At the watershed scale, soil moisture is the major control for rainfall–runoff response, especially where saturation excess runoff processes dominate. From the ecological point of …
Soil water uptake by plant roots results from the complex interplay between plant and soil which modulates and determines transport processes at a range of spatial and temporal …
Groundwater transport models that accurately describe spreading of nonreactive solutes in an aquifer can poorly predict concentrations of reactive solutes. The dispersive term in the …
M Bittelli - HortTechnology, 2011 - journals.ashs.org
Soil water content (SWC) is a soil property that plays a crucial role in a large variety of biophysical processes, such as seed germination, plant growth, and plant nutrition. SWC …
CY Wang, P Cheng - Advances in heat transfer, 1997 - Elsevier
Publisher Summary This chapter outlines several theoretical models currently prevailing for multiphase flow and heat transfer in porous media. In particular, a multiphase mixture model …
DA DiCarlo - Water Resources Research, 2004 - Wiley Online Library
Gravity‐driven fingers in uniform porous medium are known to have a distinctive nonmonotonic saturation profile, with saturated (or nearly so) tips and much less saturation …
MR Niemet, JS Selker - Advances in Water Resources, 2001 - Elsevier
Five physically based models for predicting liquid saturation from light transmission in 2D laboratory systems containing translucent porous media were developed and tested …
Soil water extraction by plant roots results from plant and soil transport processes interacting at different space and time scales. At the single root scale, local soil hydraulic status and …
When CO2 is injected into sedimentary basins, the fate of the buoyant CO2 will be determined by how it interacts with the underlying geologic heterogeneities. Here we …