . ----------------------------------------------------------------------------
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
=================================================================----=======
SOIL CLASSIFICATION IS "D"
RURAL DEVELOPMENT RUNOFF COEFFICIENT= .6700
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 3.230
*CAUTION: SUBAREA SLOPE EXCEEDS COUNTY NOMOGRAPH
DEFINITION .. EXTRAPOLATION OF NOMOGRAPH USED .
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) = 6.559
SUBAREA RUNOFF(CFS) = 4.90
TOTAL AREA(ACRES) = 1.12 TOTAL RUNOFF(CFS) 4.90
------------~---------------------------------------------------------------
END OF STUDY SUMMARY:
PEAK FLOW RATE(CFS) =
TOTAL AREA(ACRES) =
4.90
1. 12·
Tc (MIN.) = 6. 40
=============================================================-----==----=---
END OF RATIONAL METHOD ANALYSIS
(0.22 ACRES OF THIS RUN-OFF IS COMIMG FROM OFF-SITE, WHICH AMOUNTS TO A TOTAL
OF 0.96 CFS .
THEREFORE THE TOTAL RUN-OFF GENERATED FROM 0.90 ACRES IS 3.94 CFS.
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APPENDIXE
Developed Hydrologic Calculations for the 100-Year Storm Event
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****************************************************************************
RATIONAL METHOD HYDROLOGY COMPUTER PROGRAM PACKAGE
Reference: SAN DIEGO COUNTY FLOOD CONTROL DISTRICT
2003 HYDROLOGY MANUAL
(c) Copyright 1982-2003 Advanced Engineering Software (aes)
Ver. 1.5A Release Date: 01/01/04 License ID 1462
FILE NAME: CBCF.DAT
TIME/DATE OF STUDY: 16:36 5/18/2006
USER SPECIFIED HYDROLOGY AND HYDRAULIC MODEL INFORMATION:
1985 SAN DIEGO MANUAL CRITERIA
USER SPECIFIED STORM EVENT(YEAR) = 100.00
6-HOUR DURATION PRECIPITATION (INCHES) = 2.800
SPECIFIED MINIMUM PIPE SIZE(INCH) = 10.00
SPECIFIED PERCENT OF GRADIENTS(DECIMAL) TO USE FOR FRICTION SLOPE
SAN DIEGO HYDROLOGY MANUAL "C"-VALUES USED
NOTE: ONLY PEAK CONFLUENCE VALUES CONSIDERED
. 95
*****'***********************************************************************
FLOW PROCESS FROM NODE
AREA "A"
1.00 TO NODE 2.00 IS CODE= 21
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
SOIL CLASSIFICATION IS "D"
COMMERCIAL DEVELOPMENT RUNOFF COEFFICIENT= .7000
INITIAL SUBAREA FLOW-LENGTH= 170.00
UPSTREAM ELEVATION= 55.00
DOWNSTREAM ELEVATION= 19.50
ELEVATION DIFFERENCE= 35.50
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 2.131
*CAUTION: SUBAREA SLOPE EXCEEDS COUNTY NOMOGRAPH
DEFINITION. EXTRAPOLATION OF NOMOGRAPH USED .
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) = 6.559
SUBAREA RUNOFF(CFS) .58
TOTAL AREA(ACRES) = .13 TOTAL RUNOFF(CFS) .58
****************************************************************************
FLOW PROCESS FROM NODE 2.00 TO NODE 4.00 IS CODE=
>>>>>COMPUTE PIPEFLOW TRAVELTIME THRO SUBAREA<<<<<
>>>>>USING USER-SPECIFIED PIPESIZE<<<<<
4
============================================================----------===---
DEPTH OF FLOW IN 12.0 INCH PIPE IS 1.3 INCHES
PIPEFLOW VELOCITY(FEET/SEC.) 4.8
UPSTREAM NODE ELEVATION= 16.00
DOWNSTREAM NODE ELEVATION= 15.50
FLOWLENGTH(FEET) = 18.00 MANNING'S N = .011
GIVEN PIPE DIAMETER(INCH) = 18.00 NUMBER OF PIPES 1
PIPEFLOW THRU SUBAREA(CFS) .58
TRAVEL TIME(MIN.) = .06 TC(MIN.) = 6.06
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FLOW PROCESS FROM NODE
FLOW IN PIPE
4.00 TO NODE 4. 00 IS CODE =
>>>>>DESIGNATE INDEPENDENT STREAM FOR CONFLUENCE<<<<<
TOTAL NUMBER OF STREAMS= 3
CONFLUENCE VALUES USED FOR INDEPENDENT STREAM 1 ARE:
TIME OF CONCENTRATION(MIN.) 6.06
RAINFALL INTENSITY(INCH/HR) = 6.51
TOTAL STREAM AREA(ACRES) = .13
PEAK FLOW RATE (CFS) AT CONFLUENCE = . 58
1
****************************************************************************
FLOW PROCESS FROM NODE
AREA "B"
3.00 TO NODE 4.00 IS CODE= 21
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
--------------------.-------------------------------------------------------
SOIL CLASSIFICATION IS "D"
COMMERCIAL DEVELOPMENT RUNOFF COEFFICIENT= .7000
INITIAL SUBAREA FLOW-LENGTH= 235.00
UPSTREAM ELEVATION= 50.00
DOWNSTREAM ELEVATION= 19.50
ELEVATION DIFFERENCE= 30.50
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 2.936
*CAUTION: SUBAREA SLOPE EXCEEDS COUNTY NOMOGRAPH
DEFINITION. EXTRAPOLATION OF NOMOGRAPH USED.
