The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales
Abstract
Geophysics provides a multidimensional suite of investigative methods that are transforming our ability to see into the very fabric of the subsurface environment, and monitor the dynamics of its fluids and the biogeochemical reactions that occur within it. Here we document how geophysical methods have emerged as valuable tools for investigating shallow subsurface processes over the past two decades and offer a vision for future developments relevant to hydrology and also ecosystem science. The field of “hydrogeophysics” arose in the late 1990s, prompted, in part, by the wealth of studies on stochastic subsurface hydrology that argued for better field-based investigative techniques. These new hydrogeophysical approaches benefited from the emergence of practical and robust data inversion techniques, in many cases with a view to quantify shallow subsurface heterogeneity and the associated dynamics of subsurface fluids. Furthermore, the need for quantitative characterization stimulated a wealth of new investigations into petrophysical relationships that link hydrologically relevant properties to measurable geophysical parameters. Development of time-lapse approaches provided a new suite of tools for hydrological investigation, enhanced further with the realization that some geophysical properties may be sensitive to biogeochemical transformations in the subsurface environment, thus opening up the new field of “biogeophysics.” Early hydrogeophysicalmore »
- Authors:
-
- Lancaster Univ. (United Kingdom). Lancaster Environment Centre
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Agrosphere Institute (IBG 3), Jülich (Germany)
- Colorado School of Mines, Golden, CO (United States); Univ. de Savoie, Le Bourget du Lac (France)
- Center for Ecology and Hydrology, Bangor (United Kingdom)
- Colorado School of Mines, Golden, CO (United States)
- Rutgers University-Newark, NJ (United States)
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1257339
- Grant/Contract Number:
- AC02-05CH11231
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Water Resources Research
- Additional Journal Information:
- Journal Volume: 51; Journal Issue: 6; Journal ID: ISSN 0043-1397
- Publisher:
- American Geophysical Union (AGU)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES
Citation Formats
Binley, Andrew, Hubbard, Susan S., Huisman, Johan A., Revil, André, Robinson, David A., Singha, Kamini, and Slater, Lee D. The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales. United States: N. p., 2015.
Web. doi:10.1002/2015wr017016.
Binley, Andrew, Hubbard, Susan S., Huisman, Johan A., Revil, André, Robinson, David A., Singha, Kamini, & Slater, Lee D. The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales. United States. https://doi.org/10.1002/2015wr017016
Binley, Andrew, Hubbard, Susan S., Huisman, Johan A., Revil, André, Robinson, David A., Singha, Kamini, and Slater, Lee D. Mon .
"The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales". United States. https://doi.org/10.1002/2015wr017016. https://www.osti.gov/servlets/purl/1257339.
@article{osti_1257339,
title = {The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales},
author = {Binley, Andrew and Hubbard, Susan S. and Huisman, Johan A. and Revil, André and Robinson, David A. and Singha, Kamini and Slater, Lee D.},
abstractNote = {Geophysics provides a multidimensional suite of investigative methods that are transforming our ability to see into the very fabric of the subsurface environment, and monitor the dynamics of its fluids and the biogeochemical reactions that occur within it. Here we document how geophysical methods have emerged as valuable tools for investigating shallow subsurface processes over the past two decades and offer a vision for future developments relevant to hydrology and also ecosystem science. The field of “hydrogeophysics” arose in the late 1990s, prompted, in part, by the wealth of studies on stochastic subsurface hydrology that argued for better field-based investigative techniques. These new hydrogeophysical approaches benefited from the emergence of practical and robust data inversion techniques, in many cases with a view to quantify shallow subsurface heterogeneity and the associated dynamics of subsurface fluids. Furthermore, the need for quantitative characterization stimulated a wealth of new investigations into petrophysical relationships that link hydrologically relevant properties to measurable geophysical parameters. Development of time-lapse approaches provided a new suite of tools for hydrological investigation, enhanced further with the realization that some geophysical properties may be sensitive to biogeochemical transformations in the subsurface environment, thus opening up the new field of “biogeophysics.” Early hydrogeophysical studies often concentrated on relatively small “plot-scale” experiments. More recently, however, the translation to larger-scale characterization has been the focus of a number of studies. In conclusion, geophysical technologies continue to develop, driven, in part, by the increasing need to understand and quantify key processes controlling sustainable water resources and ecosystem services.},
doi = {10.1002/2015wr017016},
journal = {Water Resources Research},
number = 6,
volume = 51,
place = {United States},
year = {Mon Jun 15 00:00:00 EDT 2015},
month = {Mon Jun 15 00:00:00 EDT 2015}
}
Web of Science
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4D Active Time Constrained Resistivity Inversion
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