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<br />Staff, in conjunction with the USGS and other affected parties, have identified the following components of the project in <br />order to meet the goal; <br />Project Required <br />Component Description USGS Matching <br /> Total Cost Fundin Funds <br />Reconnaissance A reconnaissance of the study reach will be made f1uring late <br /> Jannary or early February, 2003, The cUlTent low-flow conditions <br /> resulting from the drought of 200 1-02 combined with plans to <br /> suspend diversion by the Redlands Canal during November 2002 <br /> through February 2003 provide an unprecedented opportunity for <br /> the reconnaissance effort to evaluate the geologic"hydrologic, and <br /> physical characteristics of the study reach. The location of geologic <br /> features, such as faults, or man-made features, suclt as gravel pits, $ 9,920 $ 2,950 $ 6,970 <br /> that could affect streamflow transit loss in the study reach will be <br /> noted, <br />Measurements A series of3-5 discharge measurement sets will be made in the <br />I study reach, Each set will consist of 5-6 discharge, measurements <br /> made over a 2-day period at each ofthese sites: (al At or near <br /> station 09152500, (b) at or near the two downstream stations (at the <br /> Redlands Canal only whenever streamflow is being diverted), and <br /> (c) at a number of intermediate locations to be determined during <br /> the course of the study, <br /> The first set of discharge measurements will be made during <br /> February, 2003, before diversion by Redlands Catjal commences <br /> and for a discharge range of 500-1,500 fi3/s in the, Gunnison River, <br /> Measurements also will be made at 4-6 intermediate locations <br /> based on reconnaissance results, These locations, for example, <br /> could be upstream and downstream of a particular feature that <br /> might have an effect on streamflow transit loss. <br /> The discharge measurements will be used in conjunction with the <br /> stage recorders and the stage-discharge relations to derive the total <br /> discharge volume at the upstream and downstreanj ends of the <br /> study reach during the 2-day period. Based on differences in the <br /> volume for the upstream station and the combined; volume for the <br /> two downstream stations, the streamflow transit losses or gains will <br /> be computed. The measurements at the intermediate locations will <br /> help show if the streamflow transit losses are uniformly distributed <br /> throughout the study reach or ifthe losses are justin a certain <br /> location or locations. <br /> Four additional sets of measurements will be made during April- <br /> September, 2003, at the three stations and at a sub~et of the <br /> intermediate locations used in the first measurement set. The subset <br /> locations will be selected on the basis of results from the first $ 8,980 $ 2,670 $ 6,310 <br /> dischar e measurement set. <br />Mass Balance The detailed mass-balance analysis of the historical discharge <br />Analysis records at the upstream and two downstream stations will be made <br /> during March-April, 2003, using records for the last 5-10 years and <br /> evaluating discharge measurements, control condipons, stage- <br /> discharge relations, and other factors at the three stations. The <br /> discharge records will be analyzed on the basis of:time of year, <br /> hydrograph position, and discharge range. $ 23,110 $ 6,730 $ 16,380 <br /> Results of the mass-balance analysis and the first $et of <br /> measurements will be com ared. <br />Measurements A second set of discharge measurements will be clade at medium <br />2 flow (1,500-3,000 fi3/s) at the beginning of high-elevation $ 7,700 $ 2,300 $ 5,400 <br /> snowmelt. <br /> <br /> <br />Flood Protection. Water Project Planning and Financing. Stream and Lake Protection <br />Water Supply Protection. cOnservation Planning <br />