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HomeMy WebLinkAboutSDP 2019-0014; CARLSBAD OAKS NORTH LOT 2; PRIORITY PROJECT HYDROLOGY STUDY; 2020-06-01PRIORITY PROJECT HYDROLOGY STUDY FOR: CARLSBAD OAKS NOR THLOT 2 CARLSBAD, CA PREPARED FOR: Carlsbad Oaks North Ventures LP CIO Techbilt Companies 3575 Kenyon Street - Suite 200 San Diego, CA 92100 RECEIVED JUN 03 2020 LAND DEVELOPMENT ENGINEERING PREPARED BY: EXCEL ENGINEERING 440 State Place Escondido, CA 92029 Tel. (760) 745-8118 Project No. 19-0 79 DATE PREPARED: June 1, 2020 Hydrology Study TABLE OF CONTENTS 1.0 Project Description 1.1 Project Purpose 1.2 Project Proposed facilities 2.0 Vicinity Map 3.0 Site Map 4.0 Description of Watershed 4.1 Existing Conditions Topography 4.2 Existing Conditions + Project Conditions Topography 4.3 Hydrologic Unit Contribution 5.0 Methodology 5.1 Hydrology Software 5.2 Routing Software 5.3 Hydraulics Software 6.0 Calculations 6.1 Determine the Watershed that affects the project 6.2 Calculate Runoff Coefficient 6.3 Calculate Storm Flows using the Rational Method 7.0 Mitigation Measures 7.1 Mitigation of Increased Runoff 7.2 Check Capacity of Existing Downstream Storm Drain Facilities 8.0 Summary 9.0 References 10.0 Declaration of Responsible Charge 11.0 Attachments Attachment A - Site Map Attachment B - Figures & Tables from the SD Hydrology Manual 2003 Attachment C - Watershed Information Watershed Map Soils Index Map Rainfall Isopluvial Maps Attachment D - Previously Approved Improvement Plans Attachment E - Post Developed Q Calculations Attachment F - Post Developed Hydrology Map Hydrology Study 1.0 PROJECT DESCRIPTION 1.1 Project Purpose The purpose of this project is to receive approval from the City of Carlsbad on a Site Development Plan (Minor) to construct a parking lot in Lot 2 as well as the associated infrastructure and improvements on existing 7.52 acre parcel. 1.2 Project Proposed Facifities The project is proposing to build a parking lot with a total of 191,239 square feet of AC pavement. As part of this project, associated improvements will include the 343 parking spaces and 10% of the site will be landscaped throughout the parking areas, slopes and, frontages. All necessary utilities (storm, sewer, water, dry, etc.) will be installed as part of the project and tie into existing stubs provided for the site by City of Carlsbad DWG No. 415-9. Normal uses of such a development will generate storm water runoff with the potential to carry pollutants to off-site tributaries. Biofiltration basins are planned to be incorporated throughout the site to treat and detain runoff from impervious and landscaped areas. Carlsbad Oaks North Ventures LP C/O TechBilt Companies is the recorded owner of the project sites. Hydrology Study northeast corner of the site (installed as part of the Carlsbad Oaks mass grading operations). Once collected in this desiltation basin, the runoff flows through an existing storm drainage pipe to an existing storm drain structure that outlets into a storm drainage detention basin formed by the intersection of Faraday Avenue and El Fuerte Street (as referenced and designed in the Rancho Carlsbad Channel & Basin Project Hydrology Study, by Rick Engineering - circa 1985). Once released from the detention basin (installed and sized to detain the future Carlsbad Oaks Business Park 100-year flows as well as runoff from the construction of Faraday Avenue) the flows are discharged into Agua Hedionda Creek baèk to the north of Faraday Avenue and ultimately Agua Hedionda Lagoon and the Pacific Ocean. This represents the Carlsbad Hydrologic Unit, Aqua Hedionda HA, Los Monos HSA (904.31). 4.2 Existing Conditions + Project Conditions Topography The Carlsbad Oaks Lots 2 Industrial project layout proposes to install a large parking field across the site. The main drive aisle accessing the site from El Fuerte Street at the southeastern end of the site. The parking lot drains north east towards the biofiltration systems. Once within the water quality treatment systems, the stormwater infiltrates through the treatment medium into underdrains that route the flows to the private onsite storm drainage system. This system uses new piping to direct the flows to the existing storm drain structure installed as part of the Carlsbad Oaks Business Park project and ties into the existing storm drainage system within