摘要
传统的渗流模型研究中,忽略了渗流场中水压力传递的时效性。本文针对潜水含水层井流问题,分析了井流场的特征。在前人研究的基础上,作者详尽地推导了上部入渗补给为常量情况下的降落漏斗半径和水压力传递速度与时间的关系式,并对某电厂水源地进行了计算。
In traditional study of fluid flow model,time dependent propagation is neligible.In this paper,the authors analyze character of well feild.On the basic of predecesser's study,the authors expound the reationship among depression cone radius and piezometric propagationg velocity are caculated in a electrical water source head.
出处
《地球科学与环境学报》
CAS
1997年第S1期57-60,78,共5页
Journal of Earth Sciences and Environment
关键词
降落漏斗
含水层水压力
传递速度
depression cone,piezometric head,propagating velocity