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PROJ02027
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Last modified
11/19/2009 11:43:39 AM
Creation date
7/9/2007 3:24:29 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
FS0044FX
Contractor Name
Larimer County, Board of County Commissioners
Contract Type
Miscellaneous
Water District
0
Loan Projects - Doc Type
Feasibility Study
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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 />people per household, the population of the Local Basin is 4,037. In addition the Local Basin <br />has 424 businesses. <br /> <br />IV. Preliminary Engineering Investigation <br /> <br />Preliminary engineering for the project was conducted by URS Greiner Woodward Clyde <br />Engineering Company (URS). The study was published in a report entitled "Dry Creek Flood <br />Control Plan", April 2000. Larimer County engaged URS Greiner Woodward Clyde (URS) to <br />conduct a preliminary engineering investigation of alternatives for flood control on Dry Creek <br />pursuant to the terms of the IGA. Funding for this work was provided by Larimer County, the <br />City of Fort Collins, and a grant from the Colorado Water Conservation Board. The URS Plan <br />represents a conceptual solution to both flood control and local basin stormwater needs in urban <br />areas of northeast Fort Collins. The solution was determined from three alternative approaches <br />that were examined. One such alternative was to divert the entire Dry Creek flood flow from the <br />Willox Lane Dry Creek intersection south and west into the Cache La Poudre River as suggested <br />in the 1980 GAl Study. Other alternatives examined were detention storage of the entire flood <br />flow and detention storage of the partial flood flow and diversion of the residual flow. The <br />objective of the preliminary engineering study was to define improvements which would convey <br />residual upper basin flood flows, reduce the burden on irrigation canals and reservoirs, and <br />provide for disposition of Local Basin stormwater flows. The criteria for that solution was the <br />least cost solution which achieves these objectives. <br /> <br />Existing Basin Hydrology <br /> <br />Three previous hydrologic evaluations have been performed for the Dry Creek watershed by <br />Gingery Associates, Inc., (1977 and 1980) referred to herein as the GAl study, Resource <br />Consultants, Inc., 1992 referred to as RCI, and Lidstone and Anderson Inc. (1997), referred to as <br />LAI. The hydrologic information published in the effective Flood Insurance study (FIS) for the <br />City of Fort Collins (March 18, 1996) indicates a peak 100 year discharge at State Highway 287 <br />as 2,900 cfs, based on the GAl Study. A second analysis of the watershed hydrology was <br />conducted in October 1992 by RCI under contact to the Omaha District, US Army Corps of <br />engineers. The hydrologic information contained in that report indicates much higher 100 year <br />peak discharges (approximately 5,022 cfs upstream of the Larimer-Weld Canal). Larimer County <br />and the City of Fort Collins contracted an independent review of the RCI hydrology by LA! to <br />verify the information contained in the RCI Study. The results indicated similar peak 100 year <br />discharges (approximately 5,600 cfs at the Larimer-Weld Canal). This study therefore uses the <br />existing HEC-l model developed by RCI for the US Army Corps of Engineers to determine and <br />compare the effectiveness of alternative flood control measures. Flood control alternatives were <br />evaluated using a design storm of 3.46 inches from a balanced storm with a 6-hour duration. <br /> <br /> <br />Figure I shows the hydro graph of the 100 year runoff flow produced from this model at the <br />Larimer- Weld Canal. The 100 year runoff hydro graph produced from this model shows two <br />distinct peaks. The earlier peak of slightly in excess of 4,000 cfs is generated from watershed <br />areas downstream of the Douglas Reservoir. The later peak of slightly greater than 5,000 cfs. <br />is generated by flows originating upstream of Douglas Reservoir. <br /> <br />4 <br />
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