El Fuerte Street heading north toward its outfall location. As calculated below, and summarized further in Section 8, Lot 2 discharges peak 100-year flows at less than those shown on DWG No. 415-9E. On Sheet 8 of that drawing set, the Lot 2 project pipe flowrate is shown as 29.65 CFS being conveyed into the main storm drain. The existing infrastructure was sized assuming the Carlsbad Oaks Business Park pads (CT 97-13) were to be developed at a high C-factor to account for the development of the lots into industrial use. The original mass grading relied on the Rancho Carlsbad Channel & Basin Project Hydrology Study to detain the flows once they were discharged across Faraday Avenue. Drainage patterns and basin areas have been detailed and are further shown in the Attachments on the Post-Development Hydrology Basin Map. The proposed condition flowrate is 29.30 CFS, less than the allowable 29.65 CFS. 4.3 Hydrologic Unit Contribution The project site is within the Carlsbad Hydrologic Unit, Agua Hedionda HA, Los Monos HSA (904.31). After drainage leaves the site, it flows northeast into Agua Hedionda Creek. After undergoing detention at the control facility located at the intersection of Faraday Aventie and El Fuerte Street the flow then continues along 4 Hydrology Study Agua Hedionda Creek towards Agua Hedionda Lagoon and the Pacific Ocean south of Tamarack. 5.0 METHODOLOGY This study complies with the 2003 San Diego Hydrology Manual. The rational method as presented in Section 3 of that manual and workbook examples were followed. 5.1 Hydrology Software The "Rational Hydrology Method, San Diego County (2003 Manual)" module of the CIVILCADD/CIVIL DESIGN Engineering software version 7.9 is used in this study. This software was also used to developed hydrographs from the rational method results. This procedure also complies with the 2003 San Diego Hydrology Manual as presented in Section 6. 5.2 Routing Software No routing calculations were performed for this site at this time. Should further routing be required upon further development of the site and possible site plan changes causing discharge rates to increase above the predeveloped rates, the existing hydromodification/water quality treatment ponds can be used as flow control facilities. In order to show this is the case, Hydraflow Hydrographs 2004 by Intelisolve would then be used in this step. The hydrograph developed from the rational method is then manually entered into this software and routed into each detention pond. 5.3 Hydraulics Software The hydraulics calculations were performed on the Hydaflow Express Extension v.10.4 ht1i://www.autodesk.com/civi13d-stormwater. For the pipe flows on Lot 2 no increase in flows being released from the private storm drainage system at the single discharge point at the southwest corner of the site are expected versus the mass-graded (pre-developed) conditions that the infrastructure was designed for. Therefore, all downstream effects from stormwater velocities have already been accounted for by the reports and the plans approved for construction of the original Carlsbad Oaks Business Park infrastructure. 6.0 CALCULATIONS One hydrologic calculation will be done at this stage. Due to the 100-year peak flowrates already being determined for existing conditions as part of DWG No. 415-9, the only calculation to be done as part of this report is the 100-year flowrates expected from the postdeveloped conditions. These numbers will be used to size the proposed storm drain pipes and to doublecheck if the existing storm drain outlet facilities are adequate. Since this project met all conditions within the parameters of the software used, no further hydraulic calculations were Hydrology Study 6.1 Determine the Watershed that affects the project Please see the "Watershed Map" in Attachment C 6.2 Calculate Runoff Coefficient Based on NRCS maps show that this project site is in type "D" soil. The previous hydrology calculations done as part of the Carlsbad Oaks infrastructure and mass grading operation also showed type "D" soils. Therefore, we are going to use all coefficients for that type of soil. As stated in section 3.1.2 of the San Diego Hydrology Manual on the second paragraph, "impervious percentage (% Impervious) as given in Table 3-1 for any area, shall govern the selected value for D." For all areas to remain pervious post-construction a "c" factor of c=0.35 is used. The remainder of the site's "c" factors will be based on the percentage of imperviousness within that subarea. The Land use chosen from table 3-1 of the San Diego Hydrology Manual (see attachment B) with a corresponding impervious area to that land use to be used in the hydrology software. 