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HomeMy WebLinkAboutCDP 07-12; Sears Residence; Drainage Study; 2008-11-18DRAINAGE STUDY FOR CDP07-12 4017SUNNYHILLDRIVE APN 207 - 061 - 54 PREPARED FOR Tom and Wendy Sears 1387 Cynthia Lane Carlsbad, CA 92008 PREPARED BY Robert O. Sukup 4322 Sea Bright Place Carlsbad, CA 92008 November 18, 2008 oz oai o c o o The subject property is an irregularly shaped in-fill lot. It is almost bounded on three sides by either a public street or private driveways on the north, east and west. All of the water flows to the southwest corner of the property where it exits on the surface, across an existing concrete driveway, and then through an existing drainage outlet. This outlet is through a wall, where it then continues on the surface to Alder Street. The single lot grading plan has been designed for all the water to surface flow around the house where it is strategically collected in a 4" drain pipe system that discharges into the lower, non graded, back yard area. The lower back yard area has 2 - 50' long grass swales that will promote filtration and infiltration. The 2 grass swales converge to a small gravel pit. The gravel pit is meant to augment the filter and infiltration process started by the upstream grass swales. It also creates a small storage capacity of about 5.65 c.f. [assumes 30% voids in the gravel]. Whatever water is not absorbed by the gravel pit and grass swales, continues in a gravel swale downstream to the existing offsite driveway that has been the "historic conveyance channel" for the immediate houses in the area, including the subject lot. The combination of the grass swales, gravel pit and gravel swales should contain all low flows and nuisance water on site. Additional heavy storm flows not absorbed, will go down the aforementioned driveway, through a storm drain opening in a block wall, and then continue down a driveway to Alder Street where it eventually goes into the City Drainage System. In my professional opinion, the project's drainage system, as proposed, should function very well and not create any downstream erosion, flooding, or siltation. OV 21 2m O LOT jws A PAD U>\U- B£~cu>ss:" TO = A PAO. SOIL E. -' 5% ftorAbCCtJC.^ , O ,Mpe*v\o05 POST- 3^% NO (r/^BUE. NO ^c R^DOCTlOfO IW UDT Dt\OS\TV ^ 2,9 ARtA OF -TK LOT \S . 38 PCOVO TO O^B A To g "7>Q M/IO TA-^Lb COODfTlOO KlO QOK)QlTlQNi |N IHCLV3DC. YARDS, A ex IT -R> TUB \S Device. TUB ON bevies TU voo /4Eove MULT IPLB 1'ut use Tc- F\k 3-1- \'\e AS5tSKl£0 Ti\e FOLLOWING I V4U)BS vc. rro«^ *? FOIL 100 - CIA"- .Z'bS v 3,0 v ,3&ic - ,1)1 a ^- WIL-. ciA' .4* v 3^ v ^S4- -- .6 v 3b4c - .47 i^cfe f . ioo Vcflp, ^ToaM FO^ ri>te Car TO ^-^3 c?