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Environmental Earth Sciences

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01.07.2013 | Original Article

Effects of water table changes on soil CO₂, CH₄ and N₂O fluxes during the growing season in freshwater marsh of Northeast China

verfasst von: Cuicui Hou, Changchun Song, Yingchen Li, Jiaoyue Wang, Yanyu Song, Xianwei Wang

Erschienen in: Environmental Earth Sciences | Ausgabe 6/2013

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Abstract

A field control experiment was carried out to determine the influence of water table changes on soil CO₂, CH₄, and N₂O emissions in Calamagrostis angustifolia freshwater marsh in Northeast of China. The results showed that