Publication date: May 2014
Source:Geoderma, Volumes 219–220
Author(s): Lukáš Jačka , Jirka Pavlásek , Václav Kuráž , Pavel Pech
Saturated hydraulic conductivity (Ks) is a key input parameter for modeling water flow in soils. Well-established methods exist, but there is no methodological standard or benchmark. This paper presents a comparison of three well-established measurement methods, which we used in the specific conditions of extremely heterogeneous mountain podzols. The following devices were applied to undisturbed soil core samples (diameter of 5.6
Source:Geoderma, Volumes 219–220
Author(s): Lukáš Jačka , Jirka Pavlásek , Václav Kuráž , Pavel Pech