HomeMy WebLinkAboutRiverlakes Park - Drainage StudyW.O. 156-09
DRAINAGE STUDY
For
Riverlakes Community Park
Bakersfield, CA
Prepared for:
North of the River Recreation and Park District
405 Galaxy Avenue
Bakersfield, CA 93308
June 13, 2011
Revised October 21, 2011
Tory R. Walker, R.C.E. 45005
President
122 Civic Center Drive, Suite 206, Vista, CA 92084 Ph: 760.414.9212 Fx: 760.414.9277 www.Trwengineering.Com
Addendum to Drainage Study Report
October 21, 2011
Mr. Manny Behl
City of Bakersfield Public Works Dept.
Bakersfield, CA 93301
Re: Drainage Study Report Addendum, in Response to City Comment Letter Dated
August 11, 2011.
Dear Manny:
We are writing to summarize corrections and agreements made with you on the drainage
study comments dated August 11, 2011. We are also supplementing those comments with
supporting calculations for the retention basin (sump) changes made on October 18.
1. We have signed the drainage study, with a copy emailed to you, including this
addendum.
2. Through email correspondence of 9-20-11, and phone conversation on same day, the
area-wide study is not required, and it was noted that the runoff contribution from our
project (0.49 acres into 342 acres) is insignificant and produces no HGL increase
above Bakersfield standards.
3. C-value verification was provided and approved via phone. Copy provided with this
addendum.
4. Overflow storm drain will be removed from project drawings.
5. The sump (retention basin) will be fenced - to be added to project drawings.
6. One sump is acceptable, with the note "City of Bakersfield not responsible for
maintenance. North of the River Parks and Recreation Dept. will provide
maintenance."
7. A change to the depth of basin was not required , no additional borings or revisions
needed. The City will issue a conditional letter of approval that will note
recommendations on the basin. Note - the basin bottom was lowered to elevation
390.0 with the October 18 change. This improves the drawdown ability of the basin.
October 18, 2011 Update to Detention Basin:
The detention basin (sump) configuration and bottom elevation was revised due to request by
the North of the River Parks and Recreation Department. The following facts apply to the
revised basin and potential changes to the drainage report needed:
Referring to the proposed conditions hydrology map - Subarea E (0.38AC) is unchanged from
previous. The entire area is landscaped and drains into the modified retention basin.
The inflow hydrographs calculations in the Appendix C, (Retention Basin Calculations) are
unchanged, as none of the inflow hydrographs are in need of revision. The interim basin
calculations (hydrograph # 2) for both 10-year and 100-year have been rerun with the updated
pond and hydrograph report provided directly following this section of addendum
letter/report. Note the 100-year water surface is at 394.8, and the 10-year water surface is
now at 390.44 (was 392.16 previously). Freeboard is provided for the basin perimeter at one
foot above the water surface elevation (minimum).
Pipeflow Changes:
The 10-year criteria is unchanged from previous for the revised storm drains entering the
basin (two). The lower reach of each pipe has lengthened, with the invert elevation at the
outlet over 1.5 feet deeper. See pipeflow check for these revised reaches directly following
the hydrograph calculations in this letter addendum.
Thank You,
TORY R. WALKER ENGINEERING, INC.
Tory R. Walker, P.E.
President
DRAINAGE STUDY REPORT
Riverlakes Community Park
Page 1
Introduction
The proposed Riverlakes Community Park is located in NW Bakersfield, north of
Highway 58, East of Highway 99, and just northeast of the Friant-Kern Canal.
Riverlakes Drive and Coffee Road are the major roadways to the north and east of the
project. The project location is shown in Figure 1. The total park project area is
approximately 27 acres, and the site is currently vacant. The Riverlakes Community
Park is the first phase of the total park project. The proposed community center will
include a central building and extensive landscaping/park area. The first phase will
develop approximately 7 acres of the site for the community center and park, while the
remaining 20 acres will be developed at a later time, possibly as a water park. The
existing topography is relatively flat, with the highest elevations at the northeast and
northwest portions of the site around elevation 397 feet, sloping to the southeast and
southwest corners of the site, to an approximate elevation of 393 feet.
This drainage report is intended to supplement the grading plan submittal to be
reviewed by City staff. The purpose is to identify drainage basin areas, calculate peak
flow rates, and size a retention basin to meet the City’s drainage design standards.
Methodology
City of Bakersfield methods are employed in the calculations for runoff and retention.
