Effects of Elevated Stream Temperatures below a Shallow Reservoir on a Cold Water Macroinvertebrate Fauna
Effects of Elevated Stream Temperatures below a Shallow Reservoir on a Cold Water Macroinvertebrate Fauna
复制标题
浅水库以下溪流温度升高对冷水大型无脊椎动物群的影响
DOI:
10.1007/978-1-4684-8613-1_15
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发表时间:
1979
期刊:
影响因子:
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通讯作者:
J. Fraley
中科院分区:
文献类型:
--
作者:
J. Fraley
The Madison River is one of Montana's finest cold-water streams, supporting a highly productive fishery that yields nearly 100,000 trout to anglers each year (Vincent, 1969). It comprises 116 km of the 727 km of blue ribbon trout water in the state.Shortly after 1900 the Madison River was impounded to form Ennis Reservoir. Water from the reservoir is used to produce power at the Madison Power Plant located immediately below Ennis Dam. The reservoir is wide and shallow and acts as a heat trap, raising summer temperatures of downstream waters (Heaton, 1961; Vincent, 1977). These increased summer water temperatures appear to be threatening the blue ribbon trout fishery downstream from the reservoir. Recent studies (Vincent, 1977) have shown that rainbow and brown trout greater than 28 cm in length had slower growth rates in the river downstream from the reservoir (lower river) than upstream (upper river). Conversely, trout less than 28 cm grew faster downstream from the reservoir. The reasons for these differences in growth rates were not clearly understood, but the effects of high mean summer water temperatures (approaching 19 C) on trout metabolism or food supply have been suggested as possible causes.