6.3 Calculate Storm Flows using the Rational Method The 100-year post developed storm flows were calculated for this project to be 29.30 CFS. These are less than those shown on the approved drawings that originally developed the pads. Please see "Post Developed Q Calculations" in Attachment E for the developed conditions. 7.0 MITIGATION MEASURES A Storm Water Quality Management Plan (SWQMP) has been prepared for this project to discuss treatment and flow control of the lower flows (2-year and 10- year). This Hydrology study analyzes the higher 100-year flows. 7.1 Mitigate Increase Runoff As discussed above, the postdeveloped runoff rate is 29.30 CFS for Lot 2 at the outfall in El Fuerte Street. The flowrate shown on DWG No. 415-9 downstream of this project's collection point is 29.65 CFS for Lot 2 (see Attachment D). The proposed site development decreases the expected peak flows and therefore no further mitigation is required. 7.2 Check Capacity of Existing Downstream Storm Drain Facilities Since peak flows are reduced, no further capacity analysis of downstream storm drain facilities is necessary. Hydrology Study 8.0 SUMMARY This project will not negatively impact the existing downstream storm drain facilities. The resulting 100-year flowrates from the proposed development are less than those calculated and accounted for as part of the Carlsbad Oaks Business Park project (CT 97- 13) where pads were graded out and infrastructure installed to account for the expected development type that this site conforms to. 9.0 REFERENCES County of San Digo, Department of Public Works, Flood Control Section, June 2003 San Diego County Hydrology Manual Hydrology Study 10.0 DECLARATION OF RESPONSIBLE CHARGE I hereby declare that I am the engineer of work for this project. That I have exercised responsible charge over the design of the project as defined in section 6703 of the business and professions codes, and that the design is consistent with current design. I understand that the check of the project drawings and specifications by the City of Carlsbad is confined to a review only and does not relieve me, as engineer of work, of my responsibilities for project design. ENGINEER OF WORK Excel Engineering 440 State Place Escondido, CA 92029 Tel - (760)745-8118 Fax - (760)745-1890 Project Number: 19-079 $FES D. No. 456 o) 6/1/2020 Robert Vt)entino, RCE 45629 Date Registration Expire: December 31, 2020 Hydrology Study ATTACHMENT B FIGURES & TABLES FROM THE SD HYDROLOGY MANUAL 2003 Hydrology Study ATTACHMENT C WATERSHED INFORMATION Soils Index Map Point Rainfall Isophivial maps I .. J t ..... 32°45 hrt 32°30 0 Ca) County of San Diego J Hydrology Manual I 33°30 — I I A Riversid 'V H OCCC S If 7i a:!P: .. r . - : •. . 4 . 'J Soil Hydrologic Groups -.. --.•--&---- I H 3315 I.. .. 4. Legen VISTV OCEANsIrF - :. •' 4 .. . . .- H . - S QIDO Soil Gro:ps CARLBA - S K' - -; J I - Group B PROJECT SITE w s_ ._ . __ Group 0 ENCINITAS - '/ ;i.._._.•.Nf : Group D Undetermined POWAY C) SOLANABEF4 . ---- - . S.D. COUNTY . 330 Data Unavailable 0 DEL MAR' - i 2 - . -- k.b - --- ......- .- - ....... CD CD I — a Ii C) TEE 0 AN DIE _J- 04 LA MESA .• .•- :- \ -'--- --H. L GROVE DP SMGIS ,_r I - D.a*b s\ FL 'T4EI DI C STA v r { $ 1 N THIS MNP IS PROVIDED WITHOUT WARRANTY OF MY KIND OTTER EXPRESS OR IMPLIED INCLUDING. BUT NOT LIMITED TO. THE IMPLIED WARRANTIES I - OF MERCHANTABILITY AND FITNESS FORK PRATIOLLAP PURPOSE IMPERIAL BEACH . CISGIS NI,Rd M e X U E HORAS IrdwWHOth I I ISR pmdacl may P0.5K!., .,fo.mal!o., aA.y has bee., ,00soduP0d pa.m,ss.OP IssUed by Iflo,5 P.05w, Mep - -. -. 