Sens techniqueRisk of infiltration of pollutants from the surface, through the soil and unsaturated zone. The vulnerability of aquifers is intrinsic: it depends on the topographic (ground slope), pedological (permeability), geological context (permeability, thickness). A confined aquifer, covered by a low permeability formation (often clays) is not very vulnerable as compared to an unconfined aquifer.
according to BRGM
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