Hydraulic conductivity is the single most important hydraulic parameter for flow and transport‐
related phenomena in soil, but the results from different measuring methods vary under …

Vadose Zone Processes provides a unified, up-to-date treatment on the movement of water
through unsaturated media. In addition to covering the basic equations governing the flow …

Conventional Mediterranean vineyards from the Montes de Málaga (Axarquía region, Spain)
are characterized by high average temperatures, extreme rainfall events during autumn and …

Saturated hydraulic conductivity (Ksat) is an essential parameter for understanding soil
hydrology. This study evaluated the Ksat of in situ monoliths and intact cores and compared …

The saturated soil hydraulic conductivity (Ksat) is a key parameter in many hydrological and
climate models. Ksat values are primarily determined from basic soil properties and may …

To provide an improved methodology for characterizing the field‐saturated hydraulic
conductivity (Kfs) over broad areas with extreme spatial variability and ordinary limitations of …

The saturated hydraulic conductivity, Ks, is a soil property that has a key role in the
partitioning of rainfall into surface runoff and infiltration. The commonly used instruments and …

Saturated hydraulic conductivity is one of the key parameters in soil physics and
hydrological modeling. This study explores the use of Support Vector Machine (SVM) and a …

Saturated hydraulic conductivity (Ks) is one of the key parameters in the design of
engineering and environmental structures built in the unsaturated zone for infiltration …

Determination of the field‐saturated hydraulic conductivity (Kfs) can result in very high
variability due to soil heterogeneity, the measurement method, the number of replications …