32a30 0 3MiIes PROJECT SOIL MAP 21 WATERSHED MAP 24 Hydrology Study ATTACHMENT D PREVIOUSLY APPROVED IMPROVEMENT PLANS Hydrology Study ATTACHMENT E POST DEVELOPED Q CALCULATIONS Steps Taken To Analyze This Condition The Rational Method as outlined in section 3 of the June 2003 San Diego County Hydrology Manual is followed here. The software that we are using is the "Rational Hydrology Method, San Diego County (2003 Manual)" module of the CIVILCADD/CIVIL DESIGN Engineering software version 7.9. Please see the subsequent pages for the calculations. These calculations are for the Qi 00. The results are outlined/summarized in Section 8. San Diego County Rational Hydrology Program CIVILCADD/CIVILDESIGN Engineering Software, (c)1991-2014 Version 9.0 Rational method hydrology program based on San Diego County Flood Control Division 2003 hydrology manual Rational Hydrology Study Date: 05/29/20 ------------------------------------------------------------------------ 19079 POST DEVELOPMENT 100 YEAR CARLSBAD OAKS NORTH LOT 2 Hydrology Study Control Information ------------------------------------------------------------------------ Program License Serial Number 6332 ------------------------------------------------------------------------ Rational hydrology study storm event year is 100.0 English (in-lb) input data Units used Map data precipitation entered: 6 hour, precipitation(inches) = 2.750 24 hour precipitation(inches) = 5.300 P6/P24 = 51.9% San Diego hydrology manual 'C' values used Process from Point/Station 101.000 to Point/Station 102.000 INITIAL AREA EVALUATION **** Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 [COMMERCIAL area type (General Commercial Impervious value, Ai = 0.850' Sub-Area C Value = 0.820 Initial subarea total flow distance = 110.000(Ft.) Highest elevation 270.250 (Ft.) Lowest elevation = 267.220(Ft.) Elevation difference = 3.030(Ft.) Slope = 2.755 % INITIAL AREA TIME OF CONCENTRATION CALCULATIONS: The maximum overland flow distance is 85.00 (Ft) for the top area slope value of 2.75 %, in a development type of General Commercial In Accordance With Figure 3-3 Initial Area Time of Concentration = 3.31 minutes TC = [1.8*(1.1_C)*distance(Ft.).5)/(% slope(1/3)) TC= [1.8*(1.1_0.8200)*( 85.000.5)/( 2.755(1/3)1= 3.31 Calculated TC of 3.315 minutes is less than 5 minutes, resetting TC to 5.0 minutes for rainfall intensity calculations Rainfall intensity (I) = 7.246(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q=KCIA) is C = 0.820 Subarea runoff - 0.772(CFS) Total initial stream area = 0.130(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 102.000 to Point/Station 103.000 IRREGULAR CHANNEL FLOW TRAVEL TIME Estimated mean flow rate at midpoint of channel - 9.197(CFS) Depth of flow - 0.275(Ft.), Average velocity = 2.332(Ft/s) Irregular Channel Data Information entered for subchannel number 1 Point number 'X' coordinate 'Y' coordinate CARLSBAD OAKS NORTH 1012 Page lof 10 1 0.00 1.13 2 13.00 0.27 3 40.00 0.13 4 42.50 0.00 5 45.00 0.13 6 184.00 1.80 Manning's 'N' friction factor = 0.013 ----------------------------------------------------------------- Sub-Channel flow = 9.197(CFS) flow top width = 44.131 (Ft.) velocity= 2.332(Ft/s) area = 3.944(Sq.Ft) Froude number - 1.375 Upstream point elevation - 267.220 (Ft.) Downstream point elevation = 260.000(Ft.) Flow length 693.000(.Ft.) Travel time = 4.95 mm. Time of concentration = 8.27 mm. Depth of flow = 0.275(Ft.) Average velocity = 2.332(Ft/s) Total irregular channel flow = 9.197(CFS) Irregular channel normal depth above invert elev. = 0.275 (Ft.) Average velocity of channel(s) = 2.332(Ft/s) Adding area flow to channel Rainfall intensity (I) = 5.238(In/Hr) for a 100.0 year storm Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C 0.000 Decimal fraction soil group D = 1.000 (COMMERCIAL area type (General Commercial Impervious value, Ai = 0.850 Sub-Area c Value = 0.820 Rainfall intensity = 5.238(In/Hr) for a 100.0 year Storm Effective runoff coefficient used for total area (Q=KCIA) is C = 0.820 CA = 3.353 Subarea runoff = 16.792(CFS) for 3.959(Ac.) Total runoff - 17.564(CFS) Total area = 4.089(Ac.) Depth of flow = 0.320(Ft.), Average velocity - 2.907(Ft/s) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 103.000 to Point/Station 103.000 ** SUBAREA FLOW ADDITION **** Rainfall intensity (I) - 5.238(In/Hr) for a 100.0 year storm Decimal fraction Soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 (COMMERCIAL area type (General Commercial Impervious value, Ai = 0.850 Sub-Area C Value 0.820 Time of concentration 8.27 mm. Rainfall intensity = 5.238(In/Hr) for a 100.0 year storm Effective runoff coefficient used for total area (Q-KCIA) is C = 0.820 CA = 4.063 Subarea runoff 3.720(CFS) for 0.866(Ac.) Total runoff = 21.284(CFS) Total area = 4.955(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 