The evolution of the coastal aquifer of Belgium
In the unconfined aquifer below the coastal area of Belgium salt water Occurs under a fresh-water layer at depths that vary from 2 to more than 25 m. Radiocarbon dating of groundwater samples set the seawater encroachment in the deep parts of the aquifer back at least in the Sub boreal period. A working hypothesis concerning the evolution of the aquifer is formulated.
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 1975 |
Schlagwörter: | ANE / Belgium / Belgian Coast / West-Vlaanderen (Province) |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-26579808 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://www.vliz.be/imisdocs/publications/329182.pdf |