Chapter 2.1 of the City of Bakersfield Standards for Drainage provides the design
guidelines and data. Methods for calculating runoff coefficients, times-of-concentration,
and frequency-year storm events are all described in that manual. The project site area
is less than one square mile, therefore the 10-year frequency recurrence interval storm
is used to for runoff calculations. For the retention basin on the site, the storage
volume needed is based on the 100-year 24-hour storm, and the volume is based on
average runoff coefficient and total tributary drainage area. The needed volumes, in
acre-feet, are noted in the retention basin calculation section of this report, with
supporting methodology in the appendices.
DRAINAGE STUDY REPORT
Riverlakes Community Park
Page 2
Figure 1. Project Location Map (No Scale)
Proposed Development Runoff Patterns and Storm Drain Design
The proposed development has been divided into drainage basin areas, designated as
A through M on the Hydrology Map, which is attached in Appendix A. Runoff from the
drainage areas is discharged to the proposed retention basin, with a small portion of the
site entrance draining to Riverlakes Road. In addition to the 7 acres of onsite area, 1.4
acres of offsite area from the Friant-Kern Canal drains onto the site from the west, and
N
Project Location
DRAINAGE STUDY REPORT
Riverlakes Community Park
Page 3
6.2 acres of offsite area drains towards the site from the south. The drainage from the
west is a permanent condition, while the drainage from the south is a temporary
condition until the remainder of the park parcel is developed. When the remainder of
the park is developed, the runoff from the 6.2 acre offsite area (M on the attached map)
will be routed to a separate offsite retention basin. A summary of areas is shown in
Table 1, below.
Table 1. Summary of Drainage Subareas
Subarea Drainage
Area (ac)
C
Value Drain Location Retention
Vol. (ac-ft)
A 0.49 0.36 Offsite (Riverlakes Rd) N/A
B to L 7.56 0.52 Retention Basin 0.589
M (Interim) 6.22 0.10 Retention Basin 0.093
M (Ultimate) 6.22 N/A Offsite N/A
Interim Total (B to M) 13.78 0.68
Ultimate Total (B to L) 7.56 0.59
Storm drains at the site will be constructed using HDPE storm drain pipe, or similar,
since the site gradient will require relatively flat, shallow, pipes. Storm drain
calculations at the site were prepared using the Hydraflow Storm Sewers Extension
from Autodesk. Hydraflow calculates runoff using the Rational Method and also
calculates the HGL in the storm drain pipes. The drainage system was designed so
that there was at least 0.5 feet of freeboard at each catch basin during a 10-year storm.
The Hydraflow results are attached in Appendix B. The calculations were prepared for
the storm drain system that drains the parking lot. The laterals draining the park were
modeled as two discharge points into the trunk system. The starting water surface in
the storm drain was set at normal depth, since for a 10-year storm, the water surface in
the basin never exceeds 0.2 feet (See Retention Basin calculations for 10-year storm).
Retention Basin Design
A site-specific permeability test was performed to determine the capability of the soils at
the site to drain within the required one week time period. Two borings were taken from
the retention basin location. The measured percolation rates for the retention basin
were 10.0 and 4.5 inches per hour. The design permeability of 2.4 inches per hour was
determined by adjusting the average of the measured rates (7.25 in/hr) by a factor of
safety. A factor of safety of 3.0 was used to account for reduction in permeability over
time, as silt might collect in the basin between maintenance activities.
DRAINAGE STUDY REPORT
Riverlakes Community Park
Page 4
Hydraflow Hydrographs Extension from Autodesk was used to size the retention basin.
The inflow hydrograph was determined using the 100-year 24-hour precipitation total of
2.8 inches from the NOAA Atlas. A Type I SCS storm was used for the hydrograph,
and the curve numbers for the interim and ultimate conditions were adjusted so the total
inflow volumes were equal to the volumes from the Rational Method approach, as listed
in Table 1.
Outflow hydrographs were determined in Hydraflow Hydrographs using the geometry of
the basin and the design percolation rate of 2.4 inches per hour. For the interim
condition when Subarea M drains to the retention basin, a maximum depth of 0.98 feet
was calculated for the 100-year 24-hour storm. For the ultimate condition, when
Subarea M is routed to a different location, the maximum basin depth is 0.89 feet for
the 100-year 24-hour storm. In both the interim and ultimate conditions, the basins will
drain within 12 hours of the end of the 24-hour SCS design storm. The results are
summarized in Table 2 and the output from Hydraflow Hydrographs, for the 10-year and
100-year storms, is included in Appendix C.
