Comparison of hydrochemistry and organic compound transport in two non-glaciated high Arctic catchments with a permafrost regime (Bellsund Fjord, Spitsbergen)
Abstract
An increase in air temperature related to climate change results in the retreat of glaciers, the degradation of permafrost, and the expansion of glacier-free areas in the polar regions. All these processes lead to changes in the Arctic landscape. They influence the hydrochemistry of streams and rivers fed by glaciers and thawing permafrost. In this study, we examine eighty two water samples from two non-glaciated catchments with snow-permafrost regime: the Tyvjobekken Creek and the Reindeer Creek (NW Wedel-Jarlsberg Land, Spitsbergen). We cover hydrometeorological measurements, fluctuations of physicochemical parameters (pH, specific electrolytic conductivity (SEC)), and the presence of selected organic compounds (dissolved organic carbon (DOC), formaldehyde (HCHO), ∑phenols). The obtained levels of DOC (0.061-0.569 mgC L-1) and HCHO (
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- Accepted or Published Version
- DOI:
- Digital Object Identifier (open in new tab) 10.1016/j.scitotenv.2017.09.064
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- Category:
- Articles
- Type:
- artykuł w czasopiśmie wyróżnionym w JCR
- Published in:
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SCIENCE OF THE TOTAL ENVIRONMENT
no. 613-614,
pages 1037 - 1047,
ISSN: 0048-9697 - Language:
- English
- Publication year:
- 2018
- Bibliographic description:
- Lehmann-Konera S., Franczak ł., Kociuba w., Szumińska D., Chmiel S., Polkowska Ż.: Comparison of hydrochemistry and organic compound transport in two non-glaciated high Arctic catchments with a permafrost regime (Bellsund Fjord, Spitsbergen)// SCIENCE OF THE TOTAL ENVIRONMENT. -Vol. 613-614, (2018), s.1037-1047
- DOI:
- Digital Object Identifier (open in new tab) 10.1016/j.scitotenv.2017.09.064
- Verified by:
- Gdańsk University of Technology
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