Permeability is the dominant parameter in most hydrogeologic studies. There is abundant evidence for dynamic variations in permeability in time as well as space, and throughout the crust. Whether this dynamic behavior should be included in quantitative models depends on the problem at hand.
CITATION STYLE
Ingebritsen, S., & Gleeson, T. (2017). Perméabilité de la croûte. Hydrogeology Journal, 25(8), 2221–2224. https://doi.org/10.1007/s10040-017-1663-4
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