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METHOD OF SOIL RESISTIVITY TIME VARIATIONS MEASUREMENT
METHOD OF SOIL RESISTIVITY TIME VARIATIONS MEASUREMENT
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机译:土壤电阻率时间变化的测量方法
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摘要
FIELD: physics.;SUBSTANCE: current is cutoff to soil through two point sources. The first source is placed close by vertical interface, and the second is taken to infinity. Position of one equipotential line of electric field is detected. Measuring electrodes is mounted by tangent to equipotential line symmetrically to tangency point of ray lined from auxiliary point presenting mirror reflection of point source relative to interface with specified equipotential. Besides, measuring electrodes can be placed by line, perpendicular to interface symmetrically to power supply provided close by interface. Near to interface there is compensatory point source with current value fixed by parity where I0, Ik are currents from the first and compensatory sources, ΔΨ1MN is differential of the space function that determinates position of measuring electrodes relative to the first source, ΔΨ2MN is differential of space function that determinates position of measuring electrodes relative to compensatory source. Measuring electrodes voltage indicates time variations of resistivity.;EFFECT: simplified positioning of electrical survey unit and improved measurement accuracy.;1 dwg
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机译:领域:物理学。;实体:电流通过两个点源截断到土壤。第一个光源通过垂直界面放置得很近,而第二个光源则被置于无限远。检测到一条等电位电场线的位置。测量电极通过与等势线相切的切线安装,该等势线与辅助点所成的射线的切点对称,该辅助点呈现点源相对于具有指定等势面的界面的镜面反射。此外,测量电极可以垂直于界面垂直于界面对称地放置,相对于由界面附近提供的电源线。在接口附近,有一个补偿点源,其当前值由奇偶校验确定。其中I 0 Sub>,I k Sub>是来自第一个补偿源的电流,ΔΨ 1MN Sub>是确定位置的空间函数的微分测量电极相对于第一源的测量值,ΔΨ 2MN Sub>是空间函数的微分,其确定测量电极相对于补偿源的位置。测量电极电压指示电阻率的时间变化。效果:简化了电气测量单元的位置并提高了测量精度。1dwg
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