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) 6.559
SUBAREA RUNOFF(CFS)
TOTAL AREA(ACRES) =
.38
.08 TOTAL RUNOFF(CFS) .38
****************************************************************************
FLOW PROCESS FROM NODE 4.00 TO NODE 4.00 IS CODE= 1
>>>>>DESIGNATE INDEPENDENT STREAM FOR CONFLUENCE<<<<<
=============================================================---------------
TOTAL NUMBER OF STREAMS= 3
CONFLUENCE VALUES USED FOR INDEPENDENT STREAM 2 ARE:
TIME OF CONCENTRATION(MIN.) 6.00
RAINFALL INTENSITY(INCH/HR) = 6.56
TOTAL STREAM AREA(ACRES) = .08
PEAK FLOW RATE(CFS) AT CONFLUENCE= .96
****************************************************************************
FLOW PROCESS FROM NODE
AREA "F" ROOF AREA
5.00 TO NODE 6.00 IS CODE= 21
----------------------------------------------------------------------------
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
================================================-=======--------------------
SOIL CLASSIFICATION IS "D"
INDUSTRIAL DEVELOPMENT RUNOFF COEFFICIENT= .8700 (DUE TO ROOF)
INITIAL SUBAREA FLOW-LENGTH= 140.00
,...
-
...
Ill
...
1111 -..
,.. -,,.. ..
...
,,,.
.. .. ..
-,..
-... ---...
,..
,.. ..
...
11111
UPSTREAM ELEVATION= 50.00
DOWNSTREAM ELEVATION 49.00
ELEVATION DIFFERENCE 1.00
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 3.574
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) = 6.559
SUBAREA RUNOFF(CFS) 1.65
TOTAL AREA(ACRES) = .29 TOTAL RUNOFF(CFS) 1.65
****************************************************************************
FLOW PROCESS FROM NODE
PIPE FLOW
6.00 TO NODE 4.00 IS CODE=
>>>>>COMPUTE PIPEFLOW TRAVELTIME THRU SUBAREA<<<<<
3
>>>>>USING COMPUTER-ESTIMATED PIPESIZE (NON-PRESSURE FLOW)<<<<<
ESTIMATED PIPE DIAMETER(INCH) INCREASED TO 10.000
DEPTH OF FLOW IN 10.0 INCH PIPE IS 1.8 INCHES
PIPEFLOW VELOCITY(FEET/SEC.) 9.2
UPSTREAM NODE ELEVATION= 16.00·
DOWNSTREAM NODE ELEVATION= 15.50
FLOWLENGTH(FEET) = 10.00 MANNING'S N .011
ESTIMATED PIPE DIAMETER(INCH) 10.00 NUMBER OF PIPES
PIPEFLOW THRU SUBAREA(CFS) 1.65
TMVEL TIME(MIN.) = .02 TC(MIN.) 6.02
1
****************************************************************************
FLOW PROCESS FROM NODE 4.00 TO NODE 4.00 IS CODE=
>>>>>DESIGNATE INDEPENDENT STREAM FOR CONFLUENCE<<<<<
>>>>>AND COMPUTE VARIOUS CONFLUENCED STREAM VALUES<<<<<
1
============================================================------===-------
TOTAL NUMBER OF STREAMS= 3
CONFLUENCE VALUES USED FOR INDEPENDENT STREAM 3 ARE:
TIME OF CONCENTRATION(MIN.) 6.02
RAINFALL INTENSITY(INCH/HR) = 6.55
TOTAL STREAM AREA(ACRES) = . 29
PEAK FLOW RATE(CFS) AT CONFLUENCE= 1.81
** CONFLUENCE DATA **
STREAM RUNOFF Tc INTENSITY
NUMBER (CFS) (MIN.) (INCH/HOUR)
1 .58 6.06 6.515
2 .38 6.00 6.559
3 1. 65 6.02 6.546
RAINFALL INTENSITY AND TIME OF CONCENTRATION
CONFLUENCE FORMULA USED FOR 3 STREAMS.
