EFFECTS OF AQUIFER ANISOTROPY ON THE MIGRATION OF INFILTRATED STREAM WATER TO A PUMPING WELL

Examples of hydraulic conductivity and anisotropy of alluvial aquifers. A 3D code is used to simulate the migration process. Discussion on pathlines, influence zone and travel times. Evaluation of rates of stream infiltration and produced stream water. Effects of baseflow, recharge and well placement are analysed.