|
|
|
George Kargas, Paraskevi A. Londra and Kyriaki Sotirakoglou
Saturated hydraulic conductivity (Ks) of soil, especially of the upper soil layer, is a basic parameter for modeling water infiltration and solute transport in the soil. In the present study, spatial and temporal variability of Ks in the upper soil layer...
ver más
|
|
|