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HomeMy WebLinkAboutHydrology .- I ,. I I I I I I I I I 1\ I . I I I I I tbf/ INCLUDED WIT . HYDR~~ill~NC~~~~~!I~~~RU~~~~~ ~~~ PARCEL MA~ DRAIN FOR IN TH(FRONT STR~ Z~z.., E CITY OF TEMECULA . ~/prf~ fl$'CII~,;P ~~ ~cef do ?:;,vMf}JrJ a q:f:I, ~ ~ ~,f fto#' (1I,fet 7~ I, '00"- )/lIPf' /I r,; .... to"",.,., +~ __ ~/ 0 tic, ~ t'Y: '2. ,{; , .. "-'r~:'J~I., !ll It 'C rvP< f( VI' C'" '7 oJ), .", .. -:. JIflI fb! 4If't /::..J.Jt'O" p,#l "If OF "'-~~~ "1"11# t>< lfI P · If tp=ARED BY R __ ~' '.d(JP /It I Er. 1= l\ It: r> ./ ~fI1vP JUI 28100 I:: Lohr + A' C11Y~ . 0 ~'M","' ssoclates Inc ENGINEE,,",,"""""' ~~ ~_~ ~".""~ ~_ .AT",,! urveylng Ph 9096 Temecula, CA 92590 " 76-6726 Fax 909 699-0896 ATTENTION: HERMA N HOVAGIMYAN TELEPHONE" " (909) 676-6726 \ RECEIVED SEP 2 2 2000 CITY OF ~NGtNEERINJ~MECULA EPARTMENT I I I I I I I J f I I I I f I I ,I I I ffi1. 1-U, n (Ft?ON7 67/t13f:T) HYDROLOGY JOB. NO. 2C.oo3 BY lHEr<.rtlrl-N DATE 11111/'18 . I SHT. OF _ z-. 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I tJ.7I l't. n - 77,(J , ,.7/J 5,(. , f'J.7'Z Zoo ''I- 1 g.O 7 H.7 --li",,:-h IT-- I Ft.ottJ ex e~~Oi __~~~_ ~___________'__h:"'~::':"':~::':"':'::_"":'=-== I I a ~ I I f ,I I I I I I /..:~.- ."ultflPfVJ .J. /J.. ,,,t/PIP' , 1# [(III f/lvr~ ;1;1>' Azt 1f1f17 tb 0..1 ~ I /' Jt/,"{ )p~...J1 vP" I I I I I I I I I I I I I I ,I I I I I I I I I I I 9 Riverside County Rational Hydrology Program CIVILCADD/CIVILDESIGN Engineering Software, (c) 1989 - 1998 Version 5.1 Rational Hydrology Study Date: 07/19/00 File:P28627.out PM 28627 HYDROLOGY ANALYSIS 10 YEAR STORM IN 26003 ********* Hydrology Study Control Information ********** English (in-lb) Units used in input data file Lohr + Associates, Inc., Temecula, California - SIN 773 Rational Method Hydrology Program based on Riverside County Flood Control & Water Conservation District 1978 hydrology manual Storm event (year) = 10.00 Antecedent Moisture Condition = 2 Standard intensity-duration curves data (Plate D-4.1) For the [ Murrieta,Tmc,Rnch CaNorco ] area used. 10 year storm 10 minute intensity = 2.360(In/Hr) 10 year storm 60 minute intensity = 0.880(In/Hr) 100 year storm 10 minute intensity = 3.480(In/Hr) 100 year storm 60 minute intensity = 1.300(In/Hr) Storm event year = 10.0 Calculated rainfall intensity data: 1 hour intensity = 0.880(In/Hr) Slope of intensity duration curve = 0.5500 -ri<~..e /" ~':7j~.) +++++++++++++++++++++++++++++++++ Process from Point/Station 00.000 **** INITIAL AREA EVALUATION * +++++++++ + 102.00 Initial area flow distance = 570.000(Ft.) Top (of initial area) elevation = 1002.200(Ft.) Bottom (of initial area) elevation: 994.400(Ft.) Difference in elevation = 7.800(Ft.~ Slope = 0.01368 s(percent) = 1.37 TC = k(0.300)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 8.958 min. Rainfall intensity = 2.505(In/Hr) for a 10.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.873 Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 1. 000 A - I Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 \0 I I I I I I I I I I I I I I I I I I I {o Initial subarea runoff = Total initial stream area = Pervious area fraction = 0.100 2.866(CFS) 1.310(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 102.000 to Point/Station 102.