Abstract
Fluxes of methane and nitrous oxide from a wetland were compared to hydrochemistry (NO −3 and SO 2−4 ) and soil enzyme activities (β-glucosidase) in an attempt to predict gas fluxes using chemical and enzymatic activities in north Wales, UK. In a one-year survey, the enzyme activities ranged from 0.028 to 0.065 μmol g−1 min−1, while NO −3 and SO 2−4 concentrations ranged between 0–0.78 and 5–200 mg L−1, respectively. Methane and nitrous oxide emissions varied between 0.32–240 and 0.28–5.48 mg m−1 da−1, respectively. The field survey was followed by laboratory-based manipulation experiments, from which pilot mathematical models were constructed, and related to the field data. The variation of methane emission was attributed to changes in SO 2−4 concentration and temperature at the site. In contrast, NO −3 concentration, water table height, and β-glucosidase activity were major controlling factors for nitrous oxide emission. The models explained more than 80% of the variation observed in the field study.
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Kang, H., Freeman, C., Lock, M.A. (1998). Trace Gas Emissions from a North Wales Fen — Role of Hydrochemistry and Soil Enzyme Activity. In: Wieder, R.K., Novák, M., Černý, J. (eds) Biogeochemical Investigations at Watershed, Landscape, and Regional Scales. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-0906-4_11
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DOI: https://doi.org/10.1007/978-94-017-0906-4_11
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