This review discusses the causes and consequences of 'non‐equilibrium'water flow and
solute transport in large structural pores or macropores (root and earthworm channels …

The soil hydraulic parameters for analyzing soil water movement can be determined by
fitting a soil water retention curve to a certain function, ie, a soil hydraulic model. For this …

This review discusses the causes and consequences of 'non‐equilibrium'water flow and
solute transport in large structural pores or macropores (root and earthworm channels …

Large‐scale application of biochar has been promoted as a strategy for improving soil
quality in agricultural and contaminated lands, as biochar has the potential to alter soil …

SWIM3 is the latest release in the family of SWIM (Soil Water Infiltration and Movement)
models that provides efficient solutions to the Richards and advection-dispersion equations …

Critical path analysis from percolation theory is used to calculate the unsaturated hydraulic
conductivity, K (S), of soils with pore space compatible with a (sometimes complex) fractal …

Numerical‐simulation models of water flow and solute transport in the vadose zone are
important tools in environmental research. The accuracy of predictions with these models …

Application of continuum percolation theory to a fractal pore space model yields results for
the constitutive relationships for unsaturated flow in agreement with experiment. This …

Measurements have been made of the effect of compaction on water retention, saturated
hydraulic conductivity, and porosity of two English soils: North Wyke (NW) grassland clay …

Characterising the unsaturated hydraulic conductivity of a green roof substrate is essential
for accurately modelling runoff detention in response to rainfall events. In this paper, the …