Electrical Anisotropic Response of Water Conducted Fractured Zone in the Mining Goaf

Based on the Maxwell equation, the occurrences of fractured zones are studied through the galvanic method. The electrical and magnetic fields are first derived in the spatial domain. To simplify the calculations, the computational formulas of the electrical fields in the spatial domain are transformed into the wavenumber domain by the Fourier transform. The basic solution of the electromagnetic field can thus be easily solved in the wavenumber domain. According to the boundary conditions, a recursive relationship between the different layers is established. The electromagnetic fields are obtained through the recursive relationships with the bottom-last layer. Finally, the apparent resistivity is calculated using the surface electric field. A typical goaf model is used for the numerical simulation. Based on the modeling results, the effectiveness of this method is determined. The modeling results indicate that the galvanic method is very effective for detecting the electrical anisotropic characters.

[1]  Zhixiong Li,et al.  A new compound faults detection method for rolling bearings based on empirical wavelet transform and chaotic oscillator , 2016 .

[2]  Misac N. Nabighian,et al.  Electromagnetic Methods in Applied Geophysics: Volume 2, Application, Parts A and B , 1991 .

[3]  C. Yin,et al.  Geoelectrical fields in a layered earth with arbitrary anisotropy , 1999 .

[4]  F. Abramovici,et al.  The electromagnetic fields of a horizontal dipole over a vertically inhomogeneous and anisotropic Earth , 1981 .

[5]  W. Sui,et al.  Interactions of overburden failure zones due to multiple-seam mining using longwall caving , 2015, Bulletin of Engineering Geology and the Environment.

[6]  Reza Malekian,et al.  Mine Safety System Using Wireless Sensor Network , 2016, IEEE Access.

[7]  Michael W. Asten The Influence of Electrical Anisotropy on Mise a la Masse Surveys , 1974 .

[8]  Jian-Hua Wang,et al.  Three-dimensional stability analysis of anisotropic and non-homogeneous slopes using limit analysis , 2014, Journal of Central South University.

[9]  G. M. Habberjam,et al.  The effect of structure and anisotropy on resistivity measurements , 1986 .

[10]  W. Brace,et al.  Electrical resistivity changes in saturated rocks during fracture and frictional sliding , 1968 .

[11]  G. Backus,et al.  A class of self-sustaining dissipative spherical dynamos , 1958 .

[12]  C. Balanis,et al.  Anisotropic Electrical Properties of Coal , 1980, IEEE Transactions on Geoscience and Remote Sensing.

[13]  T. D. Barber,et al.  The Effect Of Crossbedding Anisotropy On Induction Tool Response , 2001 .

[14]  SU Ben-yu Response characteristics of apparent resistivity of anisotropic laminar formation in direct current electric sounding , 2009 .