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本文是笔者1981—1985年间对辽宁省水库生态学研究的部分结果,旨在初步了解辽宁省水库的某些生态学过程。 1 水库概况 辽宁省这13座水库的形态、自然环境相差悬殊(见表1)。降雨量在西部的大清沟和东方红水库较少,而东南部的铁甲和合隆水库较大。光照自西向东减弱。这些水库中浑江和大伙房属较深的山谷型水库,合隆、东方红、疙瘩楼和团结属平原型水库,其余介于二者之间。
This paper is a part of the author’s research on reservoir ecology in Liaoning Province from 1981 to 1985, and aims to understand some ecological processes of reservoirs in Liaoning Province. 1 Reservoir Overview Liaoning Province, the shape of the 13 reservoirs, the natural environment there is a big difference (see Table 1). Rainfall in the western Qing ditch and the Dongfanghong Reservoir less, while the southeast of the armor and Helong reservoir larger. Light weakened from west to east. These reservoirs in the Hunjiang River and Dachang room is deeper valley-type reservoirs, co-Long, Dongfanghong, pimples floor and unity is a plain reservoir, the rest between the two.