| 断层裂隙水的天然电场动态响应特征 |
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| 引用本文： | 王连元.断层裂隙水的天然电场动态响应特征[J].煤田地质与勘探,2012(1):76-78,84. |
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| 作者姓名： | 王连元 |
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| 作者单位： | 黑龙江科技学院建筑工程学院 |
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| 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。
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| 关 键 词： | 断层裂隙水 天然电场 动态响应 电场效应 |
The natural electric field dynamic characters of fracture water in fault |
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| WANG Lianyuan.The natural electric field dynamic characters of fracture water in fault[J].Coal Geology & Exploration,2012(1):76-78,84. |
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| Authors: | WANG Lianyuan |
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| Institution: | WANG Lianyuan(College of Architecture and Civil Engineering,Heilongjiang University of Science and Technology,Harbin 150027,China) |
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| Abstract: | 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. |
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| Keywords: | fracture water of fault natural electric field dynamic response electric field effects |
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