摘要
鄱阳湖是典型的吞吐型、季节性自流过水湖泊,水位变化主要受五河、湖口进出水量的制约,有明显的稳定退水期。德定退水期内,湖区地下水的进出量远小于“五河”入水量和湖口出水量,据此建立湖水位与蓄水量、净输出流量与水位、蓄水量之间的关系,并将它们结合,推得鄱阳湖稳定退水公式,经1952～1986年退水资料的验证,其结果令人满意。
The characteristics of the water flow in Poyang Lake are analysed. The relationships between the water level, the storage volume and the net flow-out rate during the stable water-receding period are established and a formula describing the water-receding is derived. The formula is tested with the data of 1952—1986 and the result is satisfactory.
出处
《海洋湖沼通报》
CSCD
北大核心
1989年第4期30-34,共5页
Transactions of Oceanology and Limnology