Table 2. Summary of Retention Analysis
Condition Drainage
Area (ac) CN Value*
Inflow
Volume
(ac-ft)
Max
Elevation
(ft)
Max Stage
(ft)
Interim 13.78 70.5 0.70 392.98 0.98
Ultimate 7.56 77.5 0.59 392.89 0.89
(*) Note: CN Adjusted so inflow volume matches Rational Method volume in Table 1.
To allow maximum use of the retention basin area for the park, we have designed the
basin so that the depth for a 100-year storm is less than 18 inches. Since the total
basin depth is approximately 4 feet, we are proposing an overflow storm drain
connection from the retention basin to the existing storm drain in Riverlakes Drive.
While the project area was not included in the Riverlakes Area Drainage Plan (ADP),
the storm drain between the site and the sump north of Hageman Road has a minimum
of 2.1 feet of freeboard and a maximum of 12 feet of freeboard. This site would only be
draining to the storm drain under the worst case scenario of the basin not being
maintained and severe storms occurring back to back. The basin is in a prominent
location next to the community center, so it is anticipated that it will be well maintained
by the Parks District staff, making the probability of an overflow to the storm drain very
low. Even if the site did spill, there is capacity in the Riverlakes storm drain to handle
the additional runoff for a single event until the permeability of the basin can be
restored. Excerpts from the ADP are included in Appendix D.
DRAINAGE STUDY REPORT
Riverlakes Community Park
Page 5
Conclusion
The project storm drains and retention basin have been designed to meet City of
Bakersfield standards for the conservative case of the interim condition. When the full
park parcel is developed, the performance of the retention basin and storm drain will
improve, since 6.2 acres of tributary area will no longer contribute to this drainage
system.
DRAINAGE STUDY REPORT
Riverlakes Community Park
Appendix A: HYDROLOGY MAPS
Existing Condition Topography Map
Proposed Condition Hydrology Map
DRAINAGE STUDY REPORT
Riverlakes Community Park
APPENDIX B: RATIONAL METHOD AND
HGL CALCULATIONS
123
45
6
7
8
9
10
11
12
13Outfall
Riverlakes Community CenterProject File: Riverlakes SD.stm
Number of lines: 13Date: 06-09-2011Hydraflow Storm Sewers Extension v6.052
Storm Sewer Inventory Report
Page 1
LineAlignmentFlow Data
Physical Data
Line ID
No.
DnstrLineDeflJuncKnownDrngRunoffInletInvertLineInvertLineLineNJ-lossInlet/linelengthangletypeQareacoefftimeEl DnslopeEl Upsiz
eshapevaluecoeffRim ElNo.(ft)(deg)(cfs)(ac)(C)(min)(ft)(%)(ft)(in)(n)(K)(ft)
1End25.3000.000MH0.000.000.000.092.000.5192.1318Cir
0.0131.0095.802123.0000.000MH0.000.000.000.092.130.3992.2218Cir0.
0131.0095.80
3295.9000.000MH0.000.000.000.092.220.4892.6818Cir0.
0131.0094.40
436.600-90.000MH0.000.000.000.092.680.7692.7312Cir0
.0131.0094.40
5469.1000.000Grate0.000.650.8210.092.730.7793.2612Cir0.0131.0095.26G643.90090.000Grate0.000.570.8210.092.731.7992.8012C
ir0.0131.0094.14H
7261.400-90.000Grate0.000.470.8210.092.471.0793.131
2Cir0.0131.0095.13F83252.1000.000Grate0.000.400.3615.092.680.3893.6412
Cir0.0131.0096.80K
9342.00090.000Grate0.001.100.3615.092.680.4892.8812
Cir0.0131.0095.50J101155.600-90.000MH0.000.000.000.092.380.3992.9912Cir0.0131.0096.60
111099.00090.000Grate0.006.220.1015.092.990.3993.38
12Cir0.0131.0094.50M
1210119.1000.000Grate0.000.370.8210.092.990.3493.39
12Cir0.0131.5095.16D
131266.000-90.000Grate0.000.300.8210.093.640.6194.0
46Cir0.0131.0095.04C
Riverlakes Community Center
Number of lines: 13Date: 06-09-2011Hydraflow Storm Sewers Extension v6.052
Storm Sewer Summary Report
Page 1
LineLine IDFlowLineLineLineInvertInvertLineHGLHGLMi
norHGLDnsJunction
No.
ratesizeshapelengthEL DnEL UpslopedownuplossJunctli
neType(cfs)(in)(ft)(ft)(ft)(%)(ft)(ft)(ft)(ft)No.
