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Muhr, Jan ; Goldberg, Stefanie D. ; Borken, Werner ; Gebauer, Gerhard:
Repeated drying-rewetting cycles and their effects on the emission of CO2, N2O, NOx and CH4 in a forest soil.
In: Journal of Plant Nutrition and Soil Science.
Bd. 171
(2008)
Heft 5
.
- S. 719-728.
ISSN 1436-8730
DOI: https://doi.org/10.1002/jpln.200700302
Abstract
Prolonged summer droughts due to climate change are expected for this century, but little isknown about the effects of drying and wetting on biogenic trace-gas fluxes of forest soils. Here,the response of CO2, N2O, NO, and CH4 fluxes from temperate forest soils towards drying–wettingevents has been investigated, using undisturbed soil columns from a Norway spruce forestin the “Fichtelgebirge”, Germany. Two different types of soil columns have been used for thisstudy to quantify the contribution of organic and mineral horizons to the total fluxes: (1) organichorizons (O) and (2) organic and mineral soil horizons (O+M). Three drying–wetting treatmentswith different rewetting intensities (8, 20, and 50mm of irrigation d–1) have been compared to aconstantly moist control to estimate the influence of rainfall intensity under identical drying conditionsand constant temperature (+15°C). Drought significantly reduced CO2, N2O, and NO fluxesin most cycles. Following rewetting, CO2 fluxes quickly recovered back to control level in the Ocolumns but remained significantly reduced in the O+M columns with total CO2 fluxes from thedrying–wetting treatment ranging approx. 80% of control fluxes. Fluxes of N2O and NOremained significantly reduced in both O and O+M columns even after rewetting, with cumulativefluxes from drying–wetting treatments ranging between 20% and 90% of the control fluxes,depending on gas and cycle. Fluxes of CH4 were small in all treatments and seem to play no significantrole in this soil. No evidence for the release of additional gas fluxes due to drying–wettingwas found. The intensity of rewetting had no significant effect on the CO2, N2O, NO, and CH4fluxes, suggesting that the length of the drought period is more important for the emission ofthese gases. We can therefore not confirm earlier findings that fluxes of CO2, N2O, and NO duringwetting of dry soil exceed the fluxes of constantly moist soil.
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| Publikationsform: | Artikel in einer Zeitschrift |
|---|---|
| Begutachteter Beitrag: | Ja |
| Zusätzliche Informationen: | BAYCEER55051 |
| Institutionen der Universität: | Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften > Fachgruppe Geowissenschaften > Lehrstuhl Bodenökologie Forschungseinrichtungen > Forschungszentren > Bayreuther Zentrum für Ökologie und Umweltforschung - BayCEER Fakultäten Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften > Fachgruppe Geowissenschaften Forschungseinrichtungen Forschungseinrichtungen > Forschungszentren |
| Titel an der UBT entstanden: | Ja |
| Themengebiete aus DDC: | 500 Naturwissenschaften und Mathematik |
| Eingestellt am: | 11 Sep 2015 06:33 |
| Letzte Änderung: | 11 Sep 2015 06:33 |
| URI: | https://eref.uni-bayreuth.de/id/eprint/19104 |