103.000 to Point/Station 103.000 **** CONFLUENCE OF MAIN STREAMS **** The following data inside Main Stream is listed: In Main Stream number: 1 Stream flow area = 4.955(Ac.) Runoff from this stream = 21 .284 (CFS) CARLSBAD OAKS NORTH LOT 2 Page 2 of 10 Time of concentration = 8.27 mm. Rainfall intensity = 5.238(In/Hr) Program is now starting with Main Stream No. 2 Process from Point/Station 201.000 to Point/Station 202.000 INITIAL AREA EVALUATION **** Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 [COMMERCIAL area type (General Commercial Impervious value, Ai = 0.850 Sub-Area C Value = 0.820 Initial subarea total flow distance = 77.000(Ft.) Highest elevation = 266.220(Ft.) Lowest elevation = 265.170(Ft.) Elevation difference - 1.050(Ft.) Slope - 1.364 % INITIAL AREA TIME OF CONCENTRATION CALCULATIONS: The maximum overland flow distance is 60.00 (Ft) for the top area slope value of 1.36 %, in a development type of General Commercial In Accordance With Figure 3-3 Initial Area Time of Concentration = 3.52 minutes TC = (1.8*(1.1_C)*distance(Ft.).5)/(% s1ope(1/3)] TC - (1.8*(1.1_0.8200)*( 60.000.5)/( 1.364(1/3)1= 3.52 Calculated TC of 3.520 minutes is less than 5 minutes, resetting TC to 5.0 minutes for rainfall intensity calculations Rainfall intensity (I) = 7.246(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q=KCIA) is C = 0.820 Subarea runoff = 0.784(CFS) Total initial stream area = 0.132(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 202.000 to Point/Station 203.000 IRREGULAR CHANNEL FLOW TRAVEL TIME **** Estimated mean flow rate at midpoint of channel = 2.454(CFS) Depth of flow = 0.166(Ft.), Average velocity - 1.745(Ft/s) Irregular Channel Data *********** ----------------------------------------------------------------- Information entered for subchannel number 1 Point number 'X' coordinate '1' coordinate 1 0.00 0.84 2 123.50 0.07 3 125.00 0.00 4 126.50 0.07 5 193.00 0.83 Manning's 'N' friction factor - 0.013 ----------------------------------------------------------------- Sub-Channel flow 2.454(CFS) flow top width - 25.583(Ft.) velocity= 1.745(Ft/s) area = 1.406(Sq.Ft) Froude number = 1.312 Upstream point elevation = 265.170(Ft.) Downstream point elevation = 263.340 (Ft.) Flow length 164.000(Ft.) Travel time = 1.57 mm. Time of concentration - 5.09 mm. Depth of flow = 0.166(Ft.) Average velocity - 1.745(Ft/s) Total irregular channel flow = 2.454(CFS) Irregular channel normal depth above invert elev. = 0.166(Ft.) Average velocity of channel(s) = 1.745(Ft/s) Adding area flow to channel CARLSBAD OAKS NORTH LOT 2 Page 3 of 10 Rainfall intensity (I) = 7.166(In/Hr) for a 100.0 year storm Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 (COMMERCIAL area type (General Commercial Impervious value, Ai = 0.850 Sub-Area C Value = 0.820 Rainfall intensity = 7.166(In/Hr) for a 100.0 year storm Effective runoff coefficient used for total area (Q-KCIA) is C = 0.820 CA = 0.569 Subarea runoff 3.294(CFS) for 0.562(Ac.) Total runoff = 4.078(CFS) Total area = 0.694(Ac.) Depth of flow = 0.189(Ft.), Average velocity = 1.970(Ft/s) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 203.000 to Point/Station 204.000 IRREGULAR CHANNEL FLOW TRAVEL TIME Depth of flow = 0.254(Ft.), Average velocity = 10.574(Ft/s) !Warning: Water is above left or right bank elevations ******* Irregular Channel Data ----------------------------------------------------------------- Information entered for subchannel number 1 Point number 'X' coordinate 'Y' coordinate 1 0.00 0.00 2 1.50 0.13 3 3.00 0.25 Manning's 'N' friction factor = 0.013 ----------------------------------------------------------------- Sub-Channel flow 4.078(CFS) flow top width = 3.000 (Ft.) velocity- 10.574(Ft/s) area - 0.386(Sq.Ft) Froude number = 5.197 Upstream point elevation = 263.340 (Ft.) Downstream point elevation = 261.750(Ft.) Flow length 12.000(Ft.) Travel time - 0.02 mm. Time of concentration = 5.11 mm. Depth of flow = 0.254(Ft.) Average velocity = 10.574(Ft/s) Total irregular channel flow 4.078(CFS) Irregular channel normal depth above invert elev. = 0.254(Ft.) Average velocity of channel(s) = 10.574(Ft/s) !Warning: Water is above left or right bank elevations Process from Point/Station 204.000 to Point/Station 204.000 ** SUBAREA FLOW ADDITION **** Rainfall intensity (I) - . 