Groundwater from the Quaternary aquifer on the marine terrace in Gdańsk has been exploited for almost a century, supplying the town with water of good quality. However intensive exploitation in the past and development of the urban area influenced the chemical composition of the water. Hydrogeochemical background for such ions as chlorine, sulphate and ammonia has changed and also some organic micro compounds appeared in single wells.
Authors
Additional information
- Category
- Publikacja w czasopiśmie
- Type
- artykuł w czasopiśmie wyróżnionym w JCR
- Language
- angielski
- Publication year
- 2009
