Research on three-dimensional full-space transient electromagnetic modeling for advanced prediction

被引:0
作者
Yang, Haiyan [1 ]
Deng, Juzhi [1 ]
Yue, Jianhua [2 ]
机构
[1] Coll Nucl Engn & Technol ECIT, Fuzhou 344000, Jiangxi, Peoples R China
[2] China Univ Min & Technol, Sch Resource & Earth Sci, Xuzhou 221116, Jiangsu, Peoples R China
来源
NEAR-SURFACE GEOPHYSICS AND GEOHAZARDS - PROCEEDINGS OF THE 4TH INTERNATIONAL CONFERENCE ON ENVIRONMENTAL AND ENGINEERING GEOPHYSICS, VOLS 1 AND 2 | 2010年
关键词
full-space; transient electromagnetic method; advanced prediction; modeling; apparent resistivity; FINITE-DIFFERENCE;
D O I
暂无
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
The 3D full-space TEM modeling algorithm was implemented by directly solving diffusion equation using time-domain finite-difference method, calculating field components adopting remedial Liao's absorbing boundary condition, and correspondingly applying Laplace equation and "upper continuation" method to tunnel space and its boundary. Based on analyzed solution of loop source in uniform full-space, full-space "late-time" apparent resistivity formula was derived. And then, advanced prediction of water inrush structure was simulated. The results indicate that, the remedial ABC has a better effect than Dirichlet condition when modeling diffusion of electromagnetic field in 3D infinite medium. Full-space apparent resistivity value is 1.842 times than half-space for the same loop parameters. Transient response at tunnel end is proportional to the resistivity contrast between anomaly structure and its surrounding rock, and reciprocally proportional to the distance of the structure to observation point. However, to the high-resistivity structure, the change of its resistivity has a limited effect to transient response. And also, transient response of the structure is submerged by the response of surrounding rock for the long distance between the structure and observation point.
引用
收藏
页码:529 / 533
页数:5
相关论文
共 6 条
[1]   DIFFUSION OF ELECTROMAGNETIC-FIELDS INTO A TWO-DIMENSIONAL EARTH - A FINITE-DIFFERENCE APPROACH [J].
ORISTAGLIO, ML ;
HOHMANN, GW .
GEOPHYSICS, 1984, 49 (07) :870-894
[2]   A FINITE-DIFFERENCE, TIME-DOMAIN SOLUTION FOR 3-DIMENSIONAL ELECTROMAGNETIC MODELING [J].
WANG, T ;
HOHMANN, GW .
GEOPHYSICS, 1993, 58 (06) :797-809
[3]  
Ward S. H., 1987, Electromagnetic theory for geophysical applications
[4]  
[杨海燕 YANG Hai-yan], 2009, [中国矿业大学学报. 自然科学版, Journal of China University of Mining & Technology], V38, P263
[5]  
[岳建华 YUE Jianhua], 2008, [中国矿业大学学报. 自然科学版, Journal of China University of Mining & Technology], V37, P152
[6]  
[岳建华 YUE Jianhua], 2007, [地球物理学进展, Progress in Geophysiscs], V22, P1904