Electromagnetic coupling in frequency-domain induced polarization data: a method for removal

被引:35
|
作者
Routh, PS [1 ]
Oldenburg, DW [1 ]
机构
[1] Univ British Columbia, Dept Earth & Ocean Sci, UBC Geophys Invers Facil, Vancouver, BC V5Z 1M9, Canada
关键词
electromagnetic coupling; induced polarization; inversion; mineral exploration; noise;
D O I
10.1111/j.1365-246X.2001.00384.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Electromagnetic (EM) coupling is generally considered to be noise in induced polarization (IP) data and interpretation is difficult when its contribution is large compared to the IP signal. The effect is exacerbated by conductive environments and large-array survey geometries designed to explore deeper targets. In this paper we present a methodology to remove EM coupling from frequency-domain TP data. We first investigate the effect of EM coupling on the IP data and derive the necessary equations to represent the IP effect for both amplitude and phase responses of the signal. The separation of the inductive response from the total response in the low-frequency regime is derived using the electric field due to a horizontal electric dipole and it is assumed that at low frequencies the interaction of EM effects and IP effects is negligible. The total electric field is then expressed as a product of a scalar function, which is due to IP effects, and an electric field, which depends on the EM coupling response. It is this representation that enables us to obtain the IP response from EM-coupling-contaminated data. To compute the EM coupling response we recognize that conductivity information is necessary. We illustrate this with a synthetic example. The removal method developed in this work for the phase and the pur cent frequency effect (PFE) data are applicable to 1-D, 2-D and 3-D structures. The practical utility of the method is illustrated on a 2-D field example that is typical of mineral exploration problems.
引用
收藏
页码:59 / 76
页数:18
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