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- W2023777939 abstract "Abstract The effect of the water table on nitrous oxide (N 2 O) fluxes from peat profiles representing boreal peatlands of differing nutrient status was studied in the laboratory. Lowering of the water table in peat monoliths taken from two natural waterlogged peatlands for 14 weeks in a greenhouse at 20 °C increased the fluxes of N 2 O, an effect that was enhanced further by incubation in the dark. Raising of the water table in monoliths from two drained and forested peatlands caused cessation of the N 2 O fluxes from the drained peats, which had previously been sources of N 2 O. It is known that N 2 O fluxes have increased in peatlands drained several decades ago. The results suggest that it is not necessary for the water table to be lowered for several years to change a boreal peatland from a N 2 O sink to a source of the gas. In addition to the draining of peatlands, climate change can be expected to lower ground water levels during the summertime in the boreal zone, and this could cause marked changes in N 2 O fluxes from boreal peatlands by enhancing the microbial processes involved in nitrogen transformations." @default.
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- W2023777939 title "Short‐term effects of changing water table on N<sub>2</sub>O fluxes from peat monoliths from natural and drained boreal peatlands" @default.
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- W2023777939 doi "https://doi.org/10.1046/j.1365-2486.1999.00217.x" @default.
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