摘要
绥化2号井水位日变曲线上叠加有微小的凸起形态。本文从多方面论证了这一形态是浅层抽水引起的地下水位微动态,并对其特征及机理作了初步分析。
Microconvexes have been superposed on the daily variation curves of the water level in Suihua No. 2 well. This paper proves from all sides that this pattern of the groundwater level microdynamics is caused by pumping water from the shallow aquifer. A preliminary analysis about its characteristics and mechanism has been given.
出处
《地震》
CSCD
北大核心
1989年第3期58-62,共5页
Earthquake
