Colloids in Thermokarst Lakes along a Permafrost and Climate Gradient of Permafrost Peatlands in Western Siberia Using In Situ Dialysis Procedure

Thermokarst lakes in the Western Siberian Lowland (WSL) are major environmental factors controlling organic carbon and trace metal storage in inland waters and greenhouse gas emissions to the atmosphere. In contrast to previously published research devoted to lake hydrochemistry, hydrobiology, sedim...

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Bibliographic Details
Published in:Water (Basel) 2023-05, Vol.15 (9), p.1783
Main Authors: Manasypov, Rinat M., Lim, Artem G., Kriсkov, Ivan V., Raudina, Tatiana V., Kurashev, Danil G., Shirokova, Liudmila S., Pokrovsky, Oleg S.
Format: Article
Language:English
Subjects:
Abrasion
Air pollution
Alkaline earth metals
Alkalis
Bioavailability
Carbon
Cations
Chemical elements
climate
Climate change
Colloids
Dialysis
Dissolved organic carbon
Emissions
Environmental factors
filtration
Fractionation
Global warming
Greenhouse effect
Greenhouse gases
Hemodialysis
Hydrobiology
hydrochemistry
Hydrology
ice
Inland waters
Lake sediments
Lakes
Manganese
Metals
Micronutrients
Organic carbon
Peat
Peat-bogs
Peatlands
Permafrost
Pore water
Rare earth elements
Sediments
Siberia
silicates
solutes
surface area
Taiga & tundra
Thawing
Toxicants
Trace elements
Trace metals
water
watersheds
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Description
Summary:Thermokarst lakes in the Western Siberian Lowland (WSL) are major environmental factors controlling organic carbon and trace metal storage in inland waters and greenhouse gas emissions to the atmosphere. In contrast to previously published research devoted to lake hydrochemistry, hydrobiology, sedimentary carbon, and processes controlling the lake total dissolved (
ISSN:2073-4441
2073-4441
DOI:10.3390/w15091783