Soil saturated hydraulic conductivity (Ks) is a key soil hydraulic property that determines the
hydrological cycle of check dam–dominated catchment areas. However, Ks data are lacking …

Soil hydraulic conductivity (K s) is a crucial soil physical property that not only influences soil
hydrological processes, but also the planning for vegetation recovery, irrigation practice and …

Soil hydraulic properties play an important role in modelingwater and solute movement
within the vadose zone of soils. Direct measurement of hydraulic parameters at a wide range …

Based on the sample data of agricultural soil profile, the locally-developed pedo-transfer
function (PTF) of agricultural soil saturated hydraulic conductivity (K s) in Daxing district was …

Study region Six typical regions of granite red soil in southern China. Study focus Regional
large-scale Ks analysis of granite red soil in South China is still limited to a large number of …

Abstract Purpose Pedotransfer functions (PTFs) have gained wide development in recent
years as approaches to establishing the relationship between easily measurable or readily …

Soil hydraulic parameters θ s, α, n, K s, L and θ r of the van Genuchten-Mualem model were
estimated using three pedotransfer functions (PTFs) based on soil properties for surface …

Pedo-transfer functions (PTFs) have been widely used to estimate soil hydraulic properties
in the simulation of catchment eco-hydrological processes. However, the accuracy of …

Hydraulic conductivity is an important soil physical property, especially for modeling water
flow and solute transport in soil, irrigation and drainage design, groundwater modeling and …

Soil hydraulic properties (SHPs) including the soil water retention curve and saturated soil
hydraulic conductivity (Ks) are crucial input data for simulations of soil water and solute …