</ Ac. A lH FLOU) ct> BY TUc |K)TROt>OCTlOh4 OF GRA^S PlTS— ALU TO pnovioe fitted i^)G t IK) FIL-T^TIC^ TO oOTLef AMi UOT ce^Al^ AWV DQUON^7R/->4W Olt o o o San Diego County Hydrology Manual Date: June 2003 Section: Page: 3 6 of 26 Table 3-1 RUNOFF COEFFICIENTS FOR URBAN AREAS Land NRCS Elements Undisturbed Natural Terrain (Natural) Low Density Residential (LDR) Low Density Residential (LDR) Low Density Residential (LDR) Medium Density Residential (MDR) Medium Density Residential (MDR) Medium Density Residential (MDR) Medium Density Residential (MDR) High Density Residential (HDR) High Density Residential (HDR) Commercial/Industrial (N. Com) Commercial/Industrial (G. Com) Commercial/Industrial (O.P. Com) Commercial/Industrial (Limited I.) Commercial/Industrial (General I.) Use County Elements Permanent Open Space __ Residential, 1.0 DU/A or less Residential, 2.0 DU/A or less Residential, 2.9 DU/A or less Residential, 4.3 DU/A or less p^. Residential, 7.3 DU/A or less Residential, 10.9 DU/A or less Residential, 14.5 DU/A or less Residential, 24.0 DU/A or less Residential, 43.0 DU/A or less Neighborhood Commercial General Commercial Office Professional/Commercial Limited Industrial General Industrial Runoff Coefficient "C" Soil Type % IMPER. : -StX10 20 25 r -^34% 40 45 50 65 80 80 85 90 90 95 S^^e* ( A , 0.20, ^0?7 0.34 0.38 0.41/<s-C, 0.48 0.52 0.55 0.66 0.76 0.76 0.80 0.83 0.83 0.87 > B ^ °'25 ^— ^ 0.32 0.38 0.41 3D °45 ^-^ 0.51 0.54 0.58 0.67 0.77 0.77 0.80 0.84 0.84 0.87 C 0.30 0.36 0.42 0.45 0.48 0.54 0.57 0.60 0.69 0.78 0.78 0.81 0.84 0.84 0.87 D 0.35 0.41 0.46 0.49 0.52 0.57 0.60 0.63 0.71 0.79 0.79 0.82 0.85 0.85 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 remain 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 SEARS SanD. County Hydrology Manual Date: : 2003 Section: Page: 3 12 of 26 Note that the Initial Time of Concentration should be reilective 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. o Table 3-2 provides limits of the length (Maximum Length (LM)) of sheet flow to be used in hydrology studies. Initial Tj values based on average C values for the 1 d Use Element are also included. These values can be used in planning and design apparitions as described below. Exceptions may be approved by the "Regulating Agency" when submitted with a detailed study. MAXIMUM OVERLAND FLOW LENGTH (LM) & INITIAL TIME OF CONCENTRATION QY Element* Natural LDR -LDB LDR- " 'MDR MDR MDR MDR HDR HDR N. Com G. Com , O.P./Com Limited I. General I. DU/ Acre 1 2 ^»s2.9_~*~~^ 4.3 7.3 10.9 14.5 24 43 .5 LM 50 50 50 >50 50 50 50 50 50 50 50 50 50 50 50 % TJ 13.2 12.2 11.3 10.7 10.2 9.2 8.7 8.2 6.7 5.3 5.3 4.7 4.2 4.2 3.7 1 LM 70 70 70 70 70 65 65 65 65 65 60 60 60 6( 60 % Ti 12.5 11.5 10.5 10.0 9.6 8.4 7.9 7.4 6.1 4.7 4.5 4.1 3.7 •,7 3.2 2 LM 85 85 85 85 80 80 80 80 75 75 75 75 70 70 70 % T, 10.9 10.0 9.2 8.8 8.1 7.4 6.9 6.5 5.1 4.0 4.0 3.6 3.1 3.1 2.7 3( LM 100 100 100 95 95 95 90 90 90 85 85 85 80 80 80 >/o Ti 10.3 9.5 8.8 8.1 7.8 7.0 6.4 6.0 4.9 3.8 3.8 3.4 2.9 2.9 2.6 v 5 . LM 100 100 100 100( 100 100 100 100 95 95 95 90 90 90 90 4*^) Ti 8.7 8.0 7.4 ^TXT Tf 6.0 5.7 5.4 4.3 3.4 3.4 2.9 2.6 2.6 2.3 10 LM 100 100 100 ^00 100 100 100 100 100 100 100 100 100 100 .00 % Ti 6.9 6.4 5.8 5.6 5.3 4.8 4.5 4.3 3.5 2.7 2.7 2.4 2.2 2.2 1.9 *See Table 3-1 for more detailed description 3-12 l'1 M i:I r.County of San Diego Hydrology Manual (;./V«*. Rainfall Isophivials 10 Year Rainfall Event- 6 Hours .