作者: Andreas Kallioras , Fotios Pliakas , Ioannis Diamantis
DOI: 10.1007/S11270-009-0291-6
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摘要: Groundwater flow models are applied to a large variety of hydrogeological conditions in different aquifer types, order simulate the groundwater investigated system. This paper aims present application model for simulation sedimentary aquifer, located Northern Greece. The involves period between April 2003 and 2004, is divided into two distinct stress periods, each containing time steps. found be satisfactory, conclusion which based on both graphical as well arithmetical verifications. was achieved by MODFLOW code.