Chemical composition of kettle holes as an indicator of salinity of small water bodies in northern Poland (the Parsęta catchment, the Borucinka drainage basin)

Kettle holes are commonly found in areas embraced by the last Pleistocene glaciations. They are a natural element of the landscape; together with their closed drainage basins they occupy a large proportion of the area. There are many natural conditions that determine their salinity, those listed mos...

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Veröffentlicht in:	GEOCHEMICAL JOURNAL 2020, Vol.54(2), pp.43-56
Hauptverfasser:	Cieśliński, Roman, Major, Maciej, Pietruszyński, Łukasz
Format:	Artikel
Sprache:	eng
Schlagworte:	chemical composition ions kettle holes salinity water cycle
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