摘要
破碎岩体中的渗流严格意义上是非稳态的。本文通过定义非稳态因子 ,试验研究了不同岩性不同粒径破碎岩石的非稳态渗流特性规律。另外 。
etc.Strictly speaking, the seepage in over-broken rocks is non-steady. The authors research the characteristic laws of non-steady seepage of over-broken rocks in diverse grain sizes or with different material properties by putting forward the concept of non-steady factor. In addition, the applications of the non-steady factor on analysis of seepage are discussed in this paper, too.
出处
《矿山压力与顶板管理》
北大核心
2004年第1期109-111,共3页
Ground Pressure and Strata Control