7.149(In/Hr) for a 100.0 year storm Decimal fraction soil group A = 0.000 Decimal fraction soil group B 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D 1.000 [COMMERCIAL area type (General Commercial Impervious value, Ai - 0.850 Sub-Area C Value = 0.820 Time of concentration - 5.11 mm. Rainfall intensity - 7.149(In/Hr) for a 100.0 year storm Effective runoff coefficient used for total area (Q-RCIA) is C = 0.820 CA = 0.655 Subarea runoff = 0.606(CFS) for 0.105(Ac.) Total runoff = 4.684(CFS) Total area - 0.799(Ac.) CARLSBAD OAKS NORTH LOT 2 Page 4 of 10 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to Point/Station 204.000 CONFLUENCE OF MINOR STREAMS Along Main Stream number: 2 in normal stream number 1 Stream flow area = 0.799(Ac.) Runoff from this stream 4.684(CFS) Time of concentration - 5.11 mm. Rainfall intensity = 7.149(In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 301.000 to Point/Station 302.000 **** INITIAL AREA EVALUATION **** Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 (COMMERCIAL area type (General Commercial Impervious value, Ai = 0.850 Sub-Area C Value = 0.820 Initial subarea total flow distance = 56.000(Ft.) Highest elevation = 264.590(Ft.) Lowest elevation = 262.500(Ft.) Elevation difference 2.090(Ft.) Slope = 3.732 % Top of Initial Area Slope adjusted by User to 4.328 % INITIAL AREA TIME OF CONCENTRATION CALCULATIONS: The maximum overland flow distance is 90.00 (Ft) for the top area slope value of 4.33 %, in a development type of General Commercial In Accordance With Figure 3-3 Initial Area Time of Concentration = 2.93 minutes TC = [1.8*(1.1_C)*distance(Ft.)*.5)/(% slope(1/3)J TC = (1.8*(1.1_0.8200)*( 90.000.5)/( 4.328(1/3)1- 2.93 Calculated TC of 2.934 minutes is less than 5 minutes, resetting TC to 5.0 minutes for rainfall intensity calculations Rainfall intensity (I) - 7.246(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q-KCIA) is C 0.820 Subarea runoff = 0.267(CFS) Total initial stream area = 0.045 (Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 302.000 to Point/Station 204.000 PIPEFLOW TRAVEL TIME (User specified size) Upstream point/station elevation = 261.860(Ft.) Downstream point/station elevation = 261.750(Ft.) Pipe length = 23.00(Ft.) Slope = 0.0048 Manning's N - 0.013 No. of pipes = 1 Required pipe flow = 0.267(CFS) Given pipe size = 4.00(In.) NOTE: Normal flow is pressure flow in user selected pipe size. The approximate hydraulic grade line above the pipe invert is 0.562(Ft.) at the headworks or inlet of the pipe(s) Pipe friction loss = 0.454(Ft.) Minor friction loss = 0.219(Ft.) K-factor - 1.50 Pipe flow velocity = 3.06(Ft/s) Travel time through pipe = 0.13 min. Time of concentration (TC) = 3.06 mm. ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to Point/Station 204.000 CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 2 in normal stream number 2 Stream flow area = 0.045(Ac.) Runoff from this stream = 0.267(CFS) CARLSBAD OAKS NORTH LOT 2 Page 5 of 10 Time of concentration = 3.06 mm. Rainfall intensity = 7.246(In/Hr) Summary of stream data: Stream Flow rate TC Rainfall Intensity No. (FS) (mm) (In/Hr) 1 4.684 5.11 7.149 2 0.267 3.06 7.246 Qmax(l) = 1.000 * 1.000 * 4.684) + 0.987 * 1.000 * 0.267) + = 4.948 Qmax(2) = 1.000 * 0.599 * 4.684) + 1.000 * 1.000 * 0.267) + = 3.074 Total of 2 streams to confluence: Flow rates before confluence point: 4.684 0.267 Maximum flow rates at confluence using above data: 4.948 3.074 Area of streams before confluence: 0.799 0.045 Results of confluence: Total flow rate = 4.948(CFS) Time of concentration = 5.105 mm. Effective stream area after confluence = 0.844 (Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to Point/Station 205.000 PIPEFLOW TRAVEL TIME (User specified size) **** Upstream point/station elevation 258.000(Ft.) Downstream point/station elevation = 257.890(Ft.) Pipe length = 23.00(Ft.) Slope = 0.0048 Manning's N = 0.013 No. of pipes 1 Required pipe flow = 4.948(CFS) Given pipe size = 18.00 (In.) Calculated individual pipe flow 4.948(CFS) Normal flow depth in pipe = 10.90(In.) Flow top width inside pipe = 17.59(m.) Critical Depth = 10.27(In.) Pipe flow velocity = 4.42(Ft/s) Travel time through pipe = 0.09 mm. Time of concentration (TC) = 5.19 mm. Process from Point/Station 205.000 to Point/Station 205.