1
2.6218Cir25.30092.0092.130.51492.6292.750.2292.97En
dManhole
2
1.6418Cir23.00092.1392.220.39192.9792.980.0593.031Manhole
3
1.3518Cir95.90092.2292.680.48093.0393.140.1393.272Manhole
4
1.7012Cir6.60092.6892.730.75893.2793.28n/a93.51 j3Manhole
5G
0.9512Cir69.10092.7393.260.76793.5193.67n/a93.67 j4
Grate
6H
0.8312Cir3.90092.7392.801.79593.5193.510.0393.544Gr
ate
7F
0.6912Cir61.40092.4793.131.07593.0393.48n/a93.48 j2
Grate
8K
0.2012Cir252.10092.6893.640.38193.2793.840.0693.893
Grate
9J
0.5612Cir42.00092.6892.880.47693.2793.300.0593.353G
rate
10
1.5612Cir155.60092.3892.990.39293.0093.610.1593.751
Manhole
11M
0.8812Cir99.00092.9993.380.39493.7593.870.0893.9510
Grate
12D
0.9512Cir119.10092.9993.390.33693.7593.910.1394.031
0Grate
13C
0.446Cir66.00093.6494.040.60694.0594.450.1094.5512G
rate
Riverlakes Community Center
Number of lines: 13Run Date: 06-09-2011
NOTES: Return period = 10 Yrs. ; j - Line contains hyd. jump.
Hydraflow Storm Sewers Extension v6.052
Storm Sewer Tabulation
Page 1
StationLenDrng AreaRnoffArea x CTcRainTotalCapVelPi
peInvert ElevHGL ElevGrnd / Rim ElevLine ID
coeff
(I)flowfull
LineToIncrTotalIncrTotalInletSyst
SizeSlopeDnUpDnUpDnUp
Line
(ft)(ac)(ac)(C)(min)(min)(in/hr)(cfs)(cfs)(ft/s)(in
)(%)(ft)(ft)(ft)(ft)(ft)(ft)
1End25.3000.0010.080.000.003.100.032.90.82.627.533.
80180.5192.0092.1392.6292.7594.0095.802123.0000.003.190.000.001.930.032.60.81.646.571.711
80.3992.1392.2292.9792.9895.8095.80
3295.9000.002.720.000.001.540.031.20.91.357.272.161
80.4892.2292.6893.0393.1495.8094.40436.6000.001.220.000.001.000.011.01.71.703.103.6412
0.7692.6892.7393.2793.2894.4094.40
5469.1000.650.650.820.530.5310.010.01.80.953.122.27
120.7792.7393.2693.5193.6794.4095.26G643.9000.570.570.820.470.4710.010.01.80.834.771.341
21.7992.7392.8093.5193.5194.4094.14H
7261.4000.470.470.820.390.3910.010.01.80.693.692.15
121.0792.4793.1393.0393.4895.8095.13F
83252.1000.400.400.360.140.1415.015.01.40.202.201.1
5120.3892.6893.6493.2793.8494.4096.80K9342.0001.101.100.360.400.4015.015.01.40.562.461.48
120.4892.6892.8893.2793.3094.4095.50J
101155.6000.006.890.000.001.170.016.51.31.562.233.0
7120.3992.3892.9993.0093.6195.8096.60
111099.0006.226.220.100.620.6215.015.01.40.882.241.
84120.3992.9993.3893.7593.8796.6094.50M
1210119.1000.370.670.820.300.5510.010.51.70.952.061
.91120.3492.9993.3993.7593.9196.6095.16D131266.0000.300.300.820.250.2510.010.01.80.440.442.
5360.6193.6494.0494.0594.4595.1695.04C
Riverlakes Community Center
Number of lines: 13Run Date: 06-09-2011
NOTES: Intensity = 14.49 / (Inlet time + 4.40) ^ 0.
