BEVLM_A0200_5 - Roerdalslenk deep, unsealed (from 2028)

In order to manage the groundwater, the Flemish subsoil is divided into several three-dimensional units: groundwater bodies. Within these groundwater bodies, environmental objectives are tested and, if necessary, measures are imposed. BEVLM_A0200_5 - Roerdalslenk deep, unsealed. Content: deposits of the Kempen Aquifer system A0200 lying under Kiezeloolite clay 1 A0233. The bodies of groundwater have both a name and a code. This code starts with an abbreviation of the Member State and the Region (BEVLM_A0200_2 = Belgium, Flanders), followed by the letter "S" or "M", indicating that a groundwater body is situated in the Scheldt or Meuse river basin district (BEVLM_A0200_2 = Meuse). The numerical code refers to the HCOVv2 code, which corresponds to the main aquifer (BEVLM_A0200_2 = Kempens Aquifer system). A sequential number at the end indicates the further spatial division of the groundwater bodies into that aquifer (BEVLM_A0200_2 = second groundwater body in the Meuse river basin district of which the Kempens Aquifer system is the most important aquifer).