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Saturated hydrological conductivity.
Name Location Depth of the screen Geology* Hydrological Conductivity Lon.
We calculated the mean saturated hydrological conductivity for the representative soil profiles in order to account for drainage conditions and potential water logging problems.
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Hydrological conductivities for the six wells are relatively high (Table 2).
Regarding soil hydrological parameters, saturated conductivity (Ks) and residual soil water content (res) showed similar values.
Greater hydrological connectivity leads to lower conductivity levels and increased nutrient concentrations due to the shift of the dominating source to river water.
Results suggest the model is sensitive to the key hydrological parameter soil hydraulic conductivity.
This paper analyses the seasonal and land use induced variability of soil hydraulic and soil hydrological properties such as saturated hydraulic conductivity, unsaturated hydraulic conductivity, infiltration capacity, field capacity and bulk density of two typical Northern German soil types: Podzol and Stagnosol.
We also found that uncertainties originating from modeling approaches greatly depend on the types of hydrological structures and heterogeneity of hydraulic conductivity values in the domain assigned by modelers.
Finally, we demonstrate how this results in physical and hydrological changes to soil properties, including hydraulic conductivity, swelling capacity and wettability.
Water isotopes (δD, δ18O) as well as electrical conductivity were employed to clarify hydrological relationships among precipitation, stream water, and groundwater in the Douliou Hills (DLH) of Taiwan.
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