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关于非均匀介质中电导率按深度变化时的势及其视电阻率函数
引用本文:邓本让.关于非均匀介质中电导率按深度变化时的势及其视电阻率函数[J].地球物理学报,1981,24(1):77-85.
作者姓名:邓本让
作者单位:长春地质学院
摘    要:本文共分六部分内容。在前言中,简述了电测深方面有关研究的情况,尤其叙述了E.S.Sampaio(1976)的结果。 因本文采用的方法不同,从而求解了适合要求的微分方程定解问题,获得了电导率以 (其中α、σ0、σ1均为正实数,β为实数)按深度变化时势的分布。 其次,当β=0时,对电导率σ=(σ01z)α按深度变化时势的分布,应用Bessel函数的积分表达时,明显地改进和推广了E.S.Sampaio(1976)结果中的重要部分。 最后,结合实际作出了第一类、第二类标准化视电阻率函数。这种视电阻率函数,推广了Wenner和Schlumberger分别作出的视电阻率函数的有关部分,对电阻率法和激发极化法,都有其理论价值和实际意义。

关 键 词:视电阻率  非均匀介质  深度变化  电导率  待定函数  三极排列  半空间  异常场  对应部分  类标准  
收稿时间:1979-06-05

ON THE POTENTIAL AND THE APPARENT RESISTIVITY FUNCTION IN AN INHOMOGENEOUS MEDIUM WHOSE CONDUCTIVITY VARYING WITH DEPTH
DENG BEN-BANG.ON THE POTENTIAL AND THE APPARENT RESISTIVITY FUNCTION IN AN INHOMOGENEOUS MEDIUM WHOSE CONDUCTIVITY VARYING WITH DEPTH[J].Chinese Journal of Geophysics,1981,24(1):77-85.
Authors:DENG BEN-BANG
Institution:Changchun Geological Institute
Abstract:We started out by finding the exact solution of the differential equation of the problem. The potential distribution is obtained for the medium with conductivity varying with depth as: σ = (σ0 + σ1z)αeβz (where α, σ0, σ1 are positive real unmbers, β is a real number). Then, the potential distribution is obtained when the conductivity varies with depth according to σ = (σ0 + σ1z)α, (α > 0) as β = 0, which we apply the integration of Bessel function to express it obviously the important part in the result3] of E. S. Sampaio are improved and expanded. Finally, we formed type one and type two normalized apparent resistivity functions, which include the apparent resistivity function of Wenner and Schlumberger as a special case.
Keywords:
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