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 1 Stream flow area = 1.310(Ac.) Runoff from this stream = 2.866(CFS) Time of concentration = 8.96 min. Rainfall intensity = 2.505(In/Hr) +++++++++++++++++++++++++++++++++++ ++++++++++++++++++++++ Process from Point/Station 1.000 to int/Station **** INITIAL AREA EVALUATION Initial area flow distance = 520.000(Ft.) Top (of initial area) elevation = 98.600(Ft.) Bottom (of initial area) elevation = 94.400(Ft.) Difference in elevation = 4.200(Ft.) Slope = 0.00808 s (percent) = 0.81 TC = k(0.300)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 9.596 min. Rainfall intensity = 2.412(In/Hrl for a 10.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.873 Dec~mal fraction soil group A = 0.000 A_~ Dec1mal fraction soil group B = 1.000 n ~ Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Initial subarea runoff = 4.041(CFS) Total initial stream area = 1.920(Ac.) Pervious area fraction = 0,100 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 102.000 to Point/Station 102.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 2 Stream flow area = 1.920(Ac.) Runoff from this stream = 4.041(CFS) Time of concentration = 9.60 min. Rainfall intensity = 2.412(In/Hr) Summary of stream data: Stream No. Rainfall Intensity (In/Hr) Flow rate (CFS) TC (min) 1 2 Largest Qp = 2.866 8.96 4.041 9.60 stream flow has longer time of 4.041 + sum of ~ 2.505 2.412 concentration I I I I I I I I I I I .' I I I I I I I 1/ Qp = Qb 2.866 * 6.801 Ia/Ib 0.963 = 2.760 Total of 2 streams to confluence: Flow rates before confluence point: 2.866 4.041 Area of streams before confluence: 1.310 1.920 Results of confluence: Total flow rate = Time of concentration Effective stream area 6.801(CFS) = 9.596 min. after confluence = 3.230(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from point/Station 200.000 to point/Station 201.000 **** INITIAL AREA EVALUATION **** Initial area flow distance = 650.000(Ft.) Top (of initial area) elevation = 1001.300(Ft.) Bottom (of initial area) elevation = 994.500(Ft.) Difference in elevation = 6.800(Ft.) Slope = 0,01046 s(percent) = 1.05 TC = k(0.300)*[(length-3)/(elevation change)]-0.2 Initial area time of concentration = 9.962 min. Rainfall intensity = 2.362(In/Hr) for a 10.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.872 Decimal fraction soil group A = 0.000 6-( Decimal fraction soil group B = 1.000 Decimal fraction soil group C = 0,000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Initial subarea runoff = 5.420(CFS) Total initial stream area = 2.630(Ac.) Pervious area fraction = 0.100 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 201.000 to Point/Station 204,000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** TOp of street segment elevation = 994.500(Ft.) End of street segment elevation = 991.100(Ft.) Length of street segment = 580.000(Ft.) Height of curb above gutter flowline = 8.0(In.) Width of half street (curb to crown) = 28.000(Ft.) Distance from crown to crossfall grade break = 26.000(Ft.) Slope from gutter to grade break (v/hz) = 0.080 Slope from grade break to crown (v/hz) = 0.020 Street flow is on [1] side(s) of the street Distance from curb to property line = 11.000(Ft.) Slope from curb to property line (v/hz) = 0.020 Gutter width = 2.000(Ft.) Gutter hike from flowline = 2.000(In.) Manning'S N in gutter = 0.0150 Manning's N from gutter to grade break = 0.0150 Manning's N from grade break to crown = 0.0150 \3-2 ,1/ I I I I I I I I I I I I, I 1 I II I I I Estimated mean flow rate at midpoint of street = 9.727(CFS) Depth of flow = 0.512(Ft.), Average velocity = 2.540(Ft/s) Streetflow hydraulics at midpoint of street travel: Halfstreet flow width = 19.244(Ft.) Flow velocity = 2.54(Ft/s) Travel time = 3.81 min. TC = 13.77 min. Adding area flow to street COMMERCIAL subarea type 13 2 Runoff Coefficient = 0.869 - Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 1.