** PEAK FLOW RATE TABLE **
STREAM RUNOFF Tc INTENSITY
NUMBER (CFS) (MIN.) ( INCH/HOUR)
1 2.56 6.00 6.559
2 2.60 6.02 6.546
3 2.56 6.06 6.515
AREA
(ACRE)
.13
.08
.29
RATIO
,..
,.. ...
,.
111111
,,.
,,. .. --,,,. ...
...
....
,..
,.. ..
,,.
,,,. -.,.
-... ..
,..
,,,.
...
COMPUTED CONFLUENCE ESTIMATES ARE AS FOLLOWS:
PEAK FLOW RATE(CFS) 2.60 Tc(MIN.) = 6.02
TOTAL AREA(ACRES) = .50
****************************************************************************
FLOW PROCESS FROM NODE
PIPE FLOW
4.00 TO NODE 8.00 IS CODE=
>>>>>COMPUTE PIPEFLOW TRAVELTIME THRU SUBAREA<<<<<
3
>>>>>USING COMPUTER-ESTIMATED PIPESIZE (NON-PRESSURE FLOW)<<<<<
------------------==--------================================================
ESTIMATED PIPE DIAMETER(INCH) INCREASED TO 12.000
DEPTH OF FLOW IN 12.0 INCH PIPE IS 2.1 INCHES
PIPEFLOW VELOCITY(FEET/SEC.) 11.2
UPSTREAM NODE ELEVATION= 15.50
DOWNSTREAM NODE ELEVATION= 8.00
FLOWLENGTH(FEET) = 90.00 MANNING'S N .011
ESTIMATED PIPE DIAMETER(INCH) 10.00 NUMBER OF PIPES
PIPEFLOW THRU SUBAREA(CFS) 2.60
TRAVEL TIME(MIN.) = .13 TC(MIN.) 6.15
1
****************************************************************************
FLOW PROCESS FROM NODE 8.00 TO NODE 8.00 IS CODE= 1
>>>>>DESIGNATE INDEPENDENT STREAM FOR CONFLUENCE<<<<<
------------------=-=--.--------------==========-=========-=================
TOTAL NUMBER OF STREAMS= 2
CONFLUENCE VALUES USED FOR INDEPENDENT STREAM 1 ARE:
TIME OF CONCENTRATION(MIN.) 6.15
RAINFALL INTENSITY(INCH/HR) = 6.45
TOTAL STREAM AREA(ACRES) = .50
PEAK FLOW RATE(CFS) AT CONFLUENCE= 2.60
****************************************************************************
FLOW PROCESS FROM NODE
AREA "C"
7.00 TO NODE 8.00 IS CODE= 21
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
SOIL CLASSIFICATION IS "D"
COMMERCIAL DEVELOPMENT RUNOFF
INITIAL SUBAREA FLOW-LENGTH=
UPSTREAM ELEVATION= 38.00
COEFFICIENT
195.00
DOWNSTREAM ELEVATION= 10.25
ELEVATION DIFFERENCE= 27.75
.7000
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 2.593
*CAUTION: SUBAREA SLOPE EXCEEDS COUNTY NOMOGRAPH
DEFINITION. EXTRAPOLATION OF NOMOGRAPH USED.
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) = 6.559
SUBAREA RUNOFF(CFS) .35
TOTAL AREA(ACRES) = .11 TOTAL RUNOFF(CFS) .35
****************************************************************************
FLOW PROCESS FROM NODE 8.00 TO NODE 8.00 IS CODE= 1
>>>>>DESIGNATE INDEPENDENT STREAM FOR CONFLUENCE<<<<<
...
...
,,.
,..
,,. ..
..
,,. ...
,,,..
,,.
,,. -,,.
,,.
,,.
,..
,.. ..
...
,,. ...
,. ..
,. ..
