摘要
借用地下水动力学中贮水系数的概念，建立了一套利用贮水系数计算因过量开采地下水而产生的地面沉降量的方法，并利用唐山沿海地区地下水长期观测资料对这一地区因地下水位持续下降产生的地面沉降进行了估算。
Drawing support from the concept of storativity factor quoted from ground water dynamics,the authors advance a sort of method used to calculate ground subsidence caused by over exploiting ground water.By using long term observation data of ground water in Tangshan coastal areas the authors calculate the ground subsidence which is caused by continued dropping of ground water level in these areas. On theory,the authors research the mechanism of ground subsidence caused by over exploiting ground water.
出处
《现代地质》
CAS
CSCD
北大核心
1998年第3期419-424,共6页
Geoscience
