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The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales

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The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales. / Binley, Andrew; Hubbard, Susan; Huisman, Johan et al.
In: Water Resources Research, Vol. 51, 2015, p. 1-30.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Binley, A, Hubbard, S, Huisman, J, Revil, A, Robinson, D, Singha, K & Slater, L 2015, 'The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales', Water Resources Research, vol. 51, pp. 1-30. https://doi.org/10.1002/2015WR017016

APA

Binley, A., Hubbard, S., Huisman, J., Revil, A., Robinson, D., Singha, K., & Slater, L. (2015). The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales. Water Resources Research, 51, 1-30. https://doi.org/10.1002/2015WR017016

Vancouver

Binley A, Hubbard S, Huisman J, Revil A, Robinson D, Singha K et al. The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales. Water Resources Research. 2015;51:1-30. Epub 2015 May 13. doi: 10.1002/2015WR017016

Author

Binley, Andrew ; Hubbard, Susan ; Huisman, Johan et al. / The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales. In: Water Resources Research. 2015 ; Vol. 51. pp. 1-30.

Bibtex

@article{dbc357fe42af4a3381bc4b45ea97ed64,
title = "The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales",
abstract = "Geophysics provides a multi-dimensional 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 {\textquoteleft}plot-scale{\textquoteright} experiments. More recently, however, the translation to larger-scale characterization has been the focus of a number of studies. 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. ",
author = "Andrew Binley and Susan Hubbard and Johan Huisman and Andre Revil and David Robinson and Kamini Singha and Lee Slater",
note = "Copyright 2015 American Geophysical Union Evidence of acceptance is on publishers version.",
year = "2015",
doi = "10.1002/2015WR017016",
language = "English",
volume = "51",
pages = "1--30",
journal = "Water Resources Research",
issn = "0043-1397",
publisher = "AMER GEOPHYSICAL UNION",

}

RIS

TY - JOUR

T1 - The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales

AU - Binley, Andrew

AU - Hubbard, Susan

AU - Huisman, Johan

AU - Revil, Andre

AU - Robinson, David

AU - Singha, Kamini

AU - Slater, Lee

N1 - Copyright 2015 American Geophysical Union Evidence of acceptance is on publishers version.

PY - 2015

Y1 - 2015

N2 - Geophysics provides a multi-dimensional 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. 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.

AB - Geophysics provides a multi-dimensional 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. 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.

U2 - 10.1002/2015WR017016

DO - 10.1002/2015WR017016

M3 - Journal article

VL - 51

SP - 1

EP - 30

JO - Water Resources Research

JF - Water Resources Research

SN - 0043-1397

ER -