79; Return period = 10 Yrs. ; c = cir e = el
lip b = box
Hydraflow Storm Sewers Extension v6.052
Hydraulic Grade Line Computations
Page 1 LineSizeQDownstreamLenUpstreamCheckJLMinorcoeffloss
InvertHGLDepthAreaVelVelEGLSfInvertHGLDepthAreaVelV
elEGLSfAveEnrgyelevelevheadelevelevelevheadelevSfloss(in)(cfs)(ft)(ft)(ft)(sqft)(ft/s)(ft)(ft)(%)(ft)(ft)(ft)(ft)(sqft)(ft/s)(ft)(ft)(%)(%)(ft)(K)(ft)(1)(2)(3)(4)(5)(6)(7)(8)(9)(10)(11)(12)(13)(14)(15)
(16)(17)(18)(19)(20)(21)(22)(23)(24)
1182.6292.0092.620.620.693.820.2392.840.49325.30092
.1392.750.62**0.693.790.2292.970.4820.4870.1231.000
.22
2181.6492.1392.970.841.021.600.0493.010.06623.00092
.2292.980.760.901.820.0593.030.0930.0790.0181.000.05
3181.3592.2293.030.810.981.380.0393.060.05195.90092
.6893.140.460.462.930.1393.270.3940.2220.2131.000.13
4121.7092.6893.270.590.493.490.1993.460.5196.60092.
7393.28 j0.55**0.453.790.2293.510.6430.5810.0381.00
0.22
5120.9592.7393.510.780.661.450.0393.540.07969.10093
.2693.67 j0.41**0.313.100.1593.820.5560.317n/a1.00n
/a
6120.8392.7393.510.780.661.270.0393.530.0613.90092.
8093.510.710.591.410.0393.540.0770.0690.0031.000.03
7120.6992.4793.030.560.451.510.0493.070.10161.40093
.1393.48 j0.35**0.252.790.1293.600.5300.316n/a1.000
.12
8120.2092.6893.270.590.490.420.0093.280.007252.10093.6493.840.20**0.111.880.0693.890.4690.2380.6011.00
0.06
9120.5692.6893.270.590.491.150.0293.290.05642.00092
.8893.300.420.311.810.0593.350.1890.1220.0511.000.05
10121.5692.3893.000.62*0.513.070.1593.140.392155.60
092.9993.610.620.513.070.1593.750.3920.3920.6101.00
0.15
11120.8892.9993.750.760.641.370.0393.780.07099.0009
3.3893.870.490.382.310.0893.950.2670.1680.1671.000.
08
12120.9592.9993.750.760.641.480.0393.790.083119.100
93.3993.910.520.412.330.0893.990.2580.1700.2031.500
.13
1360.4493.6494.050.41*0.172.530.1094.150.60666.0009
4.0494.450.410.172.530.1094.550.6050.6050.4001.000.
10
Riverlakes Community Center
Number of lines: 13Run Date: 06-09-2011
Notes: * Normal depth assumed.; ** Critical depth.;
j-Line contains hyd. jump. ; c = cir e = ellip
b = box
Hydraflow Storm Sewers Extension v6.052
Hydraflow HGL Computation Procedure
Page 1
General Procedure:
Hydraflow computes the HGL using the Bernoulli ener
gy equation. Manning's equation is used to determine energy losses due to pipe friction.
In a standard step, iterative procedure, Hydraflow
assumes upstream HGLs until the energy equation bal
ances. If the energy equation
cannot balance, supercritical flow exists and criti
cal depth is temporarily assumed at the upstream end. A supercritical flow Profile
is then computed using the same procedure in a downstream direction using momentum principles.
Col. 1 The line number being computed. Calculations begin at Line 1 and proceed upstream.
Col. 2 The line size. In the case of non-circular
pipes, the line rise is printed above the span.
Col. 3 Total flow rate in the line.Col. 4 The elevation of the downstream invert.Col. 5 Elevation of the hydraulic grade line at the downstream end. This is computed as the upstream HGL + Minor loss of this line's downstream line.
Col. 6 The downstream depth of flow inside the pipe (HGL - Invert elevation) but not greater than the line size.
Col. 7 Cross-sectional area of the flow at the downstream end.Col. 8 The velocity of the flow at the downstream
end, (Col. 3 / Col. 7).
Col. 9 Velocity head (Velocity squared / 2g).Col. 10 The elevation of the energy grade line at
the downstream end, HGL + Velocity head, (Col. 5 +
Col. 9).
Col. 11 The friction slope at the downstream end (the S or Slope term in Manning's equation).
Col. 12 The line length.Col. 13 The elevation of the upstream invert.Col. 14 Elevation of the hydraulic grade line at the upstream end.Col. 15 The upstream depth of flow inside the pipe (HGL - Invert elevation) but not greater than the
line size.
