HomeMy WebLinkAboutPD 07-02; KAWANO RESIDENCE; HYDROLOGY CALCULATIONS FOR KAWANO RESIDENCE; 2007-03-06II
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HYDROLOGY CALCULATIONS S
For
KAWANO RESIDENCE 44 'j 7g-
APN: 205-220-54-00
CITY OF CARLSBAD, CALIFORNIA
Prepared For
Gary & Allison Kawano
3690 Highland Drive
Carlsbad, CA 92008
PE 1544
PREPARED BY:
PASCO ENGINEERING, INC.
535 N. HIGHWAY 101, SUITE A
SOLANA BEACH, CA 92075
(858)259-8212
DATE: 01-09-06
REVISED: 3-6-07
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Hydrology Study for Kawano Residence
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TABLE OF CONTENTS
SECTION
DISCUSSION...............................................................................A
CONCLUSION..............................................................................B
PRE-CONSTRUCTION 100 YEAR HYDROLOGY CALCULATIONS :........0
POST-CONSTRUCTION 100 YEAR HYDROLOGY CALCULATIONS .......D
APPENDIX..................................................................................E
Sub-basin 3 Volume Calculation
Sub-basin 3 Velocity Calculation
Sub-basin 4 Volume Calculation
Isopluvials
Intensity Duration Curve
SCS Soil Classification
Delineated Drainage Map
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A. INTRODUCTION
The purpose of this report is to analyze the storm water runoff produced from the 100
year storm event of the developed site on Highland Drive. The subject property is
physically located at 3690 Highland Drive, Carlsbad California. The property is
geographically located at N 33009'00" W 117019'00".
Pre-Developed Conditions
The existing condition of the project site consists of an existing house at 3690 Highland
Drive. A detached driveway off Highland Drive allows for access to the residence. The
site is surrounded by single family residences to the north and east. The western
boundary is Highland Drive and along the south is Magnolia Avenue. The site is
characterized .by a ridge running in the north south direction. Rainfall collected on the
eastern portion of the site flows towards the eastern boundary of the site. Runoff in the
eastern portion of the property then sheet flows over the eastern property line. Rainfall
collected in the western portion of the site generally sheet flows in a westerly direction
where runoff ultimately sheet flows over Highland Drive away from the project site. The
highpoint of the site occurs near the existing residence at an elevation of 175.0'. The low
point occurs along Highland Drive near the north west portion of the site at an elevation
of 168.6'.
The total volume generated by the site in its existing condition is 0.75 cfs. The
calculations for this volume can be seen in the section C of this report.
Post- Development Conditions
The proposed development consists of the construction of a detached garage with guest
residence above. Runoff from the site will flow in the same general manner as in the pre-
development condition of the site. Runoff collected in the western portion of the site will
continue to flow to the west and runoff collected in the eastern -portion of the site will
continue to flow to the east.
For the post-development analysis the site was divided into five drainage sub-basins.
Runoff generated in sub-basins 1, 2, and 5 do not increase impervious surface and as a
result do not contribute to the increase in runoff. Sub-basin 3 collects runoff from a
portion of the roof and rain that falls in the rear of the proposed structure. Runoff
collected in this sub-basin travels over grass BMP from the rear of the structure to. the
front of the structure and discharges along Highland Drive. The total flow for this area
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was determined to be 0.24 cfs with a maximum velocity of 3.22 fs. The calculations for
this volume and velocity can be seen in the appendix, sheet 1 and 2, respectfully.
Sub-basin 4 collects runoff from a portion of the roof and from the proposed driveway.
This runoff is then directed to flow towards and over grass BMP strips located at the ends
of the proposed driveway. The volume for this sub-basin was found to be 0.25 cfs. The
calculations for this volume can be seen in the appendix, sheet 6.
The total volume generated by the site in its post-construction condition is 0.78 cfs. The
calculations for this volume can be seen in section D of this report
Drainage patterns in the eastern portion of the site will not be affected by the proposed
structure and therefore not analyzed as part of this hydrology report. A detailed map
illustrating the delineated drainage basins has been included in this report.
