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during our study. <br />River backwater: River backwaters are submerged during high flows and do not <br />emerge as distinct entities until the river drops. For this reason, the river backwater was <br />not sampled during peak flow (June). The river backwater we sampled was located just <br />upstream of the river channel site described above and was approximately 10 m wide x <br />50 m long and 1.3 m deep. The substrate consisted mostly of loose silt and detritus with <br />virtually no sand. Silt and det-itus were constantly being deposited during the study <br />period. <br />Seasonally inundated Wetland: This site is commonly called "Old Charlie's Wash". <br />It is a shallow floodplain pond managed by the United States Fish and Wildlife Service <br />for waterfowl and is located approximately ?km south of the U.S.F.W.S hatchery. As <br />the river level rises in the spring, water flows into "Old Charlies Wash" and, at peak <br />flow, retaining structures are put in place creating a 43 hectare lake and preventing the <br />impounded water from receding as rapidly as the river itself. By early fall, the water <br />in "Old Charlie's Wash" is nearly depleted by seepage and evaporation. The substrate <br />consisted of firm silt, detritus, and sand. <br />5