Col. 16 Cross-sectional area of the flow at the upstream end.Col. 17 The velocity of the flow at the upstream e
nd, (Col. 3 / Col. 16).
Col. 18 Velocity head (Velocity squared / 2g).Col. 19 The elevation of the energy grade line at
the upstream end, HGL + Velocity head, (Col. 14 + Col. 18) .
Col. 20 The friction slope at the upstream end (the S or Slope term in Manning's equation).Col. 21 The average of the downstream and upstream
friction slopes.
Col. 22 Energy loss. Average Sf/100 x Line Length
(Col. 21/100 x Col. 12). Equals (EGL upstream - EGL downstream) +/- tolerance.
Col. 23 The junction loss coefficient (K).Col. 24 Minor loss. (Col. 23 x Col. 18). Is added
to upstream HGL and used as the starting HGL for the next upstream line(s).
DRAINAGE STUDY REPORT
Riverlakes Community Park
APPENDIX C: RETENTION BASIN CALCULATIONS
Interim Condition
Ultimate Condition
Hydraflow Table of Contents Bakersfield Comm Hydro.gpw
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Watershed Model Schematic ...................................................................................1
10 - Year
Hydrograph Reports .................................................................................................................2
Hydrograph No. 1, SCS Runoff, Interim to W. Basin ..............................................................2
Hydrograph No. 2, Reservoir, Interim West Basin .................................................................3
Pond Report - Interim West Basin .....................................................................................4
Hydrograph No. 3, SCS Runoff, Ultimate to W. Basin ...........................................................5
Hydrograph No. 4, Reservoir, Ultimate West Basin ...............................................................6
Pond Report - Ultimate West Basin ...................................................................................7
100 - Year
Hydrograph Reports .................................................................................................................8
Hydrograph No. 1, SCS Runoff, Interim to W. Basin ..............................................................8
Hydrograph No. 2, Reservoir, Interim West Basin .................................................................9
Hydrograph No. 3, SCS Runoff, Ultimate to W. Basin .........................................................10
Hydrograph No. 4, Reservoir, Ultimate West Basin .............................................................11
1
2
3
4
1
Watershed Model Schematic Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052
Project: Bakersfield Comm Hydro.gpwThursday, Jun 9, 2011
Hyd.OriginDescription
Legend
1SCS RunoffInterim to W. Basin
2ReservoirInterim West Basin
3SCS RunoffUltimate to W. Basin
4ReservoirUltimate West Basin
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 1
Interim to W. Basin
Hydrograph type= SCS RunoffPeak discharge= 0.130 cfs
Storm frequency= 10 yrsTime to peak= 12.87 hrs
Time interval= 2 minHyd. volume= 5,602 cuft
Drainage area= 13.780 acCurve number= 70.5
Basin Slope= 0.0 %Hydraulic length= 0 ft
Tc method= USERTime of conc. (Tc)= 15.00 min
Total precip.= 1.59 inDistribution= Type I
Storm duration= 24 hrsShape factor= 484
2
02468101214161820222426
Q (cfs)
0.000.00
0.050.05
0.100.10
0.150.15
0.200.20
0.250.25
0.300.30
0.350.35
0.400.40
0.450.45
0.500.50
Q (cfs)
Time (hrs)
Interim to W. Basin
Hyd. No. 1 -- 10 Year
Hyd No. 1
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 2
Interim West Basin
Hydrograph type= ReservoirPeak discharge= 0.118 cfs
Storm frequency= 10 yrsTime to peak= 19.13 hrs
Time interval= 2 minHyd. volume= 5,594 cuft
Inflow hyd. No.= 1 - Interim to W. BasinMax. Elevation= 392.13 ft
Reservoir name= Interim West BasinMax. Storage= 1,015 cuft
Storage Indication method used. Outflow includes exfiltration.
