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时域激电单极~偶极测深数据转换为施伦贝格尔测深数据及其二维反演

雒志锋 穆建强

物探化探计算技术2012,Vol.34Issue(4):390-396,7.
物探化探计算技术2012,Vol.34Issue(4):390-396,7.DOI:10.3969/j.issn.1001-1749.2012.04.04

时域激电单极~偶极测深数据转换为施伦贝格尔测深数据及其二维反演

POLE - DIPOLE ARRAY SOUNDING DATA CHANGED INTO SCHLUMBERGER ARRAY SOUNDING DATA AND THEIR TWO-DIMENSION INVERSION FOR TIME DOMAIN INDUCED POLARIZATION METHOD

雒志锋 1穆建强1

作者信息

  • 1. 中国冶金地质总局地球物理勘查院正元地球物理有限公司,保定071051
  • 折叠

摘要

Abstract

This paper sketch and graphical show sounding principle and the electrodes array mode for pole-dipole array and symmetry four-pole (also Schlumberger) array. According "the equivalent resistivity method", and the resistivity internal relation for pole-dipole with Schlumberger, we give equation for Schlumberger array chargeabili-ty with pole-dipole array chargeability. And we can also change pole-dipole array acquire electro-parameter data into Schlumberger array data, at the same time, we make two-dimension inversion, plot imaging and comparison for the two sounding array resistivity and chargeability parameter. At last, To combine simple geological character, shows same geological effect with the two type sounding array.

关键词

测深/等效电阻率法/单极~偶极装置/施伦贝格尔测深装置/转换/视电阻率/视充电率/二维反演/地质效果

Key words

sounding/ equivalent resistivity method/ pole-dipole array/ Schlumberger array/ change into/ resistivity/ chargeability/ two-dimension inversion/ geological effect

分类

天文与地球科学

引用本文复制引用

雒志锋,穆建强..时域激电单极~偶极测深数据转换为施伦贝格尔测深数据及其二维反演[J].物探化探计算技术,2012,34(4):390-396,7.

物探化探计算技术

OACSCDCSTPCD

1001-1749

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