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Title: Time-series analysis of surface deformation at Brady Hot Springs geothermal field (Nevada) using interferometric synthetic aperture radar

Abstract

For this work, we analyze interferometric synthetic aperture radar (InSAR) data acquired between 2004 and 2014, by the ERS-2, Envisat, ALOS and TerraSAR-X/TanDEM-X satellite missions to measure and characterize time-dependent deformation at the Brady Hot Springs geothermal field in western Nevada due to extraction of fluids. The long axis of the ~4 km by ~1.5 km elliptical subsiding area coincides with the strike of the dominant normal fault system at Brady. Within this bowl of subsidence, the interference pattern shows several smaller features with length scales of the order of ~1 km. This signature occurs consistently in all of the well-correlated interferometric pairs spanning several months. Results from inverse modeling suggest that the deformation is a result of volumetric contraction in shallow units, no deeper than 600 m, likely associated with damaged regions where fault segments mechanically interact. Such damaged zones are expected to extend downward along steeply dipping fault planes, providing a high permeability conduit to the production wells. Using time series analysis, we test the hypothesis that geothermal production drives the observed deformation. We find a good correlation between the observed deformation rate and the rate of production in the shallow wells. We also explore mechanisms that couldmore » potentially cause the observed deformation, including thermal contraction of rock, decline in pore pressure and dissolution of minerals over time.« less

Authors:
; ; ; ; ; ; ; ; ; ; ;
Publication Date:
Research Org.:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States); Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States); Univ. of Wisconsin, Madison, WI (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences, and Biosciences Division; European Space Agency (ESA); National Aeronautics and Space Administration (NASA); German Space Agency (DLR); National Science Foundation (NSF); USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office
OSTI Identifier:
1266399
Alternate Identifier(s):
OSTI ID: 1474937; OSTI ID: 1618446
Grant/Contract Number:  
AC02-05CH11231; EE0005510; EE0006760; DGE-1256259
Resource Type:
Published Article
Journal Name:
Geothermics
Additional Journal Information:
Journal Name: Geothermics Journal Volume: 61 Journal Issue: C; Journal ID: ISSN 0375-6505
Publisher:
Elsevier
Country of Publication:
United Kingdom
Language:
English
Subject:
58 GEOSCIENCES; 47 OTHER INSTRUMENTATION; InSAR deformation; 15 GEOTHERMAL ENERGY

Citation Formats

Ali, S. T., Akerley, J., Baluyut, E. C., Cardiff, M., Davatzes, N. C., Feigl, K. L., Foxall, W., Fratta, D., Mellors, R. J., Spielman, P., Wang, H. F., and Zemach, E. Time-series analysis of surface deformation at Brady Hot Springs geothermal field (Nevada) using interferometric synthetic aperture radar. United Kingdom: N. p., 2016. Web. doi:10.1016/j.geothermics.2016.01.008.
Ali, S. T., Akerley, J., Baluyut, E. C., Cardiff, M., Davatzes, N. C., Feigl, K. L., Foxall, W., Fratta, D., Mellors, R. J., Spielman, P., Wang, H. F., & Zemach, E. Time-series analysis of surface deformation at Brady Hot Springs geothermal field (Nevada) using interferometric synthetic aperture radar. United Kingdom. https://doi.org/10.1016/j.geothermics.2016.01.008
Ali, S. T., Akerley, J., Baluyut, E. C., Cardiff, M., Davatzes, N. C., Feigl, K. L., Foxall, W., Fratta, D., Mellors, R. J., Spielman, P., Wang, H. F., and Zemach, E. Thu . "Time-series analysis of surface deformation at Brady Hot Springs geothermal field (Nevada) using interferometric synthetic aperture radar". United Kingdom. https://doi.org/10.1016/j.geothermics.2016.01.008.
@article{osti_1266399,
title = {Time-series analysis of surface deformation at Brady Hot Springs geothermal field (Nevada) using interferometric synthetic aperture radar},
author = {Ali, S. T. and Akerley, J. and Baluyut, E. C. and Cardiff, M. and Davatzes, N. C. and Feigl, K. L. and Foxall, W. and Fratta, D. and Mellors, R. J. and Spielman, P. and Wang, H. F. and Zemach, E.},
abstractNote = {For this work, we analyze interferometric synthetic aperture radar (InSAR) data acquired between 2004 and 2014, by the ERS-2, Envisat, ALOS and TerraSAR-X/TanDEM-X satellite missions to measure and characterize time-dependent deformation at the Brady Hot Springs geothermal field in western Nevada due to extraction of fluids. The long axis of the ~4 km by ~1.5 km elliptical subsiding area coincides with the strike of the dominant normal fault system at Brady. Within this bowl of subsidence, the interference pattern shows several smaller features with length scales of the order of ~1 km. This signature occurs consistently in all of the well-correlated interferometric pairs spanning several months. Results from inverse modeling suggest that the deformation is a result of volumetric contraction in shallow units, no deeper than 600 m, likely associated with damaged regions where fault segments mechanically interact. Such damaged zones are expected to extend downward along steeply dipping fault planes, providing a high permeability conduit to the production wells. Using time series analysis, we test the hypothesis that geothermal production drives the observed deformation. We find a good correlation between the observed deformation rate and the rate of production in the shallow wells. We also explore mechanisms that could potentially cause the observed deformation, including thermal contraction of rock, decline in pore pressure and dissolution of minerals over time.},
doi = {10.1016/j.geothermics.2016.01.008},
journal = {Geothermics},
number = C,
volume = 61,
place = {United Kingdom},
year = {Thu Feb 04 00:00:00 EST 2016},
month = {Thu Feb 04 00:00:00 EST 2016}
}

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