3
04812162024283236
Q (cfs)
0.000.00
0.050.05
0.100.10
0.150.15
0.200.20
0.250.25
0.300.30
0.350.35
0.400.40
0.450.45
0.500.50
Q (cfs)
Time (hrs)
Interim West Basin
Hyd. No. 2 -- 10 Year
Hyd No. 2 Hyd No. 1 Total storage used = 1,015 cuft
Pond Report 4
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Pond No. 1 - Interim West Basin
Pond Data
Contours - User-defined contour areas. Conic method used for volume calculation. Begining Elevation = 392.00 ft
Stage / Storage Table
Stage (ft)Elevation (ft)Contour area (sqft)Incr. Storage (cuft)Total storage (cuft)
0.00392.007,57700
0.50392.508,3543,9813,981
1.00393.009,1584,3768,357
1.50393.509,9874,78413,141
Culvert / Orifice StructuresWeir Structures
[A][B][C][PrfRsr][A][B][C][D]
Rise (in)= 0.000.000.000.00
Span (in)= 0.000.000.000.00
No. Barrels= 0000
Invert El. (ft)= 0.000.000.000.00
Length (ft)= 0.000.000.000.00
Slope (%)= 0.000.000.00n/a
N-Value= .013.013.013n/a
Orifice Coeff.= 0.600.600.600.60
Multi-Stage= n/aNoNoNo
Crest Len (ft)= 0.000.000.000.00
Crest El. (ft)= 0.000.000.000.00
Weir Coeff.= 3.333.333.333.33
Weir Type= ------------
Multi-Stage= NoNoNoNo
Exfil.(in/hr)= 2.400 (by Contour)
TW Elev. (ft)= 0.00
Note: Culvert/Orifice outflows are analyzed under inlet (ic) and outlet (oc) control. Weir risers checked for orifice conditions (ic) and submergence (s).
Stage / Storage / Discharge Table
StageStorageElevationClv AClv BClv CPrfRsrWr AWr BWr CWr DExfilUserTotal
ftcuftftcfscfscfscfscfscfscfscfscfscfscfs
0.000392.00------------------------0.000---0.000
0.503,981392.50------------------------0.464---0.464
1.008,357393.00------------------------0.509---0.509
1.5013,141393.50------------------------0.555---0.555
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 3
Ultimate to W. Basin
Hydrograph type= SCS RunoffPeak discharge= 0.547 cfs
Storm frequency= 10 yrsTime to peak= 10.10 hrs
Time interval= 2 minHyd. volume= 6,967 cuft
Drainage area= 7.560 acCurve number= 77.5
Basin Slope= 0.0 %Hydraulic length= 0 ft
Tc method= USERTime of conc. (Tc)= 15.00 min
Total precip.= 1.59 inDistribution= Type I
Storm duration= 24 hrsShape factor= 484
5
02468101214161820222426
Q (cfs)
0.000.00
0.100.10
0.200.20
0.300.30
0.400.40
0.500.50
0.600.60
0.700.70
0.800.80
0.900.90
1.001.00
Q (cfs)
Time (hrs)
Ultimate to W. Basin
Hyd. No. 3 -- 10 Year
Hyd No. 3
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 4
Ultimate West Basin
Hydrograph type= ReservoirPeak discharge= 0.149 cfs
Storm frequency= 10 yrsTime to peak= 13.50 hrs
Time interval= 2 minHyd. volume= 6,958 cuft
Inflow hyd. No.= 3 - Ultimate to W. BasinMax. Elevation= 392.16 ft
Reservoir name= Ultimate West BasinMax. Storage= 1,274 cuft
Storage Indication method used. Outflow includes exfiltration.
6
04812162024283236
Q (cfs)
0.000.00
0.100.10
0.200.20
0.300.30
0.400.40
0.500.50
0.600.60
0.700.70
0.800.80
0.900.90
1.001.00
Q (cfs)
Time (hrs)
Ultimate West Basin
Hyd. No. 4 -- 10 Year
Hyd No. 4 Hyd No. 3 Total storage used = 1,274 cuft
Pond Report 7
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Pond No. 2 - Ultimate West Basin
Pond Data
Contours - User-defined contour areas. Conic method used for volume calculation. Begining Elevation = 392.00 ft
Stage / Storage Table
Stage (ft)Elevation (ft)Contour area (sqft)Incr. Storage (cuft)Total storage (cuft)
0.00392.007,57700
0.50392.508,3543,9813,981
1.00393.009,1584,3768,357
1.50393.509,9874,78413,141
Culvert / Orifice StructuresWeir Structures
[A][B][C][PrfRsr][A][B][C][D]
Rise (in)= 0.000.000.000.00
Span (in)= 0.000.000.000.00
No. Barrels= 0000
Invert El. (ft)= 0.000.000.000.00
Length (ft)= 0.000.000.000.00
Slope (%)= 0.000.000.00n/a
N-Value= .013.013.013n/a
Orifice Coeff.= 0.600.600.600.60
Multi-Stage= n/aNoNoNo
Crest Len (ft)= 0.000.000.000.00
Crest El. (ft)= 0.000.000.000.00
Weir Coeff.= 3.333.333.333.33
Weir Type= ------------
Multi-Stage= NoNoNoNo
Exfil.(in/hr)= 2.400 (by Contour)
TW Elev. (ft)= 0.00
Note: Culvert/Orifice outflows are analyzed under inlet (ic) and outlet (oc) control. Weir risers checked for orifice conditions (ic) and submergence (s).
