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• <br />MATERIALS AND METHODS <br />Permanent staff gages were installed at the four major stations.: <br />for water level observations. Records from recording water level <br />gages maintained by the U. S. Geological Survey at Greendale (0.5 MBD) <br />and near Jensen (93.4 MBD) were also utilized. Water temperature was <br />measured with a 12-inch mercury-glass thermometer at all stations and <br />with 30-day Ryan recording thermometers at Echo Park and Island Park. <br />Additional temperature records at Greendale (0.5 MBD), Allen Ranch <br />(26.0 MBD), Jensen (93.4 MBD), and Ouray (166.0 MBD) were obtained <br />from the U. S. Geological Survey and the Utah Department of Fish and <br />Game. Turbidities were determined with a Jackson candle turbidimeter. <br />Dissolved oxygen content of the water was determined by the Thierault <br />modification of the Winkler method. Total and phenolphthalein alkalini- <br />ties were determined by procedures outlined in Standard Methods (1960). <br />Hydrogen-ion concentration was determined with a Wallace and Tiernan <br />comparator. A Gurley pygmy current meter was used to measure water <br />velocities 1-inch above the bottom at each sample site. The physical <br />nature of the substrate at each sample site was recorded according to <br />a classification scheme similar to one suggested by Lagler (1956). All <br />above environmental observations accompanied each quantitative sample <br />taken a£ invertebrates. <br />Benthic invertebrates on hard substrates were sampled with a wire- <br />mesh device similar to those described by Hess (1941) and Waters and <br />• Knapp (1961). Ninety-five and 87 samples were collected in 1964 and 1965