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<br />.. <br /> <br />60 <br /> <br />P. B. HOLDEN <br /> <br />produce warm summer temperatures; deep intakes generally produce <br />cold summer temperatures. Summer temperatures have generally been <br />lower than natural in most instances where native fishes have been <br />adversely affected. Winter temperatures may be elevated below <br />deep-release dams. ; <br /> <br />Most obligate riverine fishes are adapted to a certain daily, <br />seasonal, and yearly temperature regime, as are most fishes in gen- <br />eral (Allen, 1969; Hubbs, 1972). Therefore, changes in the preferred <br />thermal regime will affect them, and the greater the change, the <br />greater the impact or effect. Species that are relatively specialized <br />in terms of temperature requirements may disappear altogether because <br />they are unable to tolerate the "new" regime (Pfitzer, 1963; Spence <br />and Hynes, 1971; Trautman and Gartman, 1974; Edwards, 1978). They <br />are often found further downstream, where preferred temperatures are <br />still available. Other species that are preadapted to the regulated <br />temperatures often become more abundant. In many situations, the <br />altered thermal regime is sufficient for adults, but temperatures <br />are not adequate for reproduction (Pfitzer, 1963; Hubbs, 1972; <br />Zakharyan, 1972). Therefore, the tailwater population is either <br />replenished from downstream recruitment or, in the case of species <br />with short life spans and little movement capabilities, the species <br />disappear immediately below the dam. <br /> <br />The regulation of rivers also tends to alter the turbidity and <br />general water chemistry in the tailwaters. Turbidity is generally <br />lowered and, therefore, could affect fishes that require turbidity. <br />No information in the literature indicates that this has actually <br />been the cause of a species or population decline. Smith (1976) <br />indicated that increased turbidity below dams in the Trinity River, <br />California, caused siltation of salmonid spawning areas. <br /> <br />Water chemistry changes can also be great. Generally, rivers <br />below dams reflect the Water chemistry from the intake level of the <br />upstream reservoir. Therefore, the types of chemical changes vary <br />between dams, and seasonally at anyone dam, as the reservoir <br />stratifies and overturns. Again, there is little information to <br />show that these kinds of chemical changes have influenced fishes. <br /> <br />Of great concern in most large dam situations is gas super- <br />saturation in tailwaters. The Waters become supersaturated when <br />spilled over high dams, trapping air and plunging it to depths <br />where high pressures enhance solubility. This has been a major <br />problem in the Pacific Northwest, where gas-bubble disease has been <br />one of the major mortality factors on young salmon and trout (Ebel, <br />1969; Collins, 1976; Raymond, 1976; Robinson, 1978). It has been <br />solved in some cases by the use of deflectors in the spillways <br />(Collins, 1976). <br /> <br />. <br />