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<br />, .. <br /> <br />. <br /> <br />APPENDIX f <br /> <br />-''': <br /> <br />IMPACTS OF THE 3-5 NOVEMBER 1997 31,000 cfs TEST FLOW <br /> <br />Introduction <br /> <br />The Bureau of Reclamation and the Grand Canyon Monitoring and Research Center conducted ,a test of a <br />"Habitat Maintenance" style flow from Glen Canyon Dam on 3-5 November 1997. The flow peak reached <br />approximately 30,600 cfs for this 2-day test. This memo outlines the impacts of that flow event on resources <br />through Grand Canyon. <br /> <br />Phvsical Resource ImDacts <br /> <br />GCMRC coordinated pre- and post-event videography of the river corridor, and those images are being <br />examined for backwater habitat changes. <br /> <br />Using the methods of Pam ell et al. (1996), detailed topographic surveys of35 sand bar monitoring sites were <br />conducted immediately following the November 1997 test flow by members of the Northern Arizona University <br />Depamnent of Geology sand bar studies office. Information gathered from these surveys is compared to <br />previous surveys conducted in August 1997 in order to quantify sand bar change. Based on this preliminary <br />date, the November test flow benefitted the sediment resources by depositing sediment at higher elevations. The <br />higher elevation areas of sand bars contain critical riparian habitats that Ar.. of particular interest to management <br />.agencies. following the 199645,000 ft'/s test flow, erosion has steadily decreased the volume of sediment <br />.:-) contained in the upper elevations of sand bars. Preliminary results show that the November 1997 test flow <br />'." slightly increased the volume of sand bars (above the 20,000 ft'/s stage elevation), calculated as a percentage of <br />the pre-1996 test flow, from 87% to 91 %. High flows above powerplant capacity are the only means by which <br />the volume of the upper levels of sand bars can be maintained. <br /> <br />The U.S. Geological Survey (G. Fisk, D. Topping, D. Rubin and S. Wiele) monitored mainstream streamflow <br />and suspended sediment at the Lee Ferry, Above Little Colorado River, Grand Canyon and Diamond Creek <br />gauges one/day before, during and after the flow event. Bedload sampling was conducted int he mainstream and <br />in eddies at selected sites following the high flow. Bar sedimentology, grain size, deposit thickness was <br />conducted with the NAU effon immediately following the high flow. <br /> <br />Biolo~ical Resource Impacts <br /> <br />On November 6,1997, the Arizona Game and fish Depanment (AFFD) surveyed cobble bars in the Lee Ferry <br />reach to access rainbow trout stranding post downramp. AGfD evaluated stranding by dividing each cobble bar <br />examined into quadrants and obtaining a total count of stranded fish by examining total area of the bars. AGFD <br />also noted stranding ofmacroinvenebrates. Cobble bars selected for evaluation were representative of this <br />habitat type in the Lee Ferry reach and were in areas which receive preferential use by fishing guides and trout <br />(6Omm) was observed to have been stranded and low concentrations of Gammarus were observed stranded in a <br />few shallow pools, no other stranded macroinvenebrates noted. At RM-8, two live rainbow trout (9Omm and <br />.400-500mm) were observed stranded in a large pool, Gammarus (~I,OOO) of diverse size range were observed <br />tranded in one small pool, and several thousand snails (Physidae) were observed stranded on two small sand <br />~ habitats associated with sedges nearshore. At RM-2.5, one dead adult flanneimouth sucker (catostomus <br />latipinnis) was observed in approximately 3 ft. Of water just inside mouth of backwater. This was judged not to <br />be a stranding-related monality. <br />