Drivers of soil nitrogen availability and carbon exchange processes in a High Arctic wetland

• Published in: Arctic science 2024-03, Vol.10 (1), p.22-33
• Main Authors: Hung, Jacqueline K.Y., Scott, Neal A., Treitz, Paul M.
• Format: Article
• Language: English
• Subjects: Abiotic factors; Ammonium; Ammonium compounds; Atmosphere; Availability; Biogeochemistry; Carbon cycle; Carbon dioxide; Climate change; Climate prediction; Climate system; Climatic conditions; ecosystem respiration; Ecosystems; Environmental conditions; Environmental control; Feedback; gross ecosystem productivity; High Arctic wetland; Influence; Mineralization; Negative feedback; net ecosystem exchange; Nitrates; Nitrogen; nitrogen availability; Nutrient availability; Nutrient cycles; Permafrost; Productivity; Respiration; Sampling; Seasons; Soil; Soil layers; Soil moisture; Soil nutrients; Soil temperature; Temperature; Vegetation; Watersheds; Wetlands
• ISSN: 2368-7460; 2368-7460
• DOI: 10.1139/as-2022-0048

Increased soil nutrient availability, and associated increases in vegetation productivity, could create a negative feedback between Arctic ecosystems and the climate system, thereby reducing the contribution of Arctic ecosystems to future climate change. To predict whether this feedback will develop, it is important to understand the environmental controls over nutrient cycling in High Arctic ecosystems and their impact on carbon cycling processes. Here, we examined the environmental controls over soil nitrogen availability in a High Arctic wet sedge meadow and how abiotic factors and soil nitrogen influenced carbon dioxide exchange processes. The importance of environmental variables was consistent over the 3 years, but the magnitudes of their effect varied depending on climate conditions. Ammonium availability was higher in warmer years and wetter conditions, while drier areas within the wetland had higher nitrate availability. Carbon uptake was driven by soil moisture, active layer depth, and variability between sampling sites and years ( R 2  = 0.753), while ecosystem respiration was influenced by nitrogen availability, soil temperature, active layer depth, and sampling year ( R 2  = 0.848). Considered together, the future carbon dioxide source or sink potential of high latitude wetlands will largely depend on climate-induced changes in moisture and subsequent impacts on nutrient availability.