Effects of short-term drying and irrigation on $ CO_{2} $ and $ CH_{4} $ production and emission from mesocosms of a northern bog and an alpine fen
Abstract Atmospheric $ CO_{2} $ and $ CH_{4} $ exchange in peatlands is controlled by water table levels and soil moisture, but impacts of short periods of dryness and rainfall are poorly known. We conducted drying-rewetting experiments with mesocosms from an ombrotrophic northern bog and an alpine, minerotrophic fen. Efflux of $ CO_{2} $ and $ CH_{4} $ was measured using static chambers and turnover and diffusion rates were calculated from depth profiles of gas concentrations. Due to a much lower macroporosity in the fen compared to the bog peat, water table fluctuated more strongly when irrigation was stopped and resumed, about 11 cm in the fen and 5 cm in the bog peat. Small changes in air filled porosity caused $ CO_{2} $ and $ CH_{4} $ concentrations in the fen peat to be insensitive to changes in water table position. $ CO_{2} $ emission was by a factor of 5 higher in the fen than in the bog mesocosms and changed little with water table position in both peats. This was probably caused by the importance of the uppermost, permanently unsaturated zone for auto- and heterotrophic $ CO_{2} $ production, and a decoupling of air filled porosity from water table position. $ CH_{4} $ emission was <0.4 mmol $ m^{−2} $ $ day^{−1} $ in the bog peat, and up to >12.6 mmol $ m^{−2} $ $ day^{−1} $ in the fen peat, where it was lowered by water table fluctuations. $ CH_{4} $ production was limited to the saturated zone in the bog peat but proceeded in the capillary fringe of the fen peat. Water table drawdown partly led to inhibition of methanogenesis in the newly unsaturated zone, but $ CH_{4} $ production appeared to continue after irrigation without time-lag. The identified effects of irrigation on soil moisture and respiration highlight the importance of peat physical properties for respiratory dynamics; but the atmospheric carbon exchange was fairly insensitive to the small-scale fluctuations induced..
| Medienart: |
E-Artikel |
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| Erscheinungsjahr: |
2010 |
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| Erschienen: |
2010 |
| Enthalten in: |
Zur Gesamtaufnahme - volume:100 |
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| Enthalten in: |
Biogeochemistry - 100(2010), 1-3 vom: 16. Feb., Seite 89-103 |
| Sprache: |
Englisch |
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| Beteiligte Personen: |
Deppe, Marianna [VerfasserIn] |
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| Links: |
Volltext [lizenzpflichtig] |
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| Themen: |
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| Anmerkungen: |
© Springer Science+Business Media B.V. 2010 |
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| doi: |
10.1007/s10533-010-9406-9 |
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| funding: |
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| Förderinstitution / Projekttitel: |
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| PPN (Katalog-ID): |
OLC2111763632 |
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| 100 | 1 | |a Deppe, Marianna |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Effects of short-term drying and irrigation on $ CO_{2} $ and $ CH_{4} $ production and emission from mesocosms of a northern bog and an alpine fen |
| 264 | 1 | |c 2010 | |
| 336 | |a Text |b txt |2 rdacontent | ||
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| 500 | |a © Springer Science+Business Media B.V. 2010 | ||
| 520 | |a Abstract Atmospheric $ CO_{2} $ and $ CH_{4} $ exchange in peatlands is controlled by water table levels and soil moisture, but impacts of short periods of dryness and rainfall are poorly known. We conducted drying-rewetting experiments with mesocosms from an ombrotrophic northern bog and an alpine, minerotrophic fen. Efflux of $ CO_{2} $ and $ CH_{4} $ was measured using static chambers and turnover and diffusion rates were calculated from depth profiles of gas concentrations. Due to a much lower macroporosity in the fen compared to the bog peat, water table fluctuated more strongly when irrigation was stopped and resumed, about 11 cm in the fen and 5 cm in the bog peat. Small changes in air filled porosity caused $ CO_{2} $ and $ CH_{4} $ concentrations in the fen peat to be insensitive to changes in water table position. $ CO_{2} $ emission was by a factor of 5 higher in the fen than in the bog mesocosms and changed little with water table position in both peats. This was probably caused by the importance of the uppermost, permanently unsaturated zone for auto- and heterotrophic $ CO_{2} $ production, and a decoupling of air filled porosity from water table position. $ CH_{4} $ emission was <0.4 mmol $ m^{−2} $ $ day^{−1} $ in the bog peat, and up to >12.6 mmol $ m^{−2} $ $ day^{−1} $ in the fen peat, where it was lowered by water table fluctuations. $ CH_{4} $ production was limited to the saturated zone in the bog peat but proceeded in the capillary fringe of the fen peat. Water table drawdown partly led to inhibition of methanogenesis in the newly unsaturated zone, but $ CH_{4} $ production appeared to continue after irrigation without time-lag. The identified effects of irrigation on soil moisture and respiration highlight the importance of peat physical properties for respiratory dynamics; but the atmospheric carbon exchange was fairly insensitive to the small-scale fluctuations induced. | ||
| 650 | 4 | |a Fen | |
| 650 | 4 | |a Methane | |
| 650 | 4 | |a Peatland | |
| 650 | 4 | |a Water table | |
| 700 | 1 | |a Knorr, Klaus-H. |4 aut | |
| 700 | 1 | |a McKnight, Diane M. |4 aut | |
| 700 | 1 | |a Blodau, Christian |4 aut | |
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| 773 | 1 | 8 | |g volume:100 |g year:2010 |g number:1-3 |g day:16 |g month:02 |g pages:89-103 |
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| 952 | |d 100 |j 2010 |e 1-3 |b 16 |c 02 |h 89-103 | ||