Reemission of inorganic pollution from permafrost? A freshwater hydrochemistry study in the lower Kolyma basin (North-East Siberia) - Publication - Bridge of Knowledge

Search

Reemission of inorganic pollution from permafrost? A freshwater hydrochemistry study in the lower Kolyma basin (North-East Siberia)

Abstract

Permafrost regions are under particular pressure from climate change resulting in widespread landscape changes, which impact also freshwater chemistry. We investi- gated a snapshot of hydrochemistry in various freshwater environments in the lower Kolyma river basin (North-East Siberia, continuous permafrost zone) to explore the mobility of metals, metalloids and non-metals resulting from permafrost thaw. Partic- ular attention was focused on heavy metals as contaminants potentially released from the secondary source in the permafrozen Yedoma complex. Permafrost creeks represented the Mg-Ca-Na-HCO3-Cl-SO 4 ionic water type (with mineralisation in the range 600–800 mg L1 ), while permafrost ice and thermokarst lake waters were the HCO 3-Ca-Mg type. Multiple heavy metals (As, Cu, Co, Mn and Ni) showed much higher dissolved phase concentrations in permafrost creeks and ice than in Kolyma and its tributaries, and only in the permafrost samples and one Kolyma tributary we have detected dissolved Ti. In thermokarst lakes, several metal and metalloid dis- solved concentrations increased with water depth (Fe, Mn, Ni and Zn – in both lakes; Al, Cu, K, Sb, Sr and Pb in either lake), reaching 1370 μg L1 Cu, 4610 μg L1 Mn, and 687 μg L1 Zn in the bottom water layers. Permafrost-related waters were also enriched in dissolved phosphorus (up to 512 μg L1 in Yedoma-fed creeks). The impact of permafrost thaw on river and lake water chemistry is a complex problem which needs to be considered both in the context of legacy permafrost shrinkage and the interference of the deepening active layer with newly deposited anthropogenic contaminants.

Citations

  • 2

    CrossRef

  • 0

    Web of Science

  • 2

    Scopus

Authors (7)

  • Photo of Dr Danuta Szumińska

    Danuta Szumińska Dr

    • Faculty of Geographical Sciences, Kazimierz Wielki University, Bydgoszcz, Poland
  • Photo of dr Kozioł Krystyna

    Kozioł Krystyna dr

    • Faculty of Geographical Sciences, Kazimierz Wielki University, Bydgoszcz, Poland
  • Photo of Prof. Sergey R. Chalov

    Sergey R. Chalov Prof.

    • Faculty of Geographical Sciences, Kazimierz Wielki University, Bydgoszcz, Poland
  • Photo of  Vasilii A. Efimov

    Vasilii A. Efimov

    • Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia
  • Photo of  Marcin Frankowski

    Marcin Frankowski

    • Faculty of Chemistry, Adam Mickiewicz University, Poznan, Poland
  • Photo of Dr Sara Lehmann-konera

    Sara Lehmann-konera Dr

    • Faculty of Earth Science and Spatial Management, Maria Curie-Skłodowska University in Lublin, Lublin, Poland

Cite as

Full text

full text is not available in portal

Keywords

Details

Category:
Articles
Type:
artykuły w czasopismach
Published in:
LAND DEGRADATION & DEVELOPMENT no. 34, pages 5591 - 5605,
ISSN: 1085-3278
Language:
English
Publication year:
2023
Bibliographic description:
Szumińska D., Krystyna K., Chalov S. R., Efimov V. A., Frankowski M., Lehmann-Konera S., Polkowska Ż.: Reemission of inorganic pollution from permafrost? A freshwater hydrochemistry study in the lower Kolyma basin (North-East Siberia)// LAND DEGRADATION & DEVELOPMENT -Vol. 34,iss. 17 (2023), s.5591-5605
DOI:
Digital Object Identifier (open in new tab) 10.1002/ldr.4866
Sources of funding:
  • INTERACT, H2020-EU.1.4.1.2. (PollAct, grant no. 730938) and by the Project Supporting Maintenance of Research Potential at Kazimierz Wielki University
Verified by:
Gdańsk University of Technology

seen 58 times

Recommended for you

Meta Tags