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 2 in normal stream number 1 Stream flow area = 0.844 (Ac.) Runoff from this stream = 4.948(CFS) Time of concentration = 5.19 mm. Rainfall intensity = 7.072(In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 401.000 to Point/Station 402.000 INITIAL AREA EVALUATION Decimal fraction soil group A 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 (UNDISTURBED NATURAL TERRAIN (Permanent Open Space Impervious value, Ai = 0.000 Sub-Area C Value 0.350 CARLSBAD OAKS NORTH LOT 2 Page 6 of 10 Initial subarea total flow distance = 106.000(Ft.) Highest elevation - 300.780(Ft.) Lowest elevation = 268.190(Ft.) Elevation difference = 32.590(Ft.) Slope = 30.745 % INITIAL AREA TIME OF CONCENTRATION CALCULATIONS: The maximum overland flow distance is 100.00 (Ft) for the top area slope value of 30.75 %, in a development type of Permanent Open Space In Accordance With Figure 3-3 Initial Area Time of Concentration 4.31 minutes TC (1.8*(1.1_C)*distance(Ft.).5)/(% slope(1/3)] TC = (1.8*(1.1_0.3500)*( 100.000.5)/( 30.745(1/3)]= 4.31 Calculated TC of 4.309 minutes is less than 5 minutes, resetting TC to 5.0 minutes for rainfall intensity calculations Rainfall intensity (I) = 7.246(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (QKCIA) is C = 0.350 Subarea runoff = 0.203(CFS) Total initial stream area = 0.080 (Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 402.000 to Point/Station 403.000 IRREGULAR CHANNEL FLOW TRAVEL TIME **** Estimated mean flow rate at midpoint of channel = 1.663(CFS) Depth of flow = 0.863(Ft.), Average velocity 2.979(Ft/s) ******* Irregular Channel Data *********** ----------------------------------------------------------------- Information entered for subchannel number 1 Point number 'X' coordinate 'Y' coordinate 1 0.00 32.50 2 67.00 2.00 3 68.00 0.00 4 69.00 1.00 Manning's 'N' friction factor = 0.015 ----------------------------------------------------------------- Sub-Channel flow = 1.663(CFS) flow top width 1.294 (Ft.) velocity= 2.979(Ft/s) area = 0.558(Sq.Ft) Froude number - 0.799 Upstream point elevation - 268.190(Ft.) Downstream point elevation = 263.000 (Ft.) Flow length = 931.000(Ft.) Travel time = 5.21 mm. Time of concentration = 9.52 mm. Depth of flow - 0.863(Ft.) Average velocity = 2.979(Ft/s) Total irregular channel flow = 1.663(CFS) Irregular channel normal depth above invert elev. = 0.863(Ft.) Average velocity of channel(s) - 2.979(Ft/s) Adding area flow to channel Rainfall intensity (I) = 4.783(In/Hr) for a 100.0 year storm Decimal fraction soil group A = 0.000 Decimal fraction soil group B - 0.000 Decimal fraction soil group C 0.000 Decimal fraction soil group D = 1.000 [UNDISTURBED NATURAL TERRAIN (Permanent Open Space Impervious value, Ai = 0.000 Sub-Area C Value = 0.350 Rainfall intensity = 4.783(In/Hr) for a 100.0 year storm Effective runoff coefficient used for total area (Q=KCIA) is C = 0.350 CA - 0.639 Subarea runoff = 2.856(CFS) for 1.747(Ac.) Total runoff = 3.059(CFS) Total area = 1.827(Ac.) Depth of flow - 1.076(Ft.), Average velocity = 3.536(Ft/s) CARLSBAD OAKS NORTH LOT 2 Page 7 of 10 Process from Point/Station 403.000 to Point/Station 205.000 PIPEFLOW TRAVEL TIME (User specified size) **** Upstream point/station elevation = 260.400(Ft.) Downstream point/station elevation = 260.040(Ft.) Pipe length = 72.00(Ft.) Slope - 0.0050 Manning's N = 0.013 No. of pipes = 1 Required pipe flow = 3.059(CFS) Given pipe size 18.00 (In.) Calculated individual pipe flow - 3.059(CFS) Normal flow depth in pipe = 8.05(In.) Flow top width inside pipe = 17.90(In.) Critical Depth = 7.97 (In.) Pipe flow velocity = 4.00(Ft/s) Travel time through pipe - 0.30 mm. Time of concentration (TC) = 9.82 mm. ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 205.000 to Point/Station 205.000 **** CONFLUENCE OF MINOR STREAMS Along Main Stream number: 2 in normal stream number 2 Stream flow area = 1.827(Ac.) Runoff from this stream = 3.059(CFS) Time of concentration - 9.82 mm. Rainfall intensity = 4.689(In/Hr) Summary of stream data: Stream Flow rate TC Rainfall Intensity No. (CFS) (mm) (In/Hr) 1 4.948 5.19 7.072 2 3.059 9.82 4.689 Qmax(1) = 1.000 1.000 * 4.948) + 1.000 * 0.529 * 3.059) + = 6.565 Qmax(2) - 0.663 * 1.000 * 4.948) + 1.000 * 1.000 * 3.059) + = 6.339 Total of 2 streams to confluence: Flow rates before confluence point: 4.948 3.059 Maximum flow rates at confluence using above data: 6.565 6.339 Area of streams before confluence: 0.844 1.827 Results of