The redox limit shows the shift between oxidised and reduced conditions in the geological stratum and is based primarily on colour changes in sediments recorded during drilling. The redox limit is input to determine reduced accumulated clay thickness over magazines. The dataset contains polygons formed from points of redox change, possibly by interpolation. Data is made as points and polygons. Data have been collected since the beginning of groundwater mapping in 2000 and will be updated on a regular basis.
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