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<br />Secondly, peak flows and runoff volumes were compared to previous studies by ASI, <br />USACE, and UDFCD. The other studies used some different assumptions and also <br />different modelling techniques than were used in this study. However, comparison between <br />studies can still be made by careful analysis of the data from the previous studies. <br /> <br />The UDFCD-ca1culated peak inflow to Standley Lake compares closely with the value <br />calculated in this Master Plan (4 percent to 22 percent higher). <br /> <br />The relevant different assumptions used in the previous studies are as follows: <br /> <br />FUTURE BASIN HYDROLOGY <br /> <br />1. <br /> <br />ASI used the SCS TR-20 computer model for the hydrologic analysis. ASI <br />assumed that Coal Creek would spill to ditches that cross the plant site and <br />contribute to peak flows on site. Site surveys for this Master Plan indicated <br />that this would not occur, and therefore Coal Creek flows were not included <br />in this study. Spill flows were subtracted from ASI flows before comparison <br />to Master Plan flows. Because the total spill volumes are not provided by <br />ASI, runoff volume cannot be compared for design points that receive spill <br />flows. <br /> <br />This 1992 Master Plan, to be consistent with the previous UDFCD master plan for the Big <br />Dry Creek basin, uses similar future projections of basin development. UDFCD assumed <br />that future urban development would be modest. To follow up on this assumption, the 1991 <br />zoning maps of Jefferson County were examined as they relate to a new development, <br />Jefferson Center. Meetings were held with Arvada, Jefferson County, Westminster and the <br />UDFCD. A meeting was also held with Mr. Howard Lacy, President of the Jefferson <br />Center Metropolitan District. Mr. Lacy said that the Jefferson Center will most likely utilize <br />a complete stormwater detention system and would thereby have little effect on Rocky Flats' <br />drainage planning. <br /> <br /> <br />2. <br /> <br />The USACE (USACE, 1989) study used a different design storm precipitation <br />distribution than the present study. It used the HEC-l model for hydrologic <br />analysis. The study included only the scenario of the ponds being empty at <br />the outset of the storm. <br /> <br />As a result, a timeline was established for development projection to the year 2015 (25 <br />years) and it was concluded that the UDFCD future land use projections as used in their <br />Master Plan for Big Dry Creek (Greiner Engineering, 1986) would be applicable, at least <br />through the year 2015. In the event that these projects did not materialize, this Master Plan <br />could be modified. <br /> <br />3. <br /> <br />The UDFCD study was based on the CUHP model, but used future <br />development conditions for the plant area with a higher impermeable area <br />than used in this Master Plan. This tended to slightly increase the UDFCD <br />peak flow and runoff volume for Walnut Creek. <br /> <br />INFLOW TO STANDLEY LAKE/GREAT WESTERN <br /> <br />Standley Lake and Great Western Reservoir are located downstream and east of the Master <br />Plan study area. It should be noted that the previously approved UDFCD plans are not <br />affected. Table IV-ll presents a summary of flood magnitudes adopted for this Master <br />Plan. <br /> <br />ASI-ca1culated 100-year peak flows compare well (5 percent higher to 23 percent lower) with <br />those calculated for this report with two exceptions. First, runoff values at the Woman <br />Creek Diversion Dam and to Pond C-2 are lower in the ASI analysis. The Coal Creek Spill <br />flow was subtracted directly from the ASI value before comparison was made. No spill flow <br />hydrographs were presented by ASI; therefore it is not possible to verify that the peak spill <br />flow and peak basin flow are directly additive. Second, peak flows below the Core Area in <br />the Walnut Creek basin are higher (40 percent to 170 percent) than those calculated by AS!. <br />The Master Plan flows show a rapid routing of high Core Area runoff to correspond to <br />slower runoff peaks from the undeveloped areas farther upstream. <br />