2022
DOI: 10.1029/2022wr032369
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A Thermodynamic Formulation of Water Potential in Soil

Abstract: Water potential (Pa) refers to the Gibbs free energy of water per unit volume relative to free water. In soil, water is not inert to soils but instead unfailingly interacts with them, giving rise to enormous complexities in understanding soil behavior. Such interaction between soil and water is conventionally quantified via the concept of soil water potential, which is defined as the free energy change per unit volume of water when moving from the free water state to the soil water state (Noy-Meir & Ginzburg, … Show more

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Cited by 16 publications
(5 citation statements)
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References 59 publications
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“…Both of them are often modified by water-salt transport, frost heave and thawing in the environmental system (Greco & Gargano, 2015;S. Hu et al, 2023;C. Zhang et al, 2022).…”
Section: Analysis Of Experimental Resultsmentioning
confidence: 99%
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“…Both of them are often modified by water-salt transport, frost heave and thawing in the environmental system (Greco & Gargano, 2015;S. Hu et al, 2023;C. Zhang et al, 2022).…”
Section: Analysis Of Experimental Resultsmentioning
confidence: 99%
“…Increasing concentration increases the osmotic potential, and at very high concentrations, the soil water potential is high even in a soil water environment with large pores (weak water holding capacity and low matric potential). Then, the change of matric potential has a relatively small effect on soil water potential (Greco & Gargano, 2015; S. Hu et al., 2023; C. Zhang et al., 2022).…”
Section: Resultsmentioning
confidence: 99%
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