>>>>>AND COMPUTE VARIOUS CONFLUENCED STREAM VALUES<<<<<
------------------==-=-=-==--=-----=-=======================================
TOTAL NUMBER OF STREAMS= 2
CONFLUENCE VALUES USED FOR INDEPENDENT STREAM 2 ARE:
TIME OF CONCENTRATION(MIN.) 6.00
RAINFALL INTENSITY(INCH/HR) = 6.56
TOTAL STREAM AREA(ACRES) = .11
PEAK FLOW RATE(CFS) AT CONFLUENCE= .59
** CONFLUENCE DATA**
STREAM RUNOFF
NUMBER (CFS)
1 2.60
2 .35
Tc
(MIN.)
6.15
6.00
RAINFALL INTENSITY AND TIME
CONFLUENCE FORMULA USED FOR
** PEAK FLOW RATE TABLE **
STREAM RUNOFF Tc
NUMBER (CFS) (MIN.)
1 2.91 6.00
2 2.94 6.15
OF
2
INTENSITY
(INCH/HOUR)
6.454
6.559
CONCENTRATION
STREAMS.
INTENSITY
(INCH/HOUR)
6.559
6.454
COMPUTED CONFLUENCE ESTIMATES ARE AS FOLLOWS:
PEAK FLOW RATE(CFS) 2.94 Tc(MIN.) =
TOTAL AREA(ACRES) = .61
AREA
(ACRE)
.50
.11
RATIO
6.15
****************************************************************************
FLOW PROCESS FROM NODE
PIPE FLOW
8.00 TO NODE 9.00 IS CODE=
>>>>>COMPUTE PIPEFLOW TRAVELTIME THRO SUBAREA<<<<<
3
>>>>>USING COMPUTER-ESTIMATED PIPESIZE (NON-PRESSURE FLOW)<<<<<
=============================-=-==================-==================--=-==-
ESTIMATED PIPE DIAMETER(INCH) INCREASED TO 12.000
DEPTH OF FLOW IN 12.0 INCH PIPE IS 2.1 INCHES
PIPEFLOW VELOCITY(FEET/SEC.) 27.4
UPSTREAM NODE ELEVATION= 7.50
DOWNSTREAM NODE ELEVATION= 7.00
FLOWLENGTH(FEET) = 5.00 MANNING'S N .011
ESTIMATED PIPE DIAMETER(INCH) 10.00 NUMBER OF PIPES 1
PIPEFLOW THRU SUBAREA(CFS) = 2.94
TRAVEL TIME(MIN.) = .00 TC(MIN.) 6.15
=============================-=-==-=-=-==-=-=-==----------------------------
END OF STUDY SUMMARY:
PEAK FLOW RATE(CFS) =
TOTAL AREA(ACRES) =
2.94
. 61
Tc(MIN.) = 6.15
=================================================--=-=-==-=-=-=-=-----------
END OF RATIONAL METHOD ANALYSIS
... ...
...
,,. ..
,,. -,,,, .. ..
-
,,.
,,. ..
,,,.
,,. -,,,. ..
,,.
,,. ..
,.. ...
,... ..
,,,.
****************************************************************************
RATIONAL METHOD HYDROLOGY COMPUTER PROGRAM PACKAGE
Reference: SAN DIEGO COUNTY FLOOD CONTROL DISTRICT
2003 HYDROLOGY MANUAL
(c) Copyright 1982-2003 Advanced Engineering Software (aes)
Ver. 1.5A Release Date: 01/01/04 License ID 1462
AREA "D"
FILE NAME: CBCF2.DAT
TIME/DATE OF STUDY: 16:38 5/18/2006
USER SPECIFIED HYDROLOGY AND HYDRAULIC MODEL INFORMATION:
1985 SAN DIEGO MANUAL CRITERIA
USER SPECIFIED STORM EVENT(YEAR) = 100.00
6-HOUR DURATION PRECIPITATION (INCHES)= 2.800
SPECIFIED MINIMUM PIPE SIZE(INCH) = 10.00
SPECIFIED PERCENT OF GRADIENTS(DECIMAL) TO USE FOR FRICTION SLOPE
SAN DIEGO HYDROLOGY MANUAL "C"-VALUES USED
NOTE: ONLY PEAK CONFLUENCE VALUES CONSIDERED
.95
****************************************************************************
FLOW PROCESS FROM NODE 10.00 TO NODE 11.00 IS CODE= 21
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
===================---------==--==========-=-----======-==--------------=---
SOIL CLASSIFICATION IS "D"
COMMERCIAL DEVELOPMENT RUNOFF COEFFICIENT= .7000
INITIAL SUBAREA FLOW-LENGTH= 290.00
UPSTREAM ELEVATION= 50.00
DOWNSTREAM ELEVATION= 6.00
ELEVATION DIFFERENCE= 44.00
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 3.096
*CAUTION: SUBAREA SLOPE EXCEEDS COUNTY NOMOGRAPH
DEFINITION. EXTRAPOLATION OF NOMOGRAPH USED.
