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

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 trans...

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Main Authors: Guiju Wu, Guangliang Yang, Hongbo Tan
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2016-09-01
Series:Geodesy and Geodynamics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984716300684
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spelling doaj-93308589b9de41e6839cc64fcc9e600c2021-04-02T11:00:49ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472016-09-017534034710.1016/j.geog.2016.04.014Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, ChinaGuiju WuGuangliang YangHongbo TanThe 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, RES2DINV and Maxwell processing software to obtain 2D resistivity structure. The results showed that the layers with maximum resistivity values (30–33 Ω m on Line 1, 30–31 Ω m on Line 2, 32–40 Ω m on Line 3) are founded at station 1–7, and 14–20 on Line 1,13–18 on Line 2, and 8–13 and 16–20 on Line 3 which is predicted as goaf layer, and the minimum resistivity values (20–26 Ω m of TEM, 45–75 Ω 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.http://www.sciencedirect.com/science/article/pii/S1674984716300684Transient electromagnetic methodHigh density resistivity methodCoalmine goaf areasGeotechnicalElectrical
collection DOAJ
language English
format Article
sources DOAJ
author Guiju Wu
Guangliang Yang
Hongbo Tan
spellingShingle Guiju Wu
Guangliang Yang
Hongbo Tan
Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
Geodesy and Geodynamics
Transient electromagnetic method
High density resistivity method
Coalmine goaf areas
Geotechnical
Electrical
author_facet Guiju Wu
Guangliang Yang
Hongbo Tan
author_sort Guiju Wu
title Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
title_short Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
title_full Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
title_fullStr Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
title_full_unstemmed Mapping coalmine goaf using transient electromagnetic method and high density resistivity method in Ordos City, China
title_sort mapping coalmine goaf using transient electromagnetic method and high density resistivity method in ordos city, china
publisher KeAi Communications Co., Ltd.
series Geodesy and Geodynamics
issn 1674-9847
publishDate 2016-09-01
description 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, RES2DINV and Maxwell processing software to obtain 2D resistivity structure. The results showed that the layers with maximum resistivity values (30–33 Ω m on Line 1, 30–31 Ω m on Line 2, 32–40 Ω m on Line 3) are founded at station 1–7, and 14–20 on Line 1,13–18 on Line 2, and 8–13 and 16–20 on Line 3 which is predicted as goaf layer, and the minimum resistivity values (20–26 Ω m of TEM, 45–75 Ω 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.
topic Transient electromagnetic method
High density resistivity method
Coalmine goaf areas
Geotechnical
Electrical
url http://www.sciencedirect.com/science/article/pii/S1674984716300684
work_keys_str_mv AT guijuwu mappingcoalminegoafusingtransientelectromagneticmethodandhighdensityresistivitymethodinordoscitychina
AT guangliangyang mappingcoalminegoafusingtransientelectromagneticmethodandhighdensityresistivitymethodinordoscitychina
AT hongbotan mappingcoalminegoafusingtransientelectromagneticmethodandhighdensityresistivitymethodinordoscitychina
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