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Electrokinetics in Earth Sciences

机译：地球科学中的电动学

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Electrokinetics is used in earth sciences to provide insights concerning near-surface earth structures (from a few hundred meters up to several thousand meters depth) that host interstitial fluids (water, ice, oil, and gas). Electrokinetic phenomena are induced by the relative motion between the fluid and the rock matrix and, therefore, can provide information about the fluids within the earth. Self-potentials have been measured in hydrology, in active volcanic areas, and in polluted environments. Various methods based on electrokinetics, including self-potentials and seismoelectromagnetic conversion, have been applied to the management of hydraulic and hydrocarbon reservoirs, the resource prospecting in glaciated regions, the exploration for and monitoring of geothermal reservoirs, the characterization of fractured reservoirs, and so forth.
机译：动力学在地球科学中用于提供有关容纳间隙流体（水，冰，石油和天然气）的近地表地球结构（从几百米到几千米深度）的见识。电动现象是由流体与岩石基质之间的相对运动引起的，因此可以提供有关地球内流体的信息。在水文学，活动火山区和污染环境中已测量了自势。基于动能的各种方法，包括自电势和地震电磁转换，已被应用到水力和油气藏的管理，冰川地区的资源勘探，地热油藏的勘探和监测，裂缝性油藏的表征等方面。向前。

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