Carbon sequestration related to soil physical and chemical properties in the high Arctic

0548009 - BC 2022 RIV US eng J - Článek v odborném periodiku
Jílková, Veronika - Devetter, Miloslav - Bryndová, Michala - Hájek, Tomáš - Kotas, P. - Luláková, P. - Meador, Travis Blake - Navrátilová, Dana - Saccone, P. - Macek, Petr
Carbon sequestration related to soil physical and chemical properties in the high Arctic.
Global Biogeochemical Cycles. Roč. 35, č. 9 (2021), č. článku e2020GB006877. ISSN 0886-6236. E-ISSN 1944-9224
Grant CEP: GA ČR(CZ) GA17-20839S; GA MŠMT(CZ) LM2015075; GA MŠMT(CZ) EF16_013/0001782
Institucionální podpora: RVO:60077344 ; RVO:67985939
Klíčová slova: glacier foreland * soil crust * tundra * bird cliff meadow * vegetation cover * mineral nutrients * aggregates * organic matter
Obor OECD: Environmental sciences (social aspects to be 5.7); Environmental sciences (social aspects to be 5.7) (BU-J)
Impakt faktor: 6.500, rok: 2021
Způsob publikování: Omezený přístup
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020GB006877

Arctic soils are an important reservoir of soil organic carbon (SOC) and their role in determining arctic ecosystem functioning in global carbon budgets requires closer attention. We investigated the coupling of soil properties and SOC stabilization mechanisms in high Arctic terrestrial habitats differing in vegetation cover and organic matter input. We focused on soil physical and chemical properties in glacier foreland, soil crust, dry tundra, wet tundra, and bird cliff meadow habitats on Svalbard (Norway). Concurrently, we performed physical fractionation to determine the amount of SOC stabilized by mineral associations or occlusion in macro and microaggregates. Initial stages of soil development (glacier foreland and soil crust habitats) exhibited characteristically high bulk density and pH, and low moisture and nutrient contents, whereas more developed soils (dry and wet tundra habitats) showed opposite trends. Contrastingly, bird cliff meadow showed low bulk density, intermediate moisture, and very high nutrient content. The amount of SOC stabilized by mineral associations and occlusion in aggregates generally increased with vegetation cover, hence, the more developed habitats supported higher contents of stabilized SOC. However, SOC was stabilized in aggregates even in initial stages of soil development. SOC content in most fractions correlated positively with contents of dissolved organic carbon and nitrogen, suggesting that both dissolved organic carbon and nitrogen might have provided some degree of SOC stabilization through increased formation of aggregates and suppression of microbial mineralization of soil organic matter, respectively. Our findings underscore the notion that models of SOC sequestration in the Arctic should account not only for total SOC content, but also SOC stabilization mechanisms, as represented by SOC content in respective soil fractions.
Trvalý link: http://hdl.handle.net/11104/0324835