Stage / Storage / Discharge Table
StageStorageElevationClv AClv BClv CPrfRsrWr AWr BWr CWr DExfilUserTotal
ftcuftftcfscfscfscfscfscfscfscfscfscfscfs
0.000392.00------------------------0.000---0.000
0.503,981392.50------------------------0.464---0.464
1.008,357393.00------------------------0.509---0.509
1.5013,141393.50------------------------0.555---0.555
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 1
Interim to W. Basin
Hydrograph type= SCS RunoffPeak discharge= 3.560 cfs
Storm frequency= 100 yrsTime to peak= 10.07 hrs
Time interval= 2 minHyd. volume= 30,574 cuft
Drainage area= 13.780 acCurve number= 70.5
Basin Slope= 0.0 %Hydraulic length= 0 ft
Tc method= USERTime of conc. (Tc)= 15.00 min
Total precip.= 2.80 inDistribution= Type I
Storm duration= 24 hrsShape factor= 484
8
02468101214161820222426
Q (cfs)
0.000.00
1.001.00
2.002.00
3.003.00
4.004.00
Q (cfs)
Time (hrs)
Interim to W. Basin
Hyd. No. 1 -- 100 Year
Hyd No. 1
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 2
Interim West Basin
Hydrograph type= ReservoirPeak discharge= 0.507 cfs
Storm frequency= 100 yrsTime to peak= 15.90 hrs
Time interval= 2 minHyd. volume= 30,566 cuft
Inflow hyd. No.= 1 - Interim to W. BasinMax. Elevation= 392.98 ft
Reservoir name= Interim West BasinMax. Storage= 8,203 cuft
Storage Indication method used. Outflow includes exfiltration.
9
04812162024283236
Q (cfs)
0.000.00
1.001.00
2.002.00
3.003.00
4.004.00
Q (cfs)
Time (hrs)
Interim West Basin
Hyd. No. 2 -- 100 Year
Hyd No. 2 Hyd No. 1 Total storage used = 8,203 cuft
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 3
Ultimate to W. Basin
Hydrograph type= SCS RunoffPeak discharge= 3.919 cfs
Storm frequency= 100 yrsTime to peak= 10.07 hrs
Time interval= 2 minHyd. volume= 25,728 cuft
Drainage area= 7.560 acCurve number= 77.5
Basin Slope= 0.0 %Hydraulic length= 0 ft
Tc method= USERTime of conc. (Tc)= 15.00 min
Total precip.= 2.80 inDistribution= Type I
Storm duration= 24 hrsShape factor= 484
10
02468101214161820222426
Q (cfs)
0.000.00
1.001.00
2.002.00
3.003.00
4.004.00
Q (cfs)
Time (hrs)
Ultimate to W. Basin
Hyd. No. 3 -- 100 Year
Hyd No. 3
Hydrograph Report
Hydraflow Hydrographs Extension for AutoCAD® Civil 3D® 2008 by Autodesk, Inc. v6.052Thursday, Jun 9, 2011
Hyd. No. 4
Ultimate West Basin
Hydrograph type= ReservoirPeak discharge= 0.499 cfs
Storm frequency= 100 yrsTime to peak= 13.20 hrs
Time interval= 2 minHyd. volume= 25,719 cuft
Inflow hyd. No.= 3 - Ultimate to W. BasinMax. Elevation= 392.89 ft
Reservoir name= Ultimate West BasinMax. Storage= 7,392 cuft
Storage Indication method used. Outflow includes exfiltration.
11
04812162024283236
Q (cfs)
0.000.00
1.001.00
2.002.00
3.003.00
4.004.00
Q (cfs)
Time (hrs)
Ultimate West Basin
Hyd. No. 4 -- 100 Year
Hyd No. 4 Hyd No. 3 Total storage used = 7,392 cuft
DRAINAGE STUDY REPORT
Riverlakes Community Park
APPENDIX D: SUPPORTING DATA
NOAA Precipitation Data
Riverlakes ADP Excerpts