断层裂隙水的天然电场动态响应特征  

The natural electric field dynamic characters of fracture water in fault

作　　者：王连元[1] 

机构地区：[1]黑龙江科技学院建筑工程学院,黑龙江哈尔滨150027

出　　处：《煤田地质与勘探》2012年第1期76-78,84,共4页Coal Geology & Exploration

摘　　要：流动于断层裂隙中的地下水径流相对较集中,可视为一种运动的导体。在天然电场这一微弱的物理场中可形成明显的动态响应,即在时间和空间上的非稳定运动产生复杂、时变的感应电磁场。试验证明,这种动态响应不仅与地下水埋深、水力坡度有关,而且与观测频率也存在着较密切的关系。The radial flow of fracture water in faults is comparatively concentrated and can be regarded as a kinetic conductor.The obvious dynamic responses are formed in faint natural electromagnetic field by the flowing groundwater.Its unstable flowing will bring complicated and time-dependent electromagnetic induction on time and space.These dynamic responses are not only related with its depth and hydraulic gradient,but also closely re-lated with observation frequency.

关 键 词：断层裂隙水 天然电场 动态响应 电场效应 

分 类 号：P631[天文地球—地质矿产勘探]