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<br />fh€ proposid Spring Creek inflo'"" frolT- each of t,'le irrig~ticn canals determined <br />in the pre li mifl;J.ry des1gn of importation facil1ties 1s presented inf able 2. <br /> <br />For both existing and future conditions, drainage ~rea tributary to Dixon Reser- <br />voir was considered non~contributing. Calculations showed the maximum outflow <br /> <br />Table 2 <br /> <br />from this reservoir to be approximately 25-cfs, and this peak would occur much <br />later than flood peah on Spring Creek. <br /> <br />Canal Importation, Peak Inflows <br />lOO.YearPeaklnflol<< <br /> <br />Canal <br /> <br />Ple~sant Valley and Lake Canal <br /> <br />380-cfs <br /> <br />For existing conditions, the Spring Creek Basin was divided into 66 sub-basins <br />with 59 channel elements. Future urbanization included theS,[MM model from the <br /> <br />LnirnerCounty n and New Mercer <br />Canal. Mulberry Street to <br />Stuart Street <br /> <br />900-cfs <br /> <br />canal importation study prepared by Resource Consultants. ~ith this SWMM model <br />feeding directly intotheSpringCreekbasinmodel,a total of 105 sub-basins <br />and 118 channel elements were included in the analysis. <br /> <br />Larimer <br />Canal <br />Creek <br /> <br />County 12 and <br />Stuart Street <br /> <br />New Mercer <br />to Spring <br /> <br />210-cfs <br /> <br />those of Spring Creek. Therefore, the inflows frOM Canal Importation ha~e 1 ittle <br />effect on the total discharge for Spring Creek. <br /> <br />The sub-basin areas, basin and channel s.lopes, thewidthofoverlandf1ow,lOd <br />the lengths of channels were taken from the U. S. Geological Survey's 7.5 min- <br />ute quadrangl e mapping (Reference 17) and SUilpl~mental infomation 'o'Ias t,1ken 3'i <br />needed from the topographic mapping provided by the City of Fort Collins (Refer- <br /> <br />Thehydrographpeaks fer the irrigation canals didnotcombinedir ectlywith <br /> <br />ence16). <br /> <br />~drolo.gic Procedure <br />fhe SWMM rnodel was prepared for existing ~nd future basin conditions separately. <br />Exi st ing tondi t ions reflect tas j n urban i l~t ion as of J anu~ry, 1980 and ignore <br />cl1na11mportationplans. The existing condition also ignores the irrigation <br />c~na1S that cross the basin. Future conditions reflect basin development as <br /> <br />He percent of impervious co~er was determined by ident ifyin9 land uses throuqh- <br />out the basin from planning and zoning maps of the City of Fort Collins and <br />LarimerCeunty(References17and18). Typical values of the percentage of lm- <br />pervious area for each land use were then assigned and an imper~ious percentage <br /> <br />identified on planning and loning maps of the City of Fort collins and Larimer <br />County. In Larimer Countj, ueas currently zoned agricultural were changedtc <br />lightresidel1tial which is tlie expected type of development. Canal importation <br />....as included in this analysis to reflect the preli~inary design discharges pre- <br />pared by Resource Consultants. In this case, a11 storm wJter drainage abo~e the <br /> <br />was esti'!'ated for E'ach ~IJl>-l>~~ in. Thl' pl'rrentagl' of i'lpl'rviolls a rea assumed for <br /> <br />each land use is presented in Ta~le 3. <br /> <br />C<lna 1 s W"S a~~u;r,ed to be in te !'\':epted by the cana 1 ~, however. some excess flows <br /> <br />R~ infd 11 d<lta WdS the Sa'fl2 for both exis ti ng and future conditi ons. The ra i n fa 11 <br />depths werE' Obtained from the Precipitation-Frequency Atla, o' the Western U~ited <br />States (Reference Ig). The tota 1 ra intal1 depth for th~ flood events andly~ed in <br />this study are presented in Table 4. <br /> <br />were considered to spil1 across the canals. <br /> <br />.13- <br /> <br />-14- <br />