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) = 6.559
SUBAREA RUNOFF(CFS) = 0.83
TOTAL AREA(ACRES) = .18 TOTAL RUNOFF(CFS) 0.83
========-======----------====----==---========----=====---------------------
END OF STUDY SUMMARY:
PEAK FLOW RATE(CFS) =
TOTAL AREA(ACRES) =
0.83
.18
Tc(MIN.) = 6.00
============================-=======----------------------------------------
END OF RATIONAL METHOD ANALYSIS
.,.
,,,.
,,.
,,.
,,.
~ --,.. ...
,..
.,.
,,.. ..
,..
,,,. -,..
....
,,. .
..
.. ,
****************************************************************************
RATIONAL METHOD HYDROLOGY COMPUTER PROGRAM PACKAGE
Reference: SAN DIEGO COUNTY FLOOD CONTROL DISTRICT
2003 HYDROLOGY MANUAL
(c) Copyright 1982-2003 Advanced Engineering Software (aes)
Ver. 1.5A Release Date: 01/01/04 License ID 1462
AREA "E"
FILE NAME: CBCF2.DAT
TIME/DATE OF STUDY: 16:38 5/18/2006
USER SPECIFIED HYDROLOGY AND HYDRAULIC MODEL INFORMATION:
1985 SAN DIEGO MANUAL CRITERIA
USER SPECIFIED STORM EVENT(YEAR) = 100.00
6-HOUR DURATION PRECIPJTATION (INCHES) = 2.800
SPECIFIED MINIMUM PIPE SIZE(INCH) = 10.00
SPECIFIED PERCENT OF GRADIENTS(DECIMAL) TO USE FOR FRICTION SLOPE
SAN DIEGO HYDROLOGY MANUAL "C"-VALUES USED
NOTE: ONLY PEAK CONFLUENCE VALUES CONSIDERED
. 95
****************************************************************************
FLOW PROCESS FROM NODE 12.00 TO NODE 13.00 IS CODE= 21
>>>>>RATIONAL METHOD INITIAL SUBAREA ANALYSIS<<<<<
SOIL CLASSIFICATION IS "D"
COMMERCIAL DEVELOPMENT RUNOFF COEFFICIENT= .6700 (50% OF AREA IS SAND)
INITIAL SUBAREA FLOW-LENGTH= 260.00
UPSTREAM ELEVATION= 11.00
DOWNSTREAM ELEVATION= 6.00
ELEVATION DIFFERENCE= 44.00
URBAN SUBAREA OVERLAND TIME OF FLOW(MINUTES) 3.096
*CAUTION: SUBAREA SLOPE EXCEEDS COUNTY NOMOGRAPH
DEFINITION. EXTRAPOLATION OF NOMOGRAPH USED.
TIME OF CONCENTRATION ASSUMED AS 6-MINUTES
100 YEAR RAINFALL INTENSITY(INCH/HOUR) = 6.559
SUBAREA RUNOFF(CFS) = 0.48
TOTAL AREA(ACRES) = .11 TOTAL RUNOFF(CFS) 0.48
-==-=-==========================================----------------------------
END OF STUDY SUMMARY:
PEAK FLOW RATE(CFS) =
TOTAL AREA(ACRES) =
0.51
.11
Tc(MIN.) = 6.00
=================================--==-=-------------------.-----------------
END OF RATIONAL METHOD ANALYSIS
,,,.
'-,,. ...
,,. ..
,. ..
,,. -,,.
.,
,,. ..
,,. ..
,..
...,
,,. ..
,,. ..
... ..
,.. ..
,,. ..
APPENDIXF
Hydraulic Calculations
,,,,.
,,. ...
,,. ... .. ...
,.. ..
,,,..
,,. .. ..
JIil
1111, ..
,.
,,.
,.,,.
....
..
,,. ...
. Carlsbad Boat Club
Onsite Drainage Calculations
The purpose of these calculations is to show that the two curb inlets along the westerly driveway
are adequately sized and will intercept the run off generated by a 100-year storm event. Below
are the calculations for the curb inlets .