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Rainfall intensity = 1.977(In/Hr) for a 10.0 year storm Subarea runoff = 7.181(CFS) for 4,180(Ac.) Total runoff = 12.601(CFS) Total area = 6.810(Ac.) Street flow at end of street = 12.601(CFS) Half street flow at end of street = 12.601(CFS) Depth of flow = 0.552(Ft.), Average velocity = 2.706(Ft/s) Flow width (from curb towards crown)= 21.282(Ft.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to point/Station 204.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 1 Stream flow area = 6.810(Ac.) Runoff from this stream = 12.601(CFS) Time of concentration = 13.77 min. Rainfall intensity = 1.977(In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 202.000 to Point/Station 203.000 **** INITIAL AREA EVALUATION **** Initial area flow distance = 610.000(Ft.) Top (of initial area) elevation = 98.600(Ft.) Bottom (of initial area) elevation = 94.500(Ft.) Difference in elevation = 4.100(Ft.) Slope = 0.00672 s (percent) = 0.67 TC = k(0.300)*[(lengthA3)/(elevation change)] AO.2 Initial area time of concentration = 10.611 min. Rainfall intensity = 2.282(In/Hr) for a 10.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.872 Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 1.000 Decimal fraction soil group C = 0.000 B-3 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Initial subarea runoff = 3.083(CFS) Total initial stream area = 1.550(Ac.) Pervious area fraction = 0.100 \~ I I I I I I I I I I I I I I I I I I I 15 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 203.000 to Point/Station 204.000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** Top of street segment elevation: 94.500(Ft.) End of street segment elevation: 91.100(Ft.) Length of street segment : 580.000(Ft.) Height of curb above gutter flowline = 6.0(In.) Width of half street (curb to crown) : 28.000(Ft.) Distance from crown to crossfall grade break : 26.000(Ft.) Slope from gutter to grade break (v/hz): 0.080 Slope from grade break to crown (v/hz) : 0,020 Street flow is on [1] side(s) of the street Distance from curb to property line : 11.000(Ft.) Slope from curb to property line (v/hz): 0.020 Gutter width: 2.000(Ft.) Gutter hike from flowline: 2.000(In.) Manning's N in gutter: 0.0150 Manning's N from gutter to grade break: 0.0150 Manning's N from grade break to crown: 0.0150 Estimated mean flow rate at midpoint of street: 3.680(CFS) Depth of flow: 0.388(Ft.), Average velocity: 2.008(Ft/s) Streetflow hydraulics at midpoint of street travel: Halfstreet flow width: 13.062(Ft.) Flow velocity: 2.01(Ft/s) Travel time: 4.81 min. TC: 15.43 min. B-4 Adding area flow to street COMMERCIAL subarea type Runoff Coefficient: 0.868 Decimal fraction soil group A : 0.000 Decimal fraction soil group B : 1.000 Decimal fraction soil group C : 0.000 Decimal fraction soil group D : 0.000 RI index for soil(AMC 2) : 56.00 Pervious area fraction: 0.100; Impervious fraction: 0.900 Rainfall intensity: 1.857(In/Hr) for a 10.0 year storm Subarea runoff: 0.967(CFS) for 0.600(Ac.) Total runoff: 4.050(CFS) Total area: 2.150(Ac.) Street flow at end of street: 4.050(CFS) Half street flow at end of street: 4.050(CFS) Depth of flow: 0.398(Ft.), Average velocity: 2.054(Ft/s) Flow width (from curb towards crown): 13.583(Ft.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to Point/Station 204.