Vadose Water
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Estimation of groundwater recharge from groundwater level fluctuations and baseflow rates around Mount Meru, Tanzania
2024, Groundwater for Sustainable DevelopmentPrediction of numerical homogenization using deep learning for the Richards equation
2023, Journal of Computational and Applied MathematicsCitation Excerpt :Unsaturated flow happens in soils when soil water travels downward, the topsoil dries out due to evaporation, or water permeates the soil surface across many soils’ pores [1,2].
Section Introduction: Groundwater sciences in Limnology
2022, Encyclopedia of Inland Waters, Second EditionThe Vadose Zone—A Semi-Aquatic Ecosystem
2022, Encyclopedia of Inland Waters, Second EditionHydraulic properties of unsaturated calcarenites by means of a new integrated approach
2021, Journal of HydrologyCitation Excerpt :The flow of water through unsaturated geologic media is, in fact, strongly conditioned by matric suction, which corresponds to a negative pressure potential, and by hydraulic conductivity, which is a nonlinear function of matric suction or water content. Although over the last 70 years a number of techniques have been used to determine the soil water retention curve (SWRC) for different geologic media, their limited applicability, poor practicality and high cost, along with the significant temporal/spatial variabilities in the hydraulic properties, suggest applying parametric empirical equations to best fit experimental data (Nimmo, 2009). The most widely used empirical equations are those by Brooks and Corey (1964), Campbell (1974), and van Genuchten (1980).