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Coal Geology & Exploration

Abstract

The borehole geophysical prospecting method is a research hotspot in recent years. Considering that the down-hole transient electromagnetic method used in metal mines has the characteristics of long radial detection distance and less susceptible to surface electromagnetic interference, it is applied to the exploration of water-filled goaf in coal mines. Three-dimensional finite-difference time-domain(FDTD) algorithm is used to simulate the total field response and abnormal response of the goaf model with different orientations of boreholes. The total field three-component could reflect the water-filled goaf obviously, and the abnormal field three-component shape combination can distinguish the azimuth of the abnormal body. Based on the principle of equivalent eddy current, the spatial location algorithm is studied, which can obtain the position, inclination and scale of anomalous body by using three components of anomalous field. By testing the theoretical models in different directions, the combination of the size and location of the equivalent current loop inverted at different times can reflect the spatial position and scale of the water-filled goaf. Finally, the down-hole TEM detection test was carried out in a mine in northern Shaanxi Province. The location and size of the water-bearing goaf were known in this area. The collected three-component signals are smooth and reliable, and the abnormal response is obvious. The three-component data of anomalous field at different time are retrieved and processed. The inversion results are basically consistent with the actual location and scale of the goaf, which proves that this method can be used as an effective means to explore the water-filled goaf through boreholes in coal mines.

Keywords

down-hole TEM, three-component response, advanced detection, three-dimensional finite-difference time-domain(FDTE) algorithm, the spatial localization algorithm

DOI

10.3969/j.issn.1001-1986.2019.05.008

Reference

[1] 刘志民,刘希高,张金涛,等. 交流聚焦激电法煤巷超前探测阻容试验模拟[J]. 煤炭学报,2015,40(9):2144-2151. LIU Zhimin,LIU Xigao,ZHANG Jintao,et al. Experimental simulation of resistance-capacitance model for advanced detection in coal roadway based on alternating current focusing induced polarization method[J]. Journal of China Coal Society,2015,40(9):2144-2151.

[2] 程久龙,李明星,肖艳丽,等. 全空间条件下矿井瞬变电磁法粒子群优化反演研究[J]. 地球物理学报,2014,57(10):3478-3484. CHENG Jiulong,LI Mingxing,XIAO Yanli,et al. Study on particle swarm optimization inversion of mine transient electromagnetic method in whole-space[J]. Chinese Journal of Geophysics,2014,57(10):3478-3484.

[3] 刘诗竹,石颖,郭雪豹,等. VSP数据逆时偏移方法研究[J]. 地球物理学进展,2014,29(5):2211-2218. LIU Shizhu,SHI Ying,GUO Xuebao,et al. Investugation on reverse-time migration of VSP data[J]. Progress in Geophysics,2014,29(5):2211-2218.

[4] 刘四新,孟旭,傅磊. 不依赖源子波的跨孔雷达时间域波形反演[J]. 地球物理学报,2016,59(12):4473-4482. LIU Sixin,MENG Xu,FU Lei. Source-independent time-domain waveform inversion of cross-hole GPR data[J]. Chinese Journal of Geophysics,2016,59(12):4473-4482.

[5] 苗彬,姜志海,刘树才. 矿井地面-巷道瞬变电磁探测系统设计及应用[J]. 煤炭科学技术,2016,44(12):148-153. MIAO Bin,JIANG Zhihai,LIU Shucai. Design and appli-cation of transient electromagnetic detection system on mine surface ground and in underground mine roadway[J]. Coal Science and Technology,2016,44(12):148-153.

[6] WOODS D V. A model study of the crone borehole pulse electromagnetic(PEM) system[D]. Kingston,Ontario:Queen's University,1975.

[7] EATON P A,HOHMANN G W. The influence of a con-ductive host on two-dimensional borehole transient electromagnetic responses[J]. Geophysics,1984,49(7):861-869.

[8] WEST R C,WARD S H. The borehole transient EM of a three-dimensional fractured zone in a conductive half space[J]. Geophysics,1988,53(11):1469-1478.

[9] BARNETT C T. Simple inversion of time-domain electromagnetic data[J]. Geophysics,1984,49(7):925-933.

[10] DUNCAN A C. Interpretation of down-hole transient EM data using current filaments[J]. Exploration Geophysics,1987,18(2):36-39.

[11] BISHOP J R,LEWIS R J G,MACNAE J C. Down-hole electromagnetic surveys at Renison Bell,Tasmania[J]. Exploration Geophysics,1987,18(3):265-277.

[12] ELDERS J,WELLINGTON A. An application of reverse coupling to increase signal strength beneath conductive sediments-Miitel mine,Kambalda,W. A.[J]. Exploration Geophysics,1998,29(4):355-360.

[13] STOLZ E M G. Direct detection of gold bearing structures at St Ives,WA-DHEM vs DHMMR[J]. Exploration Geophysics,2003,34(1/2):131-135.

[14] JOHNSON D,SHEPPARD S,PAGGI J,et al. Discovery of the Moran massive nickel sulphide deposit using down-hole transient electromagnetic surveying[C]//ASEG2010 21st Geophysical Conference. 2010:1-4.

[15] 蒋邦远. 实用近区磁源瞬变电磁法勘探[M]. 北京:地质出版社,1998.

[16] 杨毅,邓晓红,张杰,等. 一种井中瞬变电磁异常反演方法[J]. 物探与化探,2014,38(4):855-859. YANG Yi,DENG Xiaohong,ZHANG Jie,et al. A borehole TEM anomaly inversion method[J]. Geophysical and Geochemical Exploration,2014,38(4):855-859.

[17] 张杰,邓晓红,谭捍东,等. 地-井瞬变电磁资料矢量交会解释方法[J]. 物探与化探,2015,39(3):572-579. ZHANG Jie,DENG Xiaohong,TAN Handong,et al. A study of vector intersection for borehole transient electromagnetic method[J]. Geophysical and Geochemical Exploration,2015,39(3):572-579.

[18] 张海涛,许光泉. 采空区冒落结构与充水性特征[J]. 煤田地质与勘探,2018,46(4):99-102. ZHANG Haitao,XU Guangquan. Research on caving structure and water filling characteristic of goaf[J]. Coal Geology & Exploration,2018,46(4):99-102.

[19] 孙怀凤,李貅,李术才,等. 考虑关断时间的回线源激发TEM三维时域有限差分正演[J]. 地球物理学报,2013,56(3):1049-1064. SUN Huaifeng,LI Xiu,LI Shucai,et al. Three dimensional FDTD modeling of TEM excited by a loop source considering ramp time[J]. Chinese Journal of Geophysics,2013,56(3):1049-1064.

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