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• W2103734908 abstract "We propose an algorithm to invert self‐potential signals measured at the ground surface of the Earth to localize hydromechanical disturbances or to the pattern of groundwater flow in geothermal systems. The self‐potential signals result from the divergence of the streaming current density. Groundwater flow can be either driven by topography of the water table, free convection, or deformation of the medium. The algorithm includes the electrical resistivity distribution of the medium obtained independently by DC resistance tomography or electromagnetic methods or by coding the assumed geology in terms of distribution of the electrical resistivity accounting for the effect of the temperature and salinity distributions and possibly constraints from borehole measurements. Inversion of the distribution of the source current density from ground surface and borehole self‐potential measurements is achieved by solving the inverse problem using Tikhonov regularization solutions that are compatible with the physics of the primary flow problem. By introducing assumptions regarding the smoothness or the compactness of the source and the three‐dimensional distribution of the electrical resistivity of the system, the inverse problem can be solved in obtaining the three‐dimensional distribution of the current source density in the ground. However, an annihilator can be added to the inverted source geometry without affecting the measured self‐potential field. Annihilators can be obtained from boundary conditions. Synthetic models and a sandbox experiment are discussed to demonstrate the validity of the algorithm. An application is presented to the geothermal field of Cerro Prieto, Baja California, Mexico, using literature data. Inversion of the self‐potential and resistivity data allows observing a plume of hot groundwater rising to the ground surface in the central part of the investigated area and discharging to the ground surface in the southwest part. The temperature anomaly associated with the existence of this plume is independently observed by interpolating borehole temperature measurements. We found a good agreement between the distribution of the temperature and the inverted source current density. The proposed method appears therefore as a noninvasive method for remote detection and three‐dimensional mapping of subsurface groundwater flow." @default.
• W2103734908 created "2016-06-24" @default.
• W2103734908 creator A5012032240 @default.
• W2103734908 creator A5014431902 @default.
• W2103734908 creator A5039775952 @default.
• W2103734908 creator A5073873241 @default.
• W2103734908 date "2008-09-01" @default.
• W2103734908 modified "2023-10-15" @default.
• W2103734908 title "Three-dimensional inversion of self-potential data used to constrain the pattern of groundwater flow in geothermal fields" @default.
• W2103734908 cites W1527734755 @default.
• W2103734908 cites W1529484146 @default.
• W2103734908 cites W1566547199 @default.
• W2103734908 cites W1594234351 @default.
• W2103734908 cites W1603753160 @default.
• W2103734908 cites W1700117005 @default.
• W2103734908 cites W1931441157 @default.
• W2103734908 cites W1959802413 @default.
• W2103734908 cites W1964083733 @default.
• W2103734908 cites W1966717045 @default.
• W2103734908 cites W1968692372 @default.
• W2103734908 cites W1969467876 @default.
• W2103734908 cites W1972594000 @default.
• W2103734908 cites W1973789490 @default.
• W2103734908 cites W1975939793 @default.
• W2103734908 cites W1976680618 @default.
• W2103734908 cites W1978011721 @default.
• W2103734908 cites W1980115943 @default.
• W2103734908 cites W1980179959 @default.
• W2103734908 cites W1987153612 @default.
• W2103734908 cites W1988674615 @default.
• W2103734908 cites W1989137372 @default.
• W2103734908 cites W1989719232 @default.
• W2103734908 cites W1994604904 @default.
• W2103734908 cites W1995837749 @default.
• W2103734908 cites W1996504626 @default.
• W2103734908 cites W1996528796 @default.
• W2103734908 cites W1999529206 @default.
• W2103734908 cites W2001956271 @default.
• W2103734908 cites W2002480432 @default.
• W2103734908 cites W2003475047 @default.
• W2103734908 cites W2004025925 @default.
• W2103734908 cites W2004317278 @default.
• W2103734908 cites W2007780304 @default.
• W2103734908 cites W2008756302 @default.
• W2103734908 cites W2013469569 @default.
• W2103734908 cites W2014818218 @default.
• W2103734908 cites W2015991683 @default.
• W2103734908 cites W2019945415 @default.
• W2103734908 cites W2021925644 @default.
• W2103734908 cites W2022184598 @default.
• W2103734908 cites W2027128207 @default.
• W2103734908 cites W2031366688 @default.
• W2103734908 cites W2031677974 @default.
• W2103734908 cites W2032294405 @default.
• W2103734908 cites W2033524684 @default.
• W2103734908 cites W2036290829 @default.
• W2103734908 cites W2038370704 @default.
• W2103734908 cites W2044954481 @default.
• W2103734908 cites W2045762563 @default.
• W2103734908 cites W2046107702 @default.
• W2103734908 cites W2047494001 @default.
• W2103734908 cites W2048295824 @default.
• W2103734908 cites W2049195475 @default.
• W2103734908 cites W2050929040 @default.
• W2103734908 cites W2051627858 @default.
• W2103734908 cites W2055351482 @default.
• W2103734908 cites W2060090090 @default.
• W2103734908 cites W2065380553 @default.
• W2103734908 cites W2069990872 @default.
• W2103734908 cites W2070797356 @default.
• W2103734908 cites W2072679657 @default.
• W2103734908 cites W2073471899 @default.
• W2103734908 cites W2076903253 @default.
• W2103734908 cites W2079131267 @default.
• W2103734908 cites W2085173122 @default.
• W2103734908 cites W2086495404 @default.
• W2103734908 cites W2087973278 @default.
• W2103734908 cites W2091182627 @default.
• W2103734908 cites W2094675334 @default.
• W2103734908 cites W2095591137 @default.
• W2103734908 cites W2099587512 @default.
• W2103734908 cites W2105363220 @default.
• W2103734908 cites W2105986146 @default.
• W2103734908 cites W2108989885 @default.
• W2103734908 cites W2121703172 @default.
• W2103734908 cites W2134872477 @default.
• W2103734908 cites W2135842450 @default.
• W2103734908 cites W2136369356 @default.
• W2103734908 cites W2139927284 @default.
• W2103734908 cites W2141694229 @default.
• W2103734908 cites W2146283173 @default.
• W2103734908 cites W2152242052 @default.
• W2103734908 cites W2157030347 @default.
• W2103734908 cites W2159148670 @default.
• W2103734908 cites W2165320784 @default.
• W2103734908 cites W2165905458 @default.
• W2103734908 cites W2168073864 @default.
• W2103734908 cites W2170553086 @default.
• W2103734908 cites W2332990274 @default.
• W2103734908 cites W295191659 @default.

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