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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 />6. LITTLE JOHNSON/SECURITY CREEK <br /> <br />6.1. Watershed Description <br /> <br />The Little Johnson/Security Creek watershed is located south of Colorado Springs and <br />incorporates the town of Security, The basin lies generally between the railroad which parallels <br />Fountain Creek on the west and the Windmill Gulch basin to the east The basin consists of three <br />distinct areas which drain to Crews Gulch: (1) the Little Johnson Reservoir area, (2) Security area, <br />and (3) the Widefield area (Figure 6,1), <br /> <br /> <br />The basin area of Little Johnson/Security Creek at the confluence with Crews Gulch, excluding <br />Windmill Gulch is 3,12 square miles, This includes a 0,51 square mile area above Canal #4 which <br />is partially diverted to Windmill Gulch (50 cfs diversion to Windmill Gulch), Windmill Gulch streamflow <br />is conveyed via a 12-foot diameter culvert directly to Fountain Creek and therefore bypasses the Little <br />Johnson/Security Creek system, However, during the 100-year event the conveyance capacity of the <br />culvert is slightly surpassed and the resulting overflow is contributed to the Security Creek drainage, <br />The drainage basin area of Windmill Gulch is 3,38 square miles which results in a total tributary area <br />of 6,0 square miles, An area west of Grinnell discharges into this basin from Big Johnson/Crews <br />Gulch basin, <br /> <br /> <br />The majority of the watershed is urbanized, Land uses include industrial and commercial <br />properties, but the dominant land use is residential. Soils are predominantly Type "A" and "B" <br />hydrologic types as categorized by the SCS with some type "C" soils along the railroad on the west <br />side of the watershed, <br /> <br />6.2. Previous Studies <br /> <br />Two previous studies were available for review: (1) the FIS - EI Paso County, Unincorporated <br />Areas (Ref, 6,1), and (2) the Little Johnson/Security Creek Drainage Basin Planning Study (Ref, 6,2), <br />The FIS used synthetic unit hydrographs to develop peak discharges, The Little Johnson/Security <br />Creek Drainage Basin Planning Study used methods previously specified in Colorado Springs drainage <br />criteria to compute peak discharges, However, this study estimated discharges associated with the <br />100- year, 2-hour storm duration with AMC III. Current specification require use of the 24-hour <br />duration storm with AMC II conditions, <br /> <br />Peak discharges at the confluence with Crews Gulch are presented in Table 6.1 for the two <br />studies, <br /> <br />6,1 Resource Consultants & Engineers, Inc, <br />