1·The concentrated leakage passage in fissured rock is studied with dummy heat source method.
利用虚拟热源法研究坝基裂隙岩体中存在的集中渗漏通道。
2·Firstly, the basic rule of seepage in fissured rock mass and the mechanism of the effect are studied.
首先分析了裂隙岩体渗流运动的基本规律，研究了应力对渗流作用影响的机理。
3·The fissured rock seepage flow field of Xinanjiang river right dam is studied by using the isotope tracer method.
应用同位素示踪方法对新安江右坝的裂隙岩体渗流场进行了研究。
4·In this paper, the basic characteristics of the seepage of contact fissured rock mass under the stress action are studied.
对在应力作用下接触型岩体裂隙的渗流基本规律作了研究。
5·Seepage flow in fissured rock masses is strongly anisotropic, due to main water flowing only through in fissure and bedding.
由于水只能沿着岩体的裂隙及层理等流动，致使裂隙岩体的渗流具有强烈的各向异性的特征。
6·The obtained results are shown that the anchor bolts supports in the fissured rock mass is good to raise the safety of the whole structure of grottoes.
结果表明，锚杆的加固作用是明显的，在有裂隙的部位打入锚杆对石窟整体结构的安全性是有益处的。
7·The results show that the probability distribution characteristic of the vertical permeability coefficient in fissured rock zone is much close to the log-normal distribution.
结果表明，同正态分布和均匀分布相比，裂隙岩体地区的垂向渗透系数更接近对数正态分布。
8·In combination with fissured rock strike, dip Angle and distribution seepage flow in fissured rocks is determined by use of single well tracer method for the area under study.
将单孔示踪方法应用于群孔之中，结合裂隙岩体的走向、倾角、裂隙分布等参数，确定出研究区域的裂隙岩体中的渗流场分布。