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  • A mathematical model of the hydrogeological system of the dune area of De Panne is presented, dealing with the saturated and unsaturated zones. The hydrochemistry of the aquifer has been investigated by chemical analyses and geoelectrical well
  • solids concentration in melt water to describe the seasonal variation of solute and its relation to discharge, in an attempt to use melt-water hydrochemistry as an indicator of the nature of subglacial processes within an Alpine glacier. Melt-water
  • hydrochemistry provides some insight into the nature of subglacial chemical processes, but, since melt waters do not appear to have access to all areas of the glacier bed, it probably underestimates total chemical activity.