摘要
应用平面热源法分析江水位升降期北江石角段堤基内地下水实测温度场 ,以判断基岩中断层的位置、产状和渗透性 ,并认为断层为强透水通道 。
The temperature field of groundwater during raising and falling periods of water level in the dike of Shijiao reach of Beijiang River were analyzed by using a plane heat source method. The location, state and permeability of a fault in the base rock can be judged from the analyses, and it can be seen that the fault is a strong permeable access that causes leakage in the dike base in flood periods .
出处
《水利水运工程学报》
CSCD
北大核心
2002年第3期63-65,共3页
Hydro-Science and Engineering
关键词
平面热源法
温度场
断层
渗漏
北江大堤
plane heat source method
temperature field
fault
leakage
Beijiang dike
