期刊文献+

Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China 被引量:15

Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
下载PDF
导出
摘要 The research about subsurface characteristics by using transient electromagnetic method(TEM) and high density resistivity method(HDRM) were already conducted in Ordos. The objective of this research is to detect coalmine goaf areas based on rock resistivity. The data processing using wavelet transform, three point smoothing, RES2 DINV and Maxwell processing software to obtain 2D resistivity structure. The results showed that the layers with maximum resistivity values(30e33 U m on Line 1, 30e31 U m on Line 2, 32e40 U m on Line3) are founded at station 1e7, and 14e20 on Line 1,13e18 on Line 2, and 8e13 and 16e20 on Line 3 which is predicted as goaf layer, and the minimum resistivity values(20e26 U m of TEM, 45e75 U m of HDRM) at the other layers. This resistivity difference was caused by the geology and characteristics of the study area which is located close by the cleugh with rich coal, so the goaf area distinguishable with aquifer layer and coal seam. The results were also significant accidents and serious destruction of ecological environment. The research about subsurface characteristics by using transient electromagnetic method(TEM) and high density resistivity method(HDRM) were already conducted in Ordos. The objective of this research is to detect coalmine goaf areas based on rock resistivity. The data processing using wavelet transform, three point smoothing, RES2 DINV and Maxwell processing software to obtain 2D resistivity structure. The results showed that the layers with maximum resistivity values(30e33 U m on Line 1, 30e31 U m on Line 2, 32e40 U m on Line3) are founded at station 1e7, and 14e20 on Line 1,13e18 on Line 2, and 8e13 and 16e20 on Line 3 which is predicted as goaf layer, and the minimum resistivity values(20e26 U m of TEM, 45e75 U m of HDRM) at the other layers. This resistivity difference was caused by the geology and characteristics of the study area which is located close by the cleugh with rich coal, so the goaf area distinguishable with aquifer layer and coal seam. The results were also significant accidents and serious destruction of ecological environment.
出处 《Geodesy and Geodynamics》 2016年第5期340-347,共8页 大地测量与地球动力学(英文版)
基金 supported by the Institute of Seismology Foundation, China Earthquake Administration (201326126)
关键词 Transient electromagnetic method High density resistivity method Coalmine goaf areas GEOTECHNICAL ELECTRICAL Transient electromagnetic method High density resistivity method Coalmine goaf areas Geotechnical Electrical
  • 相关文献

参考文献4

二级参考文献25

  • 1陈泉霖,陈新奇.高密度电法勘察岩土工程实例[J].中国煤田地质,2004,16(6):52-54. 被引量:14
  • 2静恩杰,李志聃.瞬变电磁法基本原理[J].中国煤田地质,1995,7(2):83-87. 被引量:49
  • 3花育才,项首龙,夏双力,孟红星.电法勘探在煤矿防治水中的应用[J].中国煤田地质,2006,18(4):66-68. 被引量:16
  • 4朴华荣编著.电磁测深法原理[M].北京:地质出版社,1990.
  • 5Spies B R.Depth of investigation in electromagnetic sounding methods[J].Geophysics,1989,54(7):872-888.
  • 6Das U C.Multiseparation multisystem electromagnetic depth sounding--An extension for unification[J].Geophysics,1987,62:56-62.
  • 7Eaton P A,Hohmann G W.A rapid inversion technique for transient electromagnetic soundings[J].Physics of the Earth and Planetary Interiors,1989,53:384-404.
  • 8Kaufman A A.Harmonic and transient fields on the surface of a two-layer medium[J].Geophysics,1979,44:1208-1217.
  • 9Macnae J.Imaging quasi-layered conductive structures by simple processing of transient electromagnetic data[J].Geophysics,1987,52(4):545-554.
  • 10Nekut A G.Direct inversion of time-domain electromagnetic data[J].Geophysics,1987,52(10):1431-1435.

共引文献356

同被引文献234

引证文献15

二级引证文献46

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部