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

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TLDR
How geophysical methods have emerged as valuable tools for investigating shallow subsurface processes over the past two decades is documented and a vision for future developments relevant to hydrology and also ecosystem science is offered.
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 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.

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References
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Electromagnetic determination of soil water content: Measurements in coaxial transmission lines

TL;DR: The dependence of the dielectric constant, at frequencies between 1 MHz and 1 GHz, on the volumetric water content is determined empirically in the laboratory as discussed by the authors, and the effect of varying the texture, bulk density, temperature, and soluble salt content on this relationship was also determined.
Journal ArticleDOI

Occam's inversion; a practical algorithm for generating smooth models from electromagnetic sounding data

TL;DR: In this article, the authors proposed a smoothest model which fits the data to within an expected tolerance for the inversion of both magnetotelluric and Schlumberger sounding field data.
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A Critical Review of Data on Field-Scale Dispersion in Aquifers

TL;DR: The authors found that field-scale dispersivities are several orders of magnitude greater than lab-scale values for the same material; it is generally agreed that this difference is a reflection of the influence of natural heterogeneities which produce irregular flow patterns at the field scale.
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