Electric and magnetic fields generated by electrokinetic processes in a conductive crust

E. Fedorov , V. Pilipenko , S. Uyeda
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引用次数: 31

Abstract

The results of different models of electrokinetic sources of ULF disturbances, mostly based on numerical calculations, can be reproduced with a much simpler analytical model of an elliptic-shaped inhomogeneity. The suggested model can be applied to the estimates of electromagnetic fields from elementary sources of different geometries. Moreover, this model enables one to estimate the screening effect of the back conductivity currents and the influence of the ground-atmosphere boundary. The estimates show that the expected magnitudes of seismo-electromagnetic signals in ULF band from an elementary electrokinetic source may reach the detection level only for rather favorable set of crustal parameters.

导电地壳中由电动过程产生的电场和磁场
不同的极低频扰动电动力源模型的结果,大多基于数值计算,可以用一个更简单的椭圆型不均匀性分析模型来再现。该模型可应用于不同几何形状的初等源的电磁场估计。此外,该模型还可以估计反向电导率电流的屏蔽效应和地面-大气边界的影响。估计表明,只有在相当有利的一组地壳参数条件下,来自初级电动力源的超低频地震电磁信号的预期震级才可能达到探测水平。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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