confluence: Total flow rate = 6.565(CFS) Time of concentration = 5.192 mm. Effective stream area after confluence - 2.671 (Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 205.000 to Point/Station 206.000 PIPEFLOW TRAVEL TIME (User specified size) **** Upstream point/station elevation = 257.790(Ft.) Downstream point/station elevation = 255.870 (Ft.) Pipe length = 384.00(Ft.) Slope = 0.0050 Manning's N = 0.013 No. of pipes 1 Required pipe flow = 6.565(CFS) Given pipe size = 18.00 (In.) Calculated individual pipe flow = 6.565(CFS) Normal flowdepth in pipe - 13.15(In.) Flow top width inside pipe - 15.97(In.) Critical Depth = 11.88 (In.) Pipe flow velocity = 4.75(Ft/s) Travel time through pipe = 1.35 mm. Time of concentration (TC) 6.54 mm. CARLSBAD OAKS NORTH 1012 Page 8 of 10 Process from Point/Station 206.000 to Point/Station 103.000 PIPEFLOW TRAVEL TIME (User specified size) **** Upstream point/station elevation - 253.500(Ft.) Downstream point/station elevation = 253.150(Ft.) Pipe length = 71.00(Ft.) Slope = 0.0049 Manning's N = 0.013 No. of pipes = 1 Required pipe flow = 6.565(CFS) Given pipe size = 18.00(m.) Calculated individual pipe flow - 6.565(CFS) Normal flow depth in pipe = 13.22(m.) Flow top width inside pipe = 15.90(In.) Critical Depth = 11.88(In.) Pipe flow velocity = 4.72(Ft/s) Travel time through pipe = 0.25 mm. Time of concentration (TC) = 6.79 mm. ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 103.000 to Point/Station 103.000 ** CONFLUENCE OF MAIN STREAMS **** The following data inside Main Stream is listed: In Main Stream number: 2 Stream flow area = 2.671(Ac.) Runoff from this stream = 6.565(CFS) Time of concentration = 6.79 mm. Rainfall intensity = 5.947(In/Hr) Summary of stream data: Stream Flow rate TC Rainfall Intensity No. (CFS) (mm) (In/Hr) 1 21.284 8.27 5.238 2 6.565 6.79 5.947 Qmax(1) 1.000 * 1.000 * 21.284) + 0.881 * 1.000 * 6.565) + 27.067 Qmax(2) = 1.000 * 0.821 * 21.284) + 1.000 * 1.000 * 6.565) + 24.049 Total of 2 main streams to confluence: Flow rates before confluence point: 21.284 6.565 Maximum flow rates at confluence using above data: 27.067 24.049 Area of streams before confluence: 4.955 2.671 Results of confluence: Total flow rate = 27.067(CFS) Time of concentration = 8.268 mm. Effective stream area after confluence = 7.626(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 103.000 to Point/Station 104.000 PIPEFLOW TRAVEL TIME (User specified size) **** Upstream point/station elevation = 242.530(Ft.) Downstream point/station elevation = 239.000(Ft.) Pipe length = 39.00(Ft.) Slope = 0.0905 Manning's N = 0.013 No. of pipes = 1 Required pipe flow = 27.067(CFS) Given pipe size = 30.00 (In.) Calculated individual pipe flow = 27.067(CFS) Normal flow depth in pipe = 9.54(In.) Flow top width inside pipe = 27.95(In.) CARLSBAD OAKS NORTH LOT 2 Page 9 of 10 Critical Depth = 21.28(m.) Pipe flow velocity = 20.15(Ft/s) Travel time through pipe = 0.03 mm. Time of concentration (TC) = 8.30 mm. Process from Point/Station 104.000 to Point/Station 104.000 **** SUBAREA FLOW ADDITION **** Rainfall intensity (I) = 5.225(In/Hr) for a 100.0 year storm Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 1.000 [LOW DENSITY RESIDENTIAL (1.0 DO/A or Less Impervious value, Ai = 0.100 Sub-Area C Value = 0.410 Time of concentration 8.30 mm. Rainfall intensity = 5.225(In/Hr) for a 100.0 year storm Effective runoff coefficient used for total area (Q=KCIA) is C = 0.690 CA = 5.594 Subarea runoff = 2.162(CFS) for 0.486(Ac.) Total runoff = 29.229(CFS) Total area = 8.112(Ac.) End of computations, total study area = 8.112 (Ac.) CARLSBAD OAKS NORTH 1012 Page 10 of 10 Hydrology Study ATTACHMENT F• POST DEVELOPED HYDROLOGY MAP - 1 LEGEND WATERCOURSE WATERSHED BOUNDARY N SUB—AREA BOUNDARY -------- -- NODE NUMBER - 7 v N - N \ LTFECJ7VESTUD,VAREA=.&IIACRES o-, 0/ / - \ YJQZ\JO"hDPC \ N - —-- / _'o V P[- 6202-TS '2 7 - 48 ,k'48 AT// BAS/N \\ \\ \ r (242 5J FZ--OUT 02 ARES 1O/i\ \ \ N \ \ N, V - 'V /103 \L\\ \ 25J5/Wt\' / \\I AN V V ms / os N VI J9592 A 110 A6 Jr 14 693 El ER -' V / o / \ / \ \ 0 5e IN AIR -511 44 A 265 411 4 N1 265 \N1 - < fz OUT 19 UREA J pz 268 — O' O[ SER EASEMENT 102 /5 l --- -- PROPERTY NO TREES/NEASEMENT rn TE-F0A1N BASIN 5/, I L/NE 7470 ACRES—— 2CJJOFL/N — - — (2 /M, 6C 10 FL OUT /8 PVC o.2gA Wf -5- 77 40 L / \ jJJ SCALE f'4O' 0 '10 80 720 760 CARLSBAD OAKS LOT 2 POST DEVELOPMENT