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 2 Stream flow area: 2.150(Ac.l Runoff from this stream: 4.050(CFS) Time of concentration: 15.43 min. Rainfall intensity: 1.857(In/Hr) Summary of stream data: Stream No. Flow rate (CFS) Rainfall Intensity (In/Hr) TC (min) 1 12.601 13.77 \~ 1. 977 I I I I I I I I I I I I I I I I I I I (4 4.050 15.43 1.857 stream flow has longer or shorter time of concentration 12.601 + sum of Qa Tb/Ta 4.050 * 0.893 = 3.615 16.216 2 Largest Qp = Qp = Total of 2 streams to confluence: Flow rates before confluence point: 12.601 4.050 Area of streams before confluence: 6.810 2.150 Results of confluence: Total flow rate = 16.216(CFS) Time of concentration = 13.769 min. Effective stream area after confluence = End of computations, total study area = The following figures may be used for a unit hydrograph study of the Area averaged pervious area fraction(Ap) = Area averaged RI index number = 56.0 8.960 (Ac.) 12.19 (Ac.) same area. 0.100 \~ I I I I I I I I I I I I I I I I I I I 15 \~ I I I I I I I I I I I I I I I I I I I I~ Riverside County Rational Hydrology Program CIVILCADD/cIVILDESIGN Engineering Software, (c) 1989 - 1998 Version 5.1 Rational Hydrology Study Date: 07/19100 File:P28627.out ------------------------------------------------------------------------ PM 28627 HYDROLOGY ANALYSIS 100 YEAR STORM IN 26003 ------------------------------------------------------------------------ ********* Hydrology Study Control Information ********** English (in-lb) Units used in input data file ------------------------------------------------------------------------ Lohr + Associates, Inc., Temecula, California - SIN 773 ------------------------------------------------------------------------ Rational Method Hydrology Program based on Riverside County Flood Control & Water Conservation District 1978 hydrology manual Storm event (year) = 100.00 Antecedent Moisture Condition = 2 Standard intensity-duration curves data (Plate D-4.1) For the [ Murrieta,Tmc,Rnch CaNorco J area used. 10 year storm 10 minute intensity = 2.360(In/Hr) 10 year storm 60 minute intensity = 0.880(In/Hr) 100 year storm 10 minute intensity = 3,480(In/Hr) 100 year storm 60 minute intensity = 1.300(In/Hr) Storm event year = 100.0 Calculated rainfall intensity data: 1 hour intensity = 1.300(In/Hr) Slope of intensity duration curve = 0.5500 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 100.000 to Point/Station 102.000 **** INITIAL AREA EVALUATION **** Initial area flow distance = 570.000(Ft.) Top (of initial area) elevation = 1002,200(Ft.) Bottom (of initial area) elevation = 994.400(Ft.) Difference in elevation = 7.800(Ft.) Slope = 0.01368 s(percent) = 1,37 TC = k(0.300) * [(length^3)1 (elevation change)J^O,2 Initial area time of concentration = 8.958 min. Rainfall intensity = 3.700(In/Hr) for a 100.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.880 Decimal fraction soil group A = 0,000 A- l Decimal fraction soil group B = 1.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 \1 Pervious area fraction = 0.100; Impervious fraction = 0.900 I I I I I I I I I I I I I I I I I I I 17 Initial subarea runoff = Total initial stream area = Pervious area fraction = 0.100 4.266{CFS) 1.310{AC.} ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 102.000 to Point/Station 102.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 1 Stream flow area = 1.310{AC.} Runoff from this stream = 4.266{CFS} Time of concentration = 8.96 min. Rainfall intensity = 3.700{In/Hr} ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 101.000 to Point/Station 102.000 **** INITIAL AREA EVALUATION **** Initial area flow distance = 520.000{Ft.