Methodology and Results
Introduction
The hydrologic model used to perform the hydrologic analysis presented in this report
utilizes the Ration Method (RM) equation, Q=CIA. The RM formula estimates the peak
rate of runoff based on the variables of area, runoff coefficient, and rainfall intensity.
The rainfall intensity (I) is equal to:
I = 7.44 x P6 x
Where:
I = Intensity (in/hr)
P6 = 6-hour precipitation (inches)
D = duration (minutes - use Tc)
Using the Time of Concentration (Tc), which is the time required for a given element of
water that originates at the most remote point of the basin being analyzed to reach the
point at which the runoff from the basin is being analyzed. The RM equation determines
the storm water runoff rate (Q) for a given basin in terms of flow (typically in cubic feet
per second (cfs) but sometimes as gallons per minute (gpm)). The RM equation is as
follows:
Q=CIA
Where:
Q= flow (in cfs)
C = runoff coefficient, ratio of rainfall that produces storm water
runoff (runoff vs. infiltration/evaporation/absorption/etc)
I = average rainfall intensity for a duration equal to the Tc for the
area, in inches per hour.
A = drainage area contributing to the basin in acres.
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The RM equation assumes that the storm event being analyzed delivers precipitation to
the entire basin uniformly, and therefore the peak discharge rate will occur when a
raindrop that falls at the most remote portion of the basin arrives at the point of analysis.
The RM also assumes that the fraction of rainfall that becomes runoff or the runoff
coefficient C is not affected by the storm intensity, I, or the precipitation zone number.
The hydrologic soil group classification for the site is "D". The methodology used herein
to determine Qioo is the modified rational method. The computer modeling program
utilized to perform the hydrologic analysis of the proposed project site is produced by
Advanced Engineering Software (AES2003).
The pre and post-development runoff coefficients, used to analyze the both conditions,
were determined by using weighted "C" average.
C= 0.90 x (% impervious) + Cp x (1-%impervious)
Where:
Cp = pervious surface runoff coefficient (varies depending on soil type from
0.2 to 0.35 - since analysis assumes type d soils Cp =0.35)
For the proposed development the runoff coefficient utilized for the hydrologic analysis
of sub-basin 3 is 0.60, based on 45% impervious surface. For sub-basin 4 the runoff
coefficient was determined to be 0.86 based on 94% impervious surface.
B. CONCLUSION
Based on the information and calculations contained in this report it is the professional
opinion of Pasco Engineering, Inc. that the proposed method of capturing and conveying
the runoff on the corresponding Grading Plan will function to adequately convey Qioo to
the appropriate points of discharge. In addition, the proposed drainage will not have an
adverse affect on adjacent properties or downstream drainage facilities.
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C. PRE- CONSTRUCTION 100 YEAR HYDROLOGY CALCULATIONS
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Pre-construction Runoff Volume Calculation
This calculation represents the total volume of runoff from
the entire western portion of the project site (sub-basins 1-4).
-Assumptions:
P6=2.6
Duration, Time of Concentration (D,Tc)= 5 minutes
-Area = 9,760 sf or 0.22 ac
Impervious surface = 2,630 sf
Pervious Surface = 7,130 sf
-Runoff Coefficient, C
C, Impervious = 0.90
C, Pervious = 0.35
C = (2,630)(0.90)+(7.130)(0.35) = 0.498
9,760
-Intensity, I
I = 7.44xP6xD"-0.645
I = 7.44x2.6x5"-0.645 = 6.85
Q=CIA
Q = 0.498x6.85x0.22 = 0.75 cfs
Hydrology Study for Kawano Residence
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D. POST-CONSTRUCTION 100 YEAR HYDROLOGY CALCULATIONS
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Post-construction Runoff Volume Calculation
This calculation represents the total volume of runoff from
the entire western portion of the project site (sub-basins 1-4).
