| Issue |
E3S Web Conf.
Volume 54, 2018
25th Salt Water Intrusion Meeting (SWIM 2018)
|
|
|---|---|---|
| Article Number | 00034 | |
| Number of page(s) | 3 | |
| DOI | https://doi.org/10.1051/e3sconf/20185400034 | |
| Published online | 17 September 2018 | |
Hydrogeological structures as burried valley along the Eastern Pomerania Polish coast of the Baltic Sea
Marine Branch of Polish Geological Institute NRI, 5 Kościerska str., 80-328 Gdańsk
One of the characteristic feature of geological structure of the southern Baltic coast is presence of deep structures in Pleistocene sediments. Meaning of deep aquifers is unmeasurably important for water economy. The water bearing structures are situated in substantial depth and are better isolated from the surface than the water of shallow aquifers. It has important meaning for natural protection of these waters. Water resource of the structure is substantially increase in case when in water drainage zone where regional and local water circulation are focused. Simultaneously hydrogeological parameters of Pleistocene strata in the frame of deep structure are considerably advantageous rather than parameters of deeper aquifers.
© The Authors, published by EDP Sciences, 2018
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0 (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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