} Top {of initial area} elevation = 98.600{Ft.) Bottom {of initial area} elevation = 94,400{Ft.} Difference in elevation = 4.200{Ft.} Slope = 0.00808 s (percent) = 0.81 TC = k{O.300}*[{length^3}/{elevation change}]^0.2 Initial area time of concentration = 9.596 min. Rainfall intensity = 3,563 {In/Hr} for a 100.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.880 Decimal fraction soil group A = 0.000 A Decimal fraction soil group B = 1,000 (-i - 2 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Initial subarea runoff = 6.017{CFS} Total initial stream area = 1.920{Ac.} Pervious area fraction = 0.100 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 102.000 to Point/Station 102.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 2 Stream flow area = 1.920{Ac.} Runoff from this stream = 6.017{CFS} Time of concentration = 9.60 min. Rainfall intensity = 3.563 {In/Hr} Summary of stream data: Stream No, Rainfall Intensity {In/Hr} Flow rate {CFS} TC {min} 1 2 Largest Qp = 4.266 8.96 6.017 9.60 stream flow has longer time of 6.017 + sum of \'C 3.700 3.563 concentration II II I I I I I I I I I I I I I I I I I 18 Qp = Qb 4.266 * ~0.~24 Ia/Ib 0.963 = 4.~08 Total of 2 streams to confluence: Flow rates before confluence point: 4.266 6.017 Area of streams before confluence: 1.3~0 ~.920 Results of confluence: Total flow rate = 10.124(CFS) Time of concentration = 9.596 min. Effective stream area after confluence = 3.230(Ac.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 200.000 to Point/Station 20~.000 **** INITIAL AREA EVALUATION **** Initial area flow distance = 650.000(Ft.) Top (of initial area) elevation = 1001.300(Ft.) Bottom (of initial area) elevation = 994.500(Ft.) Difference in elevation = 6.800(Ft.) Slope = 0.0~046 s(percent) = ~.05 TC = k(0.300)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 9.962 min. Rainfall intensity = 3.490(In/Hr) for a 100.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.879 Decimal fraction soil group A = 0.000 Decimal fraction soil group B = ~. 000 B-1 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56,00 Pervious area fraction = O.~OO; Impervious fraction = 0.900 Initial subarea runoff = 8.070(CFS) Total initial stream area = 2,630(Ac.) Pervious area fraction = 0.100 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from point/Station 20~.000 to Point/Station 204.000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** Top of street segment elevation = 994.500(Ft.) End of street segment elevation = 99~.100(Ft.) Length of street segment = 580.000(Ft.) Height of curb above gutter flowline = 8.0(In.) Width of half street (curb to crown) = 28.000(Ft.) Distance from crown to crossfall grade break = 26.000(Ft.) Slope from gutter to grade break (v/hz) = 0.080 Slope from grade break to crown (v/hz) = 0.020 Street flow is on [1] side(s) of the street Distance from curb to property line = ~l. 000 (Ft.) D _~ Slope from curb to property line (v/hz) = 0.020 IJ ~ Gutter width = 2.000(Ft.) Gutter hike from flowline = 2.000(In.) Manning'S N in gutter = 0.0~50 Manning's N from gutter to grade break = 0.0150 \~ Manning'S N from grade break to crown = 0.0150 I I I I I I I I I I I I I I I I , I I I \~ Estimated mean flow rate at midpoint of street = 14.483(CFS) Depth of flow = O,576(Ft.), Average velocity = 2.801(Ft/s} Streetflow hydraulics at midpoint of street travel: Halfstreet flow width = 22.460(Ft.} Flow velocity = 2.80(Ft/s) Travel time = 3.45 min. TC = 13.41 min. Adding area flow to street COMMERCIAL subarea type B-2 Runoff Coefficient = 0.876 Decimal fraction soil group A = 0.000 Decimal fraction soil group B = 1.