Variations of self-potential and unsaturated water flow with time in sandy loam and clay loam soils
Accurate assessment of soil–water fluxes is essential in soil physics due to its direct implications in environmental, agronomical or hydrological applications. Field estimations of soil–water fluxes by ‘classical’ hydraulic methods are often difficult to obtain. Moreover, water fluxes are highly va...
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Veröffentlicht in: | Journal of hydrology (Amsterdam) 2002-10, Vol.267 (3-4), p.173-185 |
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Sprache: | eng |
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