-Assumptions:
P6=2.6
Duration, Time of Concentration (D,Tc)= 5 minutes
-Area = 9,760 sf or 0.22 ac
Impervious surface =2,935 sf
Pervious Surface = 6,825 sf
-Runoff Coefficient, C
C, Impervious = 0.90
C, Pervious = 0.35
C = (2.935)(0.90+(6.825)(0.35) = 0.515
9,760
-Intensity. I
I = 7.44xP6xD"-0.645
I = 7.44x2.6x5^-0.645 = 6.85
Q=CIA
Q = 0.515x6.85x0.22 0.78 cfs
Hydrology Study for Kawano Residence
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E. APPENDIX
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Q = 0.60x6.85x0.059
Sub-basin 3 Runoff Volume Calculation
-Assumptions:
P6=2.6
Duration, Time of Concentration (D,Tc)= 5 minutes
-Area = 2,593 sf or 0.059 ac
Impervious surface = 1,175 sf
Pervious Surface = 1,418 sf
-Runoff Coefficient, C
C, Impervious = 0.90
C, Pervious = 0.35
C =(1,175)(0.90)+(1.418)(0.35) = 0.60
2,593
-Intensity, I
I = 7.44xP6xDA0.645
I = 7.44x2.6x5"-0.645 = 6.85
Q=CIA
Kawano Velocity
Worksheet for Triangular Channel
Project Description
Project File n:\haested\academicfmw\1544.fm2
Worksheet Kawano
Flow Element Triangular Channel
Method Manning's Formula
Solve For Discharge
Input Data
Mannings Coefficient 0.013
Channel Slope 0.043000 ft/ft
Depth 0.10 ft
Left Side Slope 50.000000 H : V
Right Side Slope 100.000000 H: V
Results
Discharge 2.41 cfs
Flow Area 0.75 ft2
Wetted Perimeter 15.00 ft
Top Width 15.00 ft
Critical Depth 0.15 ft
Critical Slope 0.005906 ft/ft
Velocity 3.22 ft/s
Velocity Head 0.16 ft
Specific Energy 0.26 ft
Froude Number 2.54
Flow is supercritical.
02/14/07 Academic Edition FlowMaster v5.17
03:44:24 PM Haestad Methods, Inc. 37 Brookside Road Waterbury, CT 06708 (203) 755-1686 Page 1 of 1
Sub-basin 4 Runoff Volume Calculation
-Assumptions:
P6=2.6
Duration, Time of Concentration (D,Tc)= 5 minutes
-Area = 1,900 sf or 0.043 ac
Impervious surface = 1,780 sf
Pervious Surface = 120 sf
-Runoff Coefficient, C
C, Impervious = 0.90
C, Pervious = 0.35
C = (1,780)(0.90)+(120)(0.35) = 0.86
1,900
-Intensity, I
I = 7.44xP6xD"-0.645
I = 7.44x2.6x5"-0.645 = 6.85
Q=CIA
Q = 0.86x6.85x0.043 = 0.25 cfs
San Diego County Hydrology Manual Section: 3
Date: June 2003 Page: 6 of 26
Table 3-1
RUNOFF COEFFICIENTS FOR URBAN AREAS
Land Use I Runoff Coefficient "C"
Soil Type
NRCS Elements Elements A 13 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 (LDR) Residential, 2.0 DU/A or 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 bU/A or less 50 0.55 0.58 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 (1-IDR) Residential, 43.0 DU/A or less. 80 0.76 0.77 0.78 . 0.79
Commercial/Industrial (N. Corn) Neighborhood Commercial 80 . 0.76 0.71 0.78 0.79
Commercial/Industrial (G. Corn) General Commercial . . 85 0.80 0.80 0.81 0.82
Commercial/Industrial (O.P. Corn) Office Professional/Commercial 90 0.83 0.84 0.84 0.85
Commercial/Industrial (Limited I.) Limited Industrial 90 0.83 0.84 0.84 0.85
Commercial/Industrial (General 1.) GeneraL Industrial 95 0.87 0.87 0.87 0.87
The values associated with 0% impervious may be used for 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. Justification must be given that the area will rernain natural forever (e.g., the area
is located in Cleveland National Forest).
DU/A = dwelling units per acre
NRCS National Resources Conservation Service
3-6