The site is drained from the curb inlets via 12-inch and 10" SCH-40 PVC at slope that varies
between 2%and 2.6%. The pipe flow table below verifies that the proposed pipes carrying the
runoff can convey the flow generated by a 100-year event in open channel flow .
CURB INLET CALCULATIONS:
CHECK INLET LENGTH
SEE TABLE ON THE FOLLOWING PAGE FOR CURB INLET
LENGTH CALCULATIONS
Per figure 7-832.9A (following page) and using a flow of 0.58 cfs & a slope of 19% the required
inlet length is 3.5 feet. Use a standard curb inlet with an opening of 4.0 feet
PIPE FLOW CALCULATIONS:
CHECK PIPE FLOW
CIRCULAR PIPE CAP A CITY CHECK
DIAMETER No.OF MANNING FLOW DEPTH SLOPE VELOCITY
(ID PIPE U!l (cfs) (FT) (%) {FT/SEC)
1.0 1 0.011 0.58 0.21 2.00 4.83
l.0 1 0.011 2.60 0.46 2.00 7.33
0.83 1 0.011 l.65 0.32 2.60 7.22
RIP-RAP SIZING CALCULATIONS:
Per figure 19.7 (following pages) and using exit velocity of 7.33 fps the required rip-rap sizing
should be No. 2 backing rock approximately 1.0 feet thick with a l" aggregate base and filter
fabric
I
,,,.. .. }
Using a gutter depression and
intercepting the entire flow
Figure 7-832.9A
August. 1964
,,. ... NOTES
,,,.
,,. ...
,,.
....
,.. ...
..,
,,. ..
,..
... ...
... ...
,..
...
,,.
...
0.060
0.050
0.040
0.030
o.ozs
...,: ' LL 0.020
' -LL
I . o.o,s
Q)
-0
0 ,,_
(!) 0.010
,,_ 0.009
Q) -0.001 -:::J 0.007 (!)
0.001
0.005
0.004
0.003
0.002
0.3
.,,. -----··········--·-··-
'
..
.
m LEGEND
Solid Lines -• 0.10' gutter depression
Dash Lines --•0.251 gutter depression
L • Len(Jth of OpeninlJ
I
\ i \ \ l
1 \ , \ \\
I\ \ \\
\ \ I\ \ \,
\ _I I . \ \ 1----,\
~ \' \
\ 'I ·\
' \ '
\ \ \
i ~ ~· . a.
~ \\
\ .-\\
\ . \\ ~' \ ., \'
"· ' \ \
\ ' \
' \
\ \ \
\ \
\ ' \ . .
\ I' \ \
\
I \
CAUTION
This chart applies anly lo side apenings ·
.. paralleling the direction of th• intercepted flow
It is based on 1.s· percent pavement cross
slope and th~ gutter dtpressian cross slope as
shown in (Fig.7-832.IOA).
~ \ . ' I ., \
\ . . \
' \ ' .
\ .
\ ' .\ \ \
I
\ 1 '
1
\ ~ \· \
\ .
\ \\ ' \ .\ \ \
\ I ' -. ,, ' I .-. \ ~· \
\ { \ ~ ' l
\ \ \ . ' \
,
.. \ . \ \
,\ \ . \ \ r\ I""\
I"° I \
I"" -. • .. ' .\ -1 \ ~, q_\ -"! \ 1') -:
-~ ~\ . \J ' \ \,\
\ I f \ I ~
\ ' \ \ \ \ -~
\ \ . \ \ \ 1 I
\ \ \
l \ \ \ [
\ • , 1, I
!\ \ \ I ' \ \ . . . ' \ ' I \
\ \ ~ \ I . . .
\ I \ \
\ \ ' , \ \ .
' \
\
0.4 0.5 O.& 0.7 O.B 0.9 1.0 '·' 2.0 Z.5 3.0 4.0 5.0 6.0 8.0 10.0
Capacity -Cubic Feet per Second
,,. -,,,..
_,
,,. -,,. -,,,. -,,. ...
..
,,.
....
,.. ... ..
,,,. ...
,,,. ... -
,,.
....
,,.
,,. ..
,-
r
-------------..
·-.
,-~FROM:
5PE'ClA.L PROV /51 ON.S
·~ l<EG,loMAL STD. SPECS.