•--.I y VKVK.T \i p1 !• r \ . ! '». !..v :. V ]:; I\ aLi'>.>A\K V i o o o County of San Diego Hydrology Manual a-~t-p-;... •->.fo- Rainfall Isopluvials 10 Year Rainfall Event- 24 Hours o o County of San Diego Hydrology Manual Rainfall Isopluvials 100 Year Rainfall Event - 6 Hours INS MAP IS PROVIDED WI1HOUT WMVUNTY tf ANT WHO. EJTHtR EXPRESS, maucww. BUI NOT LIMITED 10. TitE IMPLIED WARRAHHES OF MERCWMTABlOrv AMD FITNESS FOR A PARDCUlAft PUHPOSE. SmGIS. Al Ft^liu H« o o o rtyaroiogy ivianuai Rivefsidd fcotihly Kifep'' Rainfall Isopluvials 100 Year Rainfall Event - 24 Hours ;n!?' t •. • •. '••! 1 *•' K V • < IMS MAP IS PHOV1DEO WITHOUT WARRAMTT OF AN* MND. CITVCH UPME&S OR IMPLIeD. kClUOMG, Bin HD1 tMITEO TO, THE WPLIEO WARRAHDESMERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE. i.rtahl S*nGIS. 01 Riohli FU»rvcl o o Intensity (in/hr) 6-Hour Precipitation (in) Duration (min) Directions for Application: (1) From precipitation maps determine 6 hr and 24 hr amounts for the selected frequency. These maps are included in the County Hydrology Manual (10,50, and 100 yr maps Included In the Design and Procedure Manual). (2) Adjust 6 hr precipitation (if necessary) so that it is within the range of 45% to 65% of the 24 hr precipitation (not applicaple to Desert). (3) Plot 6 hr precipitation on the right side of the chart. (4) Draw a line through the point parallel to the plotted lines. (5) This line is the intensity-duration curve for the location bei: ! Application Form: .. t...., (a) Selected frequency (b)P6=' '2,(a |n..P24« (c) Adjusted Pg(2> =''_ (d)tx = (e)l Note: This chart replaces the Intensity-Duration-Frequency curves used since 1965. pa" " Duration 5 7 10 15 20 25 30 40 SO 60 90 120 150 160 "240 300 360 1 i 1.5 1 I 1 2.63 212 tea f.30 1.08 093 083 069 060 053 041 0.34 029 026 395 318 253 1.95 162 1.40 124 1.03 0.90 080 061 051 0.44 039 0.22 j 0.33 019 1028 0.17 1 0.25 T-'2.5 i 527.659 4 24' 5 30 337!421 259J324 215)269 187!233 166 1.38 1.19 106 207 1.72 1.49 1.33 082 102o.ea 059 052 0.43 038 033 0.85 073 065 054 047 042 3"4'3.5i i i 7.90 636 SOS 389 323 2.80 249 207 1.79 1.S9 123 1.02 0.88 078 0.65 056 0.50 9,22 742 5.90 454 377 327 290 2.41 2.09 1.86 143 J.19 1.03 091 076 066 058 ""4"'j:"4.S 5"i I i I J 10.54 848 6.74 5.19 4.31 3.73 332 2.76 2.39 2 12 1 63 136 1.1 fl 104 087 075 0.67 11.86 j 13.17 9.54 i 10.60 7 58 ! 8.42 5.84 649 4.85 i 5.39 420 467 3.73 i 4.15 310 ! 345 2.69 i 2.98 239 2.6S 184 1.53 132 1 18 0.98 204 1.70 147 1.31 1.08 0 85 0 94 0.75 ! 0.84 ..._, j 14.49 11.66 927 713 593 513 456 379 3.28 2.92 225 187 162 144 1 19 103 092 af 15,81 12.72 1011 778 6.46 5.60 498 413 3.58 318 245 2.04 1.76 167 1.30 1 13 100 Intensity-Duration Design Chart - Template o o FIGURE 3-1