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Nitrous Oxide Emissions to the Atmosphere from an Artificially Oxygenated Lake
Ist Teil von
Limnology and oceanography, 1996-05, Vol.41 (3), p.548-553
Ort / Verlag
Waco, TX: American Society of Limnology and Oceanography
Erscheinungsjahr
1996
Link zum Volltext
Quelle
Wiley-Blackwell Journals
Beschreibungen/Notizen
Nitrous oxide (N-2 O) production at the sediment surface of eutrophic Lake Baldegg was quantified with three independent methods: pore-water samplers, benthic chambers, and mass balances of the aerated-oxygenated hypolimnion. N2Oproduction at the sediment surface was the most important source in this lake and led to an accumulation in the hypolimnion during summer stratification. Highest rates of N2Oemission to the atmosphere (24 μ mol m-2 d-1) were observed after the onset of winter overturn, when hypolimnetic water enriched in N2Ocame in contact with the atmosphere. During summer stratification N2Oemissions to the atmosphere decreased to ∼ 4 μ mol m-2 d-1. The winter fluxes are close to the highest reported N2Oemissions from marine systems.