Decoupling of redox processes from soil saturation in Arctic tundra
Abstract Permafrost thaw in warming Arctic landscapes alters hydrology and saturation-driven biogeochemical processes.Models assume that aerobic respiration occurs in drained soils while saturated soils support methanogenesis; however, saturated soils 2 Piece Outdoor Sofa Sectional with Chair maintain redox gradients that host a range of anaerobic