摘要
本文通过对基岩水运动的平均流速分析，提出了不同出流条件突水的涌水量理论计算方法，也为现场突然涌水量计算提供了新的理论依据。
According to the study of average velocity of confined and unconfined fissure flow of different rush conditions, this paper proposes a new approach for theoretical computation about discharge of rush on corresponding conditions. It can provide a new theoretical basis of computing discharge of rush for the spot.
出处
《水文地质工程地质》
CAS
CSCD
1997年第1期36-38,48,共4页
Hydrogeology & Engineering Geology
基金
煤炭部科学基金!91-356
