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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 />I 7 <br /> <br />1993 AND 1994 FIELD STUDIES <br />Side channel/backwater habitats were the focus of the field study due to <br />their importance to both the adult and larval stages of the Colorado squawfish <br />and razorback sucker. Backwater morphology is partly dependent upon the <br />flow regime which controls the scour and fill of sediment. The high flows of <br />spring generally cause the backwater to become a side channel and fine <br />sediment that has accumulated on the bed is scoured. Some researchers <br />theorize that river regulation has decreased flows and caused a net filling of <br />these areas with sediment (Osmundson and Kaeding, 1991; Graf, 1978). The <br />relatively high (1993) and low (1994) peak discharges of the two years allowed <br />us to document the effects of flow magnitude on backwater morphology. <br />Methods <br />Three side channel/backwater sites were chosen and 25 cross-sections of <br />bed topography were surveyed before, during, and after the peak flows of 1993 <br />and 1994. All cross-sections were permanently marked with rebar or metal <br />fence posts. Standard surveying techniques were used to measure cross- <br />sections in areas of shallow flow. In deeper areas such as the main channel, <br />cross-sections were surveyed from a boat outfitted with depth sonar (Van <br />Steeter and Pitlick, 1994). Characteristics of the three sites are summarized in <br />Table 4. <br />