Bayesian magnetotelluric inversion using methylene blue structural priors for imaging shallow conductors in geothermal fields

Author:

Ardid Alberto1ORCID,Dempsey David1,Bertrand Edward2ORCID,Sepulveda Fabian3,Tarits Pascal4,Solon Flora5,Archer Rosalind1

Affiliation:

1. University of Auckland, Department of Engineering Science, Auckland 1010, New Zealand.(corresponding author); .

2. GNS Science, Lower Hutt 5040, New Zealand..

3. Contact Energy Ltd, Wairakei Power Station, Taupo 3352, New Zealand..

4. Université de Bretagne Occidentale, Brest 6538, France..

5. Observatorio Nacional, Department of Geophysics, Rio de Janeiro 20921-400, Brazil..

Abstract

In geothermal exploration, magnetotelluric (MT) data and inversion models are commonly used to image shallow conductors typically associated with the presence of an electrically conductive clay cap that overlies the main reservoir. However, these inversion models suffer from nonuniqueness and uncertainty, and the inclusion of useful geologic information is still limited. We have developed a Bayesian inversion method that integrates the electrical resistivity distribution from MT surveys with borehole methylene blue (MeB) data, an indicator of conductive clay content. The MeB data were used to inform structural priors for the MT Bayesian inversion that focus on inferring with uncertainty the shallow conductor boundary in geothermal fields. By incorporating borehole information, our inversion reduced nonuniqueness and then explicitly represented the irreducible uncertainty as estimated depth intervals for the conductor boundary. We used the Markov chain Monte Carlo and a 1D three-layer resistivity model to accelerate the Bayesian inversion of the MT signal beneath each station. Then, inferred conductor boundary distributions were interpolated to construct pseudo-2D/3D models of the uncertain conductor geometry. We compare our approach against deterministic MT inversion software on synthetic and field examples, and our approach has good performance in estimating the depth to the bottom of the conductor, a valuable target in geothermal reservoir exploration.

Funder

Ministry for Business, Innovation and Employment of New Zealand

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Anderson, E., D. Crosby, and G. Ussher, 2000, Bulls-Eye! — Simple resistivity imaging to reliably locate the geothermal reservoir: World Geothermal Congress, 909–914.

2. Ardid, A., D. Dempsey, T. Bertrand, and R. Archer, 2018, Uncertain estimation of subsurface temperature away from the borehole using magnetotelluric inversions: 40th New Zealand Geothermal Workshop.

3. Arnason, K., R. Karlsdottir, H. Eysteinsson, O. G. Flovenz, and S. T. Gudlaugsson, 2000, The resistivity of high-temperature geothermal systems in Iceland: World Geothermal Congress.

4. Layered and laterally constrained 2D inversion of resistivity data

5. Definitions of apparent resistivity for the presentation of magnetotelluric sounding data1

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