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Rainfall intensity = 2.963 (In/Hr) for a 100.0 year storm Subarea runoff = 10.857(CFS} for 4.180(Ac.} Total runoff = 18.927(CFS} Total area = 6.810(Ac.) Street flow at end of street = 18.927(CFS) Half street flow at end of street = 18.927(CFS} Depth of flow = 0,625(Ft.}, Average velocity = 2.992(Ft/s} Flow width (from curb towards crown)= 24.898(Ft.} ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to Point/Station 204.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 1 Stream flow area = 6.810(Ac.} Runoff from this stream = 18.927(CFS) Time of concentration = 13.41 min. Rainfall intensity = 2.963 (In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 202.000 to Point/Station 203.000 **** INITIAL AREA EVALUATION **** Initial area flow distance = 610.000(Ft.) Top (of initial area) elevation = 98.600(Ft.) Bottom (of initial area) elevation = 94.500(Ft.} Difference in elevation = 4.100(Ft.} Slope = 0.00672 s(percent} = 0.67 TC = k(0.300)*[(length~3)/(elevation change)]~0.2 Initial area time of concentration = 10,611 min. Rainfall intensity = 3.371(In/Hr} for a 100.0 year storm COMMERCIAL subarea type Runoff Coefficient = 0.879 Decimal fraction soil group A = 0.000 B _ ::2 Decimal fraction soil group B = 1.000 J Decimal fraction soil group C = 0,000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Initial subarea runoff = 4.591(CFS} Total initial stream area = 1.550(AC,} Pervious area fraction = 0.100 7,.0 I I I I I I I I I I I , I I I I I I I I :20 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 203.000 to Point/Station 204.000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** TOp of street segment elevation = 94,500(Ft.) End of street segment elevation = 91.100(Ft.) Length of street segment = 580.000(Ft.) Height of curb above gutter flowline = 6.0(In.) Width of half street (curb to crown) = 28.000(Ft.) Distance from crown to crossfall grade break = 26.000(Ft.) Slope from gutter to grade break (v/hz) = 0.080 Slope from grade break to crown (v/hz) = 0.020 Street flow is on [1] side(s) of the street Distance from curb to property line = 11.000(Ft,) Slope from curb to property line (v/hz) = 0.020 Gutter width = 2.000(Ft.) Gutter hike from flowline = 2.000(In.) Manning's N in gutter = 0.0150 Manning's N from gutter to grade break = 0.0150 Manning's N from grade break to crown = 0.0150 Estimated mean flow rate at midpoint of street = 5.480(CFS) Depth of flow = 0.434(Ft.), Average velocity = 2.209(Ft/s) Streetflow hydraulics at midpoint of street travel: Halfstreet flow width = 15.343 (Ft.) f3 - 4- Flow velocity = 2.21(Ft/s) Travel time = 4.38 min, TC = 14.99 min. Adding area flow to street COMMERCIAL subarea type Runoff Coefficient = 0.875 Decimal fraction soil group A = 0,000 Decimal fraction soil group B = 1.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 RI index for soil(AMC 2) = 56.00 Pervious area fraction = 0.100; Impervious fraction = 0.900 Rainfall intensity = 2.788(In/Hr) for a 100.0 year storm Subarea runoff = 1.464(CFS) for 0.600(Ac.) Total runoff = 6.055(CFS) Total area = 2.150(Ac,) Street flow at end of street = 6.055(CFS) Half street flow at end of street = 6.055(CFS) Depth of flow = 0.446(Ft.), Average velocity = 2.263(Ft/s) Flow width (from curb towards crown)= 15.967(Ft.