( 1902)
200-1 .6 S-tone for Rtorap (p. 69)
Add: "The lndlvldual classes of rocks used In s)ope
protection shall conform to the followlng:
PERCENTAGE LARG::R n-lAN*
CI.AS~ES
Rock 1/2 1/4 No. 2 No. 3
Sl;zes 2 Ton 1 Ton Ton Ton Backing Backing
,
4 Ton 0-5
2 Ton 50-100 o-s ..
1 Ton 95-100 50-100 0-5 ,
1 /2 Ton --50-100 0-5
1/4 Ton 95-100 --50-100
200 lb 95-100 -· 75 lb 95-100 0-5
25 lb 25-75 o-5
5 lb 90-100 25-7~f
1 lb 90-100
*The amount of material smaller than the smallest
s1:ze-lls-ted In the table for any class of rock slope
protec-tlon shall not exceed the percentage llmlt
1 ls-ted In the table determined on a weight basis.
Compl lance with the percentage I lmlt shown In the
+able tor all other sizes of the lndlvtdual pieces
of any class of rock slope protec-tlon shall be de-
termined by the ratio of the number of lndlvldual
pieces larger than the smalles-t size lls-ted In the
table for that class.
•200-1.6.t Selectlon of Rlprao and FIiter
Blanket Material
Fl lter Blanket (3)
Upper Layer(s)
Opt. 1 Opt. 2
Vel. Rock Rlprap Sec. Sec.
Ft/Sec Class Thick-200 400 Opt. 3
( I) (2) ness "T" {4) (4) (5)
No. 3
Back-
6-7 Ing .6 3/16" C2 D.G.
No. 2
Back-
7-8 Ing: 1.0 1/4" BJ D.G.
Fae-
8-9.5 Ing 1 .4 3/8" --O.G. -
3/4", 1 1/2"
9.5-11 Light 2.0 1/2" -P.a.
3/4",
1/4 1 1/.2"
11-t.3 Ton 2.7 3/4" -P.a.
·, ,. 3/4", 1/2 1 1/2"
13-15 Ton J.4 1" -P.B.
15-17 1 Ton 4.3 1 1/2" -Type B
17-20 2 Ton ~ 5. 4 2" Type B -
Lower
Layer
(6)
-
-
-
-
Sand
Sand
Sand
Sand
Practical use of this table Is limited to sltua-tlons
'tlhere "T" Is less than O.
Cl) Average velocity In pipe or bottom velocity In
energy dissipater, .'tlhlc:hever ls greater •.
(2) if d:tslre-d ,:lprap and filter blanket class ls
not avallable, use next larger class. --. --.... -. -
' t.
(3) FIiter-blanket thickness" I Foat er "T", which-.
ever Is less.
(4) ~tandard Specifications for.Public Works Con-
struction •
(5.) . O.G. =-.Dlsl-n-tegrated Granite, 1 M-1 to 10 M-1
P.a.= Processed"Mlscellaneous Base-
Type B ,. Type. B be-dd Ing mater I a I , <m In llnum 75%,
crushed particles, 100% passing 2 1/2" sieve,
10% passing t" sieve)
(6) Sand 75% retained on 1200 sieve •
FIGURE _J.-9.7
III.304
,,. ...
,,.. 20 or 'l-H (min.)
"-· End-Mil (typ.)
,,..-.. --ti.
,,,. ...
,.. ...
,,. ... -...
,..
....
,,.
--..
--,,. -,,,. -,,,. ...
.,..
....
,,. ...
··= ·e =
.. Cl
Q N
fa
B
6' .. widl slot
PLAN
. . . ~ . . . . . . .. : ..
Concntl
Chann•IJ . □ or W "' ,:," ½
l ~.
2D ar '1W
SECTION B-8
1
minJ
a • Pipt Oiamtttr
W • Bonam Width at Channel
.ST (min.)
Flow ·
Filter Blank.at
Sill, Class 420-C-2000
Concnta
SECTION A-A
;NOTES::
'1. Plans shall specify:
A) Reick class and thickness m.
Bl Filter mat1ri1I. number of layers and thickness.
2. Rip ,:ap shall be either quarry stone or broken concn,u
(if shown on th11 plans.) Cobbles are not. acaptable. ·
3. Rip r1p shall be •placed over a_ filter blanket which
mav be tither-gr1nular maurial or plasti_c filt1r cloth.
4. SN standard spacial provisions for salection of rip r.ap
l!ld filtar blanket. .
5. Rip rap energy dissipaters shall be designated as either
Tvllt 1 or Type 2. Type 1 shall be with concma sill:
Type 2 shall bl without sill.
