Evaluation of Selected Geostatistical Methods for Interpolating Hydraulic Conductivity in Shallow Alluvial Aquifers Using Cross-Validation Statistics
Hydraulic conductivity (K) is essential for understanding groundwater movement in shallow alluvial aquifers. Upstream of the Siret–Moldova confluence, Romania, this parameter is poorly constrained, because available K values come from only 34 wells reported in existing hydrogeological documentation. This study provides...