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 204.000 to Point/Station 204.000 **** CONFLUENCE OF MINOR STREAMS **** Along Main Stream number: 1 in normal stream number 2 Stream flow area = 2.150(Ac.) Runoff from this stream = 6.055(CFS) Time of concentration = 14.99 min. Rainfall intensity = 2.788(In/Hr) Summary of stream data: Stream No. Flow rate (CFS) TC (min) Rainfall Intensity (In/Hr) 1 "],.\ 18.927 13 .41 2.963 1 I I I I I I I I I I I I I I I I I I 6.055 14.99 2.788 stream flow has longer or shorter time of concentration 18,927 + sum of Qa Tb/Ta 6,055 * 0.895 = 5.420 24.346 2 Largest Qp = . Qp = Total of 2 streams to confluence: Flow rates before confluence point: 18.927 6.055 Area of streams before confluence: 6.810 2.150 Results of confluence: Total flow rate = 24.346{CFS) Time of concentration = 13.414 min. Effective stream area after confluence = End of computations, total study area = The following figures may be used for a unit hydrograph study of the Area averaged pervious area fraction (Ap) = Area averaged RI index number = 56.0 -Zl 8.960 (Ac.) 12.19 (Ac.) same area. 0.100 1,1; I 1 1 I I I I I I I I I I I I 1 I I I " 'FM '2 x<:. '27 (P':?o/J-r ~TRfn?T) ~ HYDRAULI CS " \ JIHlNl, :2<:'0""3 n IkKrl114N oom Ifjlrl'"f8 SHT, ~'2 DIF 1,.'? I I I 1 I 1 I I I I I I I 1 1 I I I I crt .... ......_ Vl ~z 1 I 1 I I I I I I 1 I I I I 1 1 I I I LOHR + ASSOCIATES INC. PM '28C. 27 43513 RIDGE PARK DRIVE TEMECULA, CA 92590 PH. 9O!Ui7lHl726 FAX 90!Ui99-0896 . LAND PLANNING. CIVIL ENGINEERING. SURVEYING JOB No. BY DATE SHT, OF ?G <>03 If-t?tem/'H.I 11/1'1/'18 24 c, 1,3, ~ 71-f(; t:A1D ~F Ff;!'oN I' 071!?€ ET e,-, 0, ~ , (J - 24,35 eF'~ (00- /.l AIIJ",'30",(.. ) U( '" 3, (:J ( CA 7 'r' CJ F ,(, If, C:IHMT L t.. - 15 /, /, 0, ~ t 4, 3S ::. S. Q " C), ~ 7 uJ . .0,6 uJ.... 13,20' UjE W., /4-' ~~ () 0 r "0 I> I> ;:; "0 r--l:>'o ()m--l<- ci (/1m ~~I~I~ ~~I~I~ ~I"'~I><> ~I~I'I~ I I I I I, I I I r;-I r- 0- :r ., + )> III III o o ..... o r+ C1l III ~ I rl - . . . , ~ -.. .-~ ~ - ; oJ g m _' , - . , :'"~ , ; I ~~, . u .1 _ : u :;~ , . n. > . ~ '",. N , ". Z8!?, . . 3:7' I' ~ 3:T~ <^ <:r. r II u H " o g;;9 ~ < coCl) 0 0 "" 3' :> - N :> r,o (]I 00 (/I.o(ll(]l --I '" -, 3:: );> <.n:J N . ~:x: ~'< :) p.. II ~G) -= 0.... - 00 .l> -a. CD ~ __ 0\ :;'g ........ 0- :> ~x ~ . Gl ~ - I , ~' :(/1 :) '- (j) :t ,,0 m m ~ ;-i , - :~ < :\SI _I :1:: < - 0 ? :n . -. :7': - . . . . - . t>: -<' :7' .. ..? (/I ~ --I o Z (/I m () --I o Z o ~ 3: ^ < r -.. CO> " -I i- II C '" o ?'> a c;-z. ""~ C'\+ u . '" A U> \JO ~ "-" 6' U> '" r, ~o. 10 Ef.:-:::. c, __.L... /.~ .? .~ /0 ~ '~,j' - , : . . , -. -- - - - - . . , ,... . . . . I . . . : , . . , . - , . , . . - - I . . . . , i : 4)C>o DC;) 00 l{' ~}::I-.I:-,,-~ ^ .:n <:::lI lO ("u ~ ~ ~ ~f;'--t'-C>.t:JO.~O Y' ~ Q; ~ :t:. >L~ !' "- ~ c> ,. to ..... - t-;::' - - ~ ~ ~ - - ~ III ~ Ol. .." ~ ::! if ill t\ C '" () t \l I I 1 1 I 1 I I I I I , I I I I I I I I 2t; Circular Channel Analysis & Design Solved with Manning's Equation Open Channel - Uniform flow Worksheet Name: PM 28627 - LINE"A" Comment: IN 26003 - 6/24/00 Solve For Actual Depth Given Input Data: Diameter.......... Slope. . . . . . . . . . . . . Manning's n.,..... Discharge......... Computed Results: Depth, . . . . . . . , . . . . Velocity. . . . . . . . . . Flow Area......... Critical Depth".. Critical Slope.... Percent Full.,.... Full Capacity..... QMAX @.94D........ Froude Number..... r. ri{;ca( Ve!ocl-L:J.. , . . 2.00 ft 0.0160 ft/ft 0.013 24.35 cfs 1. 42 ft 10.23 fps 2.38 sf 1. 74 ft 0.0105 ft/ft 70.88 % 28.62 cfs 30.78 cfs 1.57 (flow is Supercritical) 8,510 t/,,$ Open Channel Flow Module, Version 3.43 (c) 1991 Haestad Methods, Inc. * 37 Brookside Rd * Waterbury, Ct 06708 '2-1