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<br />.l.lU <br /> <br />times as great above the reservoir as below the reservoir. and attri- <br /> <br />buted these differences to daily and seasonal streamflows. He showed <br /> <br />that daily vertical fluctuations of four feet commonly occur tmmediately <br /> <br />below the reservoir and stated that a maximum fluctuation of 1.850 cubic <br /> <br />feet per second may occur in less than one minute. The impact on inver- <br /> <br />tebrates is extremely detrimental especially when over 80 percent of the <br /> <br />120 <br />W <br />..J <br />Q. <br />~ <br />< <br />(f) <br />090 <br />a:= <br />< <br />o <br />z <br />~ <br />,60 <br />(f) <br />~ <br />(f) <br />Z <br />< <br />C) 30 <br />a:= <br />o <br /> <br />o <br />z <br /> <br />stream environment may be dry at low streamflows and severe ice cover <br /> <br />occurs in winter. <br /> <br />Catastrophic drift of chironomid larvae was recorded in the Green <br /> <br />River on 11 June 1965 (Pearson. 1967; figure 4). A sudden increase in <br /> <br />water level of nearly three feet caused an increase in the drift rate of <br /> <br />chironomid larvae. The drift decreased to nearly pre-flood rates after <br /> <br />about 3 hours. however. even though the water level remained high, indi- <br /> <br />cating that the organisms had been dislodged forcibly by the high water <br /> <br />velocity. <br /> <br />These examples demonstrate that changes in reservoir discharges to <br /> <br />a large stream such as the Green River can have a marked effect on bottom <br /> <br />macro invertebrates in the river. The fine review of streamflow patterns <br /> <br />below large dams on stream benthos by Ward (1976) prOVided the following <br /> <br />main points for consideration: (1) each dam must be considered individ- <br /> <br />ually in establishing flow criteria, (2) benthic species composition is <br /> <br />considerably modified by impoundments, (3) the flow regime may enhance <br /> <br />or reduce benthic organisms, and (4) the responses of benthic organisms <br /> <br />to smaller, sublethal effects related to streamflow are presently unknown. <br /> <br /> <br />o <br /> <br />0600 <br /> <br /> <br />--- <br />, <br />, <br />, ,.... <br />'" .... <br />,------ <br /> <br />~, <br />~ , <br />, <br />, <br />, <br />WATER ~ " <br />LEVEL , <br /> <br />CHIRONOMIDAE <br />LARVAE <br /> <br />\ <br /> <br />1200 <br /> <br />1800 <br /> <br />2400 <br /> <br />HOURS <br /> <br />Figure 4. <br /> <br />Increased Drift Rates of Chironomidae larvae after a Sudden <br />Increase in Flow, Little Hole, Green River, 11 June 1965 <br /> <br />3 <br />.... <br />W <br />W <br />~ <br /> <br />W <br />2(f) <br />< <br />W <br />a:= <br />U <br />Z <br />..J <br />W ~ <br />... <br />> - <br />.' <br />W .. <br />..J < <br />a:= c <br />. <br />W ... <br />.... ... <br />< .. <br />~ .. <br /> .. <br /> .. <br /> - <br />0 ~ <br /> , <br /> - <br /> .. <br /> <br />Source: W. D, Pearson and D, R, Franklin, "Some Factors Affecting Drift <br />Rates of Baetis and Simuliidae in a Large River," Ecology vol. 49, no. 1, 1968. <br />