Abstract
Temperature and oxygen regimes were monitored weekly in a four-year old reservoir and downstream for ten weeks during the summer (May 15 to July 30, 1979), and monthly in the fall and winter. During the summer discharge levels were changed from top to bottom in the eighth week, back to top in the ninth, all at 0.71 m3/s (= 25 cfs), and returned to the bottom in the tenth, but at 1.14 m3/s (= 40 cfs).
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