Heat is a useful tracer for quantifying groundwater–surface water interaction, but analyzing
large amounts of raw thermal data has many challenges. We present a computer program …

Transient anomalous diffusion characterized by transition between diffusive states (ie, sub-
diffusion and normal-diffusion) is not uncommon in real-world geologic media, due to the …

Preferential flow in soils and similar permeable media refers to processes of faster than
average water movement through only a fraction of the pore space, thereby bypassing most …

Exudates and finer particles often coat the surface of biopores, increasing the mechanical
stability and altering the physicochemical properties (eg wettability or sorption) of the …

The detection of a nonequilibrium water flow and solute transport in structured soil at various
scales is essential for better understanding of these phenomena. This study focused on the …

The formation of baseflow and stormflow was examined in the 1.18 km2 part of the
headwater catchment Uhlířská, Jizera Mountains, Czech Republic, over the period 2007 …

This study focuses on the description of soil water dynamics at four sites with different land
cover types, namely beech forest, conifer forest, meadow and clipped grass. The analysis …

Soil water dynamics at an experimental hillslope site is studied by means of a one‐
dimensional dual‐continuum model. The model is based on Richards' equation for vertical …

Numerical experiments on vertical unsaturated flow using the Richards equation were
conducted to examine the physical basis of why storm runoff responses from mountainous …

Green roofs, as an element of the green infrastructure, contribute to the urban heat island
effect mitigation and the urban drainage outflow reduction. To achieve the desired functions …