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

Bibliographic Data

ID21648752
AuthorsSzumińska Danuta (0000-0001-7142-9080, Faculty of Geographical Sciences Kazimierz Wielki University Bydgoszcz Poland, corresponding author), Krystyna Kozioł (0000-0003-1678-3647, Faculty of Geographical Sciences Kazimierz Wielki University Bydgoszcz Poland), Sergey Chalov (0000-0002-6937-7020, Faculty of Geographical Sciences Kazimierz Wielki University Bydgoszcz Poland), Vasilii A Efimov (0000-0001-9231-4493, Faculty of Geography Lomonosov Moscow State University Moscow Russia), Vasilii Efimov (Lomonosov Moscow State University), Marcin Frankowski (0000-0001-6315-3758, Faculty of Chemistry Adam Mickiewicz University Poznań Poland), Sara Lehmann‐Konera (0000-0002-8318-0224, Faculty of Earth Science and Spatial Management Maria Curie‐Skłodowska University in Lublin Lublin Poland), Żaneta Polkowska (0000-0002-2730-0068, Faculty of Chemistry Gdańsk University of Technology Gdańsk Poland, corresponding author)
Year2023
Volume34
Issue17
Pages5591-5605
Publication date2023-11-01
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.4866
OpenAlexW4386914018
LanguageEN
Citations received3
References cited71

Permafrost regions are under particular pressure from climate change resulting in widespread landscape changes, which impact also freshwater chemistry. We investigated 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. Particular 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‐HCO 3 ‐Cl‐SO 4 ionic water type (with mineralisation in the range 600–800 mg L −1 ), 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 dissolved 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 L −1 Cu, 4610 μg L −1 Mn, and 687 μg L −1 Zn in the bottom water layers. Permafrost‐related waters were also enriched in dissolved phosphorus (up to 512 μg L −1 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

Aquatic ecosystem · Drainage basin · Geography · Permafrost · Thermokarst · Tributary · Arctic and Antarctic ice dynamics · Chemistry · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Environmental Chemistry · Geology · Oceanography

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Citations per year1.5
Citation span2024 - 2026 (3)
Highly citedNo

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