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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />HYDRAULIC ANALYSES <br /> <br />TABLE 9 <br />SUMMARY OF DISCHARGES <br /> <br />Location <br /> <br />Quai 1 Creek <br />South 124th Street <br />Downstream from Tributary 0 <br />Lowell Boulevard <br />Downstream from Tributaries B&C <br />Zuni Street <br />Huron Street <br />Confluence with Big Dry Creek <br /> <br />Tributary A <br />Zuni Street <br />Confluence with Quail Creek <br /> <br />Tributary B <br />Upstream from 144th Avenue <br />Confluence with Quail Creek <br /> <br />Tributary C <br />Upstream Limit of Study <br />Confluence with Tributary B <br /> <br />Tributa ry 0 <br />South 124th Street <br />Confluence with Quail Creek <br /> <br />McKay Lake Basin <br />Downstream from W. l44th Ave. <br />Huron Street <br />Interstate 25 <br />Confluence with Southern Drainageway <br />Confluence with Big Dry Creek <br /> <br />General <br /> <br />10-Year <br />(cfs) <br /> <br />100-Year <br />(cfs) <br />- <br /> <br />The water surface profiles for all streams under study were computed using the <br />U.S. Army Corps of Engineers HEC-2 computer model (Reference 7). Cross sections <br />for streams analyzed herein were taken directly from the two foot contour mapping <br />prepared for this study (References 8 and 9). Field surveys were conducted where <br />more detailed elevation data were required. <br /> <br />190 <br />400 <br />830 <br />1,480 <br />1,730 <br />1,840 <br />1,770 <br /> <br />360 <br />830 <br />1,730 <br />2,990 <br />3,510 <br />3,790 <br />3,690 <br /> <br />Geometric measurements and invert elevations for bridge and culvert crossings <br />were obtained in the field as required. Photographs were taken of each crossing <br />and a sketch of the crossing was prepared showing appropriate dimensions, This <br />material is on file as backup information to the project. During these field <br />investigations, estimates of roughness coefficients, i.e. Manning's "n" values, <br />were also noted. <br /> <br />30 <br />100 <br /> <br />70 <br />190 <br /> <br />320 <br />50 <br /> <br />610 <br />820 <br /> <br />60 <br />280 <br /> <br />110 <br />540 <br /> <br />The "n" values utilized in the hydraulic analyses ranged from .030 to .045 for <br />the channel and from .025 to .070 for the overbanks. <br /> <br />110 <br />170 <br /> <br />220 <br />360 <br /> <br />Hydraul ic runs were completed for the lO-year and lOO-year events for streams <br />analyzed in this study. In addition, a floodway was computed for all streams <br />under study. Thi s floodway is based on the Urban Drai nage and Flood Control <br />District criteria allowing for no more than a one-half foot rise in the energy <br />grade line with encroachment during the 100-year event. <br /> <br />440 <br />800 <br />960 <br />1,530 <br />1,580 <br /> <br />910 <br />1,670 <br />1,920 <br />2,980 <br />3,080 <br /> <br />Culvert blockage was considered at each crossing structure. With the exception of <br />the Osage, Kalamath, and Huron crossings, all culverts were assumed to be com- <br />pletely blocked. <br /> <br />McKay Lake IlIpouOOlent <br /> <br />McKay Lake is a man-made reservoir constructed for storage of irrigation water. <br />The reservoir is created by two earthen entlankments located along the southern <br />and eastern sides of the reservoir. There is no emergency spillway structure at <br />this reservoir. The configuration of the McKay Lake impoundment presents some <br /> <br />17 <br />