,. r---~--r--____ F_l_G_U_R_E_~I 9_._G _____ ., _ __...----'
' Revision By . Approved Data Ila, MCO-IIID(D IY TN( SAIi DIEGO I' HGIOIIAL ST ~OAIIDS CDl&IIITTH
ae../t7 .IS-fJ "'1.c. m~
: 1---t_-_ ....... _,._Mr_r_,,._, __ o-_~ RIP RAP
~~~~~is D-40.1 ENERGY DISSJPATOR
,,.------------'-------'--III.303
SAN DIEGO REGIONAL STANDARD DRAWING Sill, ·mtar 1'(,d.
,,. -
,,. -
,.. ...
,.. -,,.
....
,.. ..
,,. ..
,,..
....
,,.. -,,,,.
.... ..
,,,. ..
APPENDIXG
ssth Percentile Calculations
,,.
,.
,..
,,...
,.. -,.
-,.
,. -... ...
,,.. ...
,,..
..
...
,,,.
San Diego County Hydrology Manual
Date: June 2003
3.1.3 Rainfall Intensity
Section:
Page:
3
7 of26
The rainfall intensity (I) is the rainfall in inches per hour (in/hr) for a duration equal to the Tc
for a selected storm frequency. Once a particular storm frequency has been selected for
design and a Tc calculated for the drainage area, the rainfall intensity can be determined from
the Intensity-Duration Design Chart (Figure 3-1). The 6-hour storm rainfall amount (P6) and
the 24-hour storm rainfall amount (P24) for the selected storm frequency are also needed for
calculation of I. P6 and P24 can be read from the isopluvial maps provided in Appendix B.
An Intensity-Duration Design Chart applicable to all areas within San Diego County is
provided as Figure 3-1. Figure 3-2 provides an example of use of the Intensity-Duration
Design Chart. Intensity can also be calculated using the following equation:
I = 7.44 p 6 ffo.645
Where: P6 = adjusted 6-hour storm rainfall amount (see discussion below)
D = duration in minutes (use Tc)
Note: This equation applies only to the 6-hour storm rainfall amount (i.e., P6 cannot be
changed to P24 to calculate a 24-hour intensity using this equation) .
The Intensity-Duration Design Chart and the equation are for the 6-hour storm rainfall
amount. In general, P6 for the selected frequency should be between 45% and 65% of P24 for
the selected frequency. If P6 is not within 45% to 65% of P24, P6 should be increased or
decreased as necessary to meet this criteria. The isopluvial lines are based on precipitation
gauge data. At the time that the isopluvial lines were created, the majority of precipitation
gauges in San Diego County were read daily, and these. readings yielded 24-hour
precipitation data. Some 6-hour data were available from the few recording gauges
distributed throughout the County at that time; however, some 6-hour data were extrapolated.
Therefore, the 24-hour precipitation data for San Diego County are considered to be more
reliable .
3-7
,,.
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85th PERTENTILE FLOWS
The chart is included in this report, immediately following this page. The isopluvial for the site
has a "P" value of 0.60 inches per hour (in/hr) for a storm. Flow for the 85th percentile storm
would amount to:
1=7 .44(P)(D )"-0645
Where: !=Intensity
P=0.60
D= 10 minutes
1=7.44(06.0)(10)"-0.645
I=l.01 in/hr
Q=C*I*A
Where: C=0.70
I=l.01
A=0.90
Q=(0. 70)*(1.0l )*(0.90)
Q=0.64 cfs
The run-off generated from the 85th percentile storm will be treated by three mechanical
methods:
1) Roof drains will be passed through a mechanical cleaning device to remove organics and
hydrocarbons .
2) The run-off generated on the paved surfaces and landscape areas will pass through a
gravel and sand filter before entering the curb inlet.
3) Run-off that has been filtered will then proceed through the storm drain system and be
allowed to settle and have additional filtration before discharging into the lagoon .
'.
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.HICH POINT-· 55
. LOW POINT -19.5
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AREA "B"
HIGH POINT -50
L0/11 POINT -19.6.
ACRES -0.08 --------
0100 = 0.38 CFS
AREA 'c"
HICH POINT -38
L0/11 POINT -10.25
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0 100 = 0.35 CFS
AREA "!J"
HICH POINT -. 50
l0/11 POINT -6
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AREA-'t"
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ACRES -0.29
0 1oo = 1.65 CFS
(jJ NOOE NUMBER
· POS T-OEV£L OPM£N T
ORA/NAG£ AREA MAP
20 40 . 60 80