| Issue |
E3S Web Conf.
Volume 54, 2018
25th Salt Water Intrusion Meeting (SWIM 2018)
|
|
|---|---|---|
| Article Number | 00016 | |
| Number of page(s) | 7 | |
| DOI | https://doi.org/10.1051/e3sconf/20185400016 | |
| Published online | 17 September 2018 | |
Groundwater chemistry and origin of the visutla delta plain
1
Nicolaus Copernicus University, Faculty of Earth Sciences, Toruń, Poland
2
Polish Polish Geological Institute NRI, Gdańsk, Poland
River estuaries are peculiar areas from the point of view of their groundwater origins, frequently connected with the diversification of groundwater chemistry. In the area of the Vistula delta in a number of places, the increased concentration of chloride and fluoride ions has occurred (Kozerski et al. 1987). These issues have already been considered in the studies of Kozerski (1981), Kozerski and Kwaterkiewicz (1984, 1988). The origin of salt and brackish water in the area of Żuławy was already the subject of scientific research in the 1930s (Schroeder 1931), and subsequently continued by Sadurski (1985, 1989), Burzyński and Sadurski (1989), Zuber at al. (1990, 2000) and Krawiec (2013).
© 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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