摘要
本文系统研究了降雨量、降雨方式等对尚志井水位年、季、日动态的影响,指出了降雨是该井水位动态的主要影响因素,剖析了这种影响的特征。此外,还提出了东北地区深井水位早春回升的“冻层底部消融”补给机制的新观点。
The influence of rainfall and its form on yearly, seasonal and day-to-day dynamics of
water level in Shangzhi well has beed systematicall studied in this paper. The paper point out
that rainfall is main, factor to have influence over dynamics of water level in the
well. Futhermore, a new view point with regard to supply mechanism because melting of
frozen layer bottom leads to a rise in water level of deep well of Northeast China region in
early spring has been also presented.
出处
《防灾减灾学报》
1992年第4期79-92,共14页
Journal of Disaster Prevention And Reduction
基金
地震科学联合基金会资助的90420课题研究成果
关键词
尚志井
降雨
水位动态
Shang zhi well
Rainfall
Dynamic water level
