Two-dimensional inversion of spectral induced polarization data using MPI parallel algorithm in data space
Zhang Zhi-Yong1,2,Tan Han-Dong1,2, Wang Kun-Peng1,2, Lin Chang-Hong1,2, Zhang Bin3, and Xie Mao-Bi1,2
1. School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China.
2. Key Laboratory of Geo-detection (China University of Geosciences, Beijing), Ministry of Education, Beijing 100083, China.
3. China Non-ferrous Metals Resource Geological Survey, Beijing 100012, China.
Abstract Traditional two-dimensional (2D) complex resistivity forward modeling is based on Poisson’s equation but spectral induced polarization (SIP) data are the coproducts of the induced polarization (IP) and the electromagnetic induction (EMI) effects. This is especially true under high frequencies, where the EMI effect can exceed the IP effect. 2D inversion that only considers the IP effect reduces the reliability of the inversion data. In this paper, we derive differential equations using Maxwell’s equations. With the introduction of the Cole–Cole model, we use the finite-element method to conduct 2D SIP forward modeling that considers the EMI and IP effects simultaneously. The data-space Occam method, in which different constraints to the model smoothness and parametric boundaries are introduced, is then used to simultaneously obtain the four parameters of the Cole–Cole model using multi-array electric field data. This approach not only improves the stability of the inversion but also significantly reduces the solution ambiguity. To improve the computational efficiency, message passing interface programming was used to accelerate the 2D SIP forward modeling and inversion. Synthetic datasets were tested using both serial and parallel algorithms, and the tests suggest that the proposed parallel algorithm is robust and efficient.
This work is jointly sponsored by the National Natural Science Foundation of China (Grant No. 41374078) , the Geological Survey Projects of the Ministry of Land and Resources of China (Grant Nos. 12120113086100 and 12120113101300), and Beijing Higher Education Young Elite Teacher Project.
Cite this article:
Zhang Zhi-Yong,Tan Han-Dong,Wang Kun-Peng et al. Two-dimensional inversion of spectral induced polarization data using MPI parallel algorithm in data space[J]. APPLIED GEOPHYSICS, 2016, 13(1): 13-24.
[1]
Attwa, M., and Günther, T., 2013, Spectral induced polarization measurements for environmental purposes and predicting the hydraulic conductivity in sandy aquifers: Hydrology and Earth System Sciences Discussions, 10(4), 5315-5354.
[2]
Avdeev, D. B., 2005, Three-dimensional electromagnetic modelling and inversion from theory to application: Surveys in Geophysics, 26(6), 767-799.
[3]
Commer, M., and Newman, G. A., 2008, New advances in three-dimensional controlled-source electromagnetic inversion: Geophysical Journal International, 172(2), 513-535.
[4]
Constable, C. S., Parker, R. L., and Constable, C. G., 1987, Occam’s inversion: A practical algorithm for generating a smooth models from electromagnetic sounding data: Geophysics, 52(3), 289-300.
[5]
Egbert, G. D., Bennett, A. F., and Foreman, M. G.G., 1994, TOPEX/POSEIDON tides estimated using a global inverse model: Journal of Geophysical Research, 99(c12), 24821-24852.
[6]
Fan, C. S., Li, T. L., and Yan, J. Y., 2012, Research and application experiment on 2.5D SIP inversion: Chinese Journal of Geophysics (in Chinese), 55(12), 4044-4050.
[7]
Fan, C. S., 2013, Research on complex resistivity forward and inversion with finite element method and its application: PhD Thesis, Jilin University.
[8]
Kemna, A., Binley, A., Ramirez, A., and Daily, W., 2000, Complex resistivity tomography for environmental applications: Chemical Engineering Journal, 77(1), 11-18.
[9]
Key, K., and Ovall, J., 2011, A parallel goal-oriented adaptive finite element method for 2.5-D electromagnetic modelling: Geophysical Journal International, 186(1), 137-154.
[10]
Kim, H. J., Song, Y., and Lee, K. H., 1999, Inequality constraint in least-squares inversion of geophysical data: Earth Planets Space, 51, 255-259.
[11]
Li, Y. G., and Key, K., 2007, 2D marine controlled-source electromagnetic modeling: Part 1 - An adaptive finite-element algorithm: Geophysics, 72(2), WA51-WA62.
[12]
Loke, M. H., Chambers J. E., and Ogilvy., R. D., 2006, Inversion of 2D spectral induced polarization imaging data: Geophysical Prospecting, 54(3), 287-301.
[13]
McGillivray, P. R., Oldenburg, D. W., Ellis R. G., and Habashy, T. M., 1994, Calculation of sensitivities for the frequency-domain electromagnetic problem: Geophysical Journal International, 116(1), 1-4.
[14]
Mitsuhata, Y., 2000, 2-D electromagnetic modeling by finite-element method with a dipole source and topography: Geophysics, 65(2), 465-475.
[15]
Nabighian, M. N., 1988, Electromagnetic Methods in Applied Geophysics, vol. 1: Theory. Society of Exploration Geophysicists.
[16]
Pacheco, P. S., 2011, An Introduction to Parallel Programming, Morgan Kaufann Publ. Inc.
[17]
Pelton, W. H., Ward, S. H., Hallof, P. G., Sill, W. R., and Nelson, P. H., 1978, Mineral discrimination and removal of inductive coupling with multifrequency IP: Geophysics, 43(3), 588-609.
[18]
Revil, A., Karaoulis, M., Johnson, T., and Kemna., A., 2012, Review: Some low-frequency electrical methods for subsurface characterization and monitoring in hydrogeology: Hydrogeology Journal, 20(4), 617-658.
[19]
Routh, P. S., Oldenburg, D. W., and Li, Y. G., 1998, Regularized inversion of spectral IP parameters from complex resistivity data: 68th Annual International Meeting, SEG Expanded Abstracts, 810−813.
[20]
Schwartz, N., and Furman, A., 2012, Spectral induced polarization signature of soil contaminated by organic pollutant: Experiment and modeling: Journal of Geophysical Research, 117, B10203.
[21]
Shin, S., Park, S., and Shin, D, 2015, Spectral-induced polarization characteristics of rock types from the skarn deposit in Gagok Mine, Taebaeksan Basin, South Korea: Environmental Earth Sciences, 73(12), 8325-8331.
[22]
Siripunvaraporn, W., and Egbert, G., 2000, An efficient data-subspace inversion method for 2-D magnetotelluric data: Geophysics, 65(3), 791-803.
[23]
Siripunvaraporn, W., Egbert, G., Lenbury, Y., and Uyeshima, M., 2005, Three-dimensional magnetotelluric inversion: data space method: Physics of the Earth and Planetary Interiors, 150(1-3), 3-14.
[24]
Xu, K. J., 2007, Study on 2.5D complex resistivity electromagnetic forward and inversion: PhD Thesis, Jilin University.
[25]
Yang, J., 2011, Environmental and Engineering Geophysics: GeologicalPublishingHouse, Beijing.
[26]
Zhao, G. M., 2009, Research of complex resistivity 2.5D electromagnetic forward and inversion with topography: PhD Thesis, Jilin University.
[27]
Zienkiewicz, O. C., 1977. The finite element method, McGraw-Hill Book Co.