The results indicate that the observed seepage behavior in Jinshuitan dam is normal.
分析表明，紧水滩大坝实测渗流性态正常。
The calculated values of pore pressure taking nonlinear seepage behavior into account are closer to the measured ones.
考虑渗透非线性情况下得到的孔隙压力计算值与实测值更接近。
Therefore, it is thought that the seepage behavior of rock masses surrounding the underground chamber can be reflected really by carrying out HPPT.
因而认为，进行高压渗透试验，可以更为真实地反映深埋地下洞室围岩体的渗流状态。
应用推荐