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<br />to those used in earlier studies (Archer et al. 1980; Miller et al. 1982) prior to completion of <br /> <br />Taylor Draw Dam (1985), and the fourth stratum ended at the dam. <br /> <br /> <br />All strata were further subdivided into smaller sampling units called habitat clusters <br /> <br /> <br />(Figures 2 and 3). The length of each habitat cluster contained at least two representative pool- <br /> <br />run-riflle habitat sequences. Leopold et al. (1964) and Bovee (1982) found that a simple pool. <br /> <br />run-riffle habitat sequence repeated itself in distance equivalent to five times the mean channel <br /> <br />width. The habitat cluster length in the White River was equal to 10 times the mean channel width <br /> <br /> <br />to capture two habitat sequences. The mean river channel width was calculated from <br /> <br />measurements taken from aerial photographs. <br /> <br /> <br />Each habitat cluster was numbered and located by RM on a topographic map. A random <br /> <br /> <br />numbers table was used to select 25 habitat clusters in each stratum to sample mesohabitat data <br /> <br /> <br />during each flow and year (25 clusters * 4 strata * 3 flows * 2 years = 600 clusters). One habitat <br /> <br /> <br />cluster was strategically placed at the Watson, Utah, u.s. Geological Survey (USGS) gage, just <br /> <br /> <br />downstream from Ignacio Bridge on Highway 45, to aid in making comparison with the historical <br /> <br /> <br />USGS gage data. <br /> <br /> <br />Two habitat cross sections were randomly placed perpendicular to the flow across the <br /> <br /> <br />river in each habitat cluster to collect mesohabitat (pool, riffle, eddy, run) and microhabitat <br /> <br /> <br />(depth, velocity) data. Figures 2 and 3 describe habitat clusters in each stratum and how cross <br /> <br /> <br />sections were located. <br /> <br /> <br />Data Collection <br /> <br />Field crews conducted a reconnaissance float trip down the White River in the early <br /> <br />4 <br />