Soil water repellency (SWR) is a widespread natural phenomenon that results from a
complex interplay between the hydrosphere, lithosphere, biosphere, atmosphere, and …

The aim of this work is to investigate the topsoil thickness affected by burning under
contrasting soil moisture content (field capacity versus air-dried conditions). A mollic horizon …

Karst slopes have thin soil layers covering bedrock and feature multiple near-surface soil-
rock interfaces (SRIs), which can produce hydrological processes that differ from those of …

High variability in the literature is reported on the soil depth affected by forest fires because
many factors are involved. We study the fire-induced changes on properties related to soil …

Soil organic carbon and nutrient content are analysed at topsoil cm-scale in a Rendzic
Phaeozem from an Aleppo pine forest in semiarid Central Ebro Basin (NE-Spain). Soil depth …

The study of soil water repellency has received increasing attention by the scientific
community in recent years since it has been found to be a much more widespread property …

After a wildfire the soil is covered by ash. Ash properties depend on vegetation type, amount
of fuel and fire intensity. The ash layer controls the post-fire soil hydrologic response, but …

Understanding the effects of elevation and related factors (climate, vegetation) on the
physical and chemical soil properties can help to predict changes in response to future …

Soil water repellency (SWR) markers are defined as hydrophobic compounds in soil causing
SWR and are mainly derived from plants. Previous studies have shown the types and …

The post-fire debris flow (PFDF) is a commonly destructive hazard that may persist for
several years following the wildfires. Susceptibility mapping is an effective method for …