Surface Water Interaction Modelling Using Visual MODFLOW and GIS

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PHYLARESModel setup / ch.6__________________________________________________________________________________________37local scale of the model of this study, the base of layer 1 is HCOV 160, which is sand. The baseof layer 2 is HCOV 230 and the base of layer 3 is HCOV250. Below HCOV 250, there is a clayaquitard known as the Boom clay aquitard.Table 6. 3 Main units of the HCOV hydrogeological code (Cools.et.al, 2006)Table 6. 4 Overview of aquifers on the HCOV classification for Flanders (Solomon T. 2007)Aquifer code(HCOV)Aquifer name0100 Quaternary aquifer/sand/0220 Campine clay-sandcomplex0230 Pleistocene andPliocene aquifer /sand/Total Hydraulic conductivity(m/d)1-105-154-400240 Pliocene clay layer 0.04-0.20250 Miocene aquifer/sand/ 3-30______________________________________________________________________________________Groundwater – Surface water interaction modeling using visual MODFLOW and GIS
PHYLARESModel setup / ch.6__________________________________________________________________________________________386.1.7 Aquifer characteristics dataThe hydrogeologic layers of the model are bounded by clay aquitard at the bottom and recentalluvial deposits at the top. The steady state model requires the hydraulic conductivity of eachmodel layer.Figure 6. 5Stratigraphy of the different aquifer units of the model.______________________________________________________________________________________Groundwater – Surface water interaction modeling using visual MODFLOW and GIS
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Page 8 and 9: PHYLARESIntroduction / ch.1________
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Page 12 and 13: PHYLARESApproach and methodology /
Page 18 and 19: PHYLARESInteraction of Groundwater
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Page 60 and 61: PHYLARESResults and Discussion / ch
Page 70 and 71: PHYLARESConclusions and Recommendat
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Surface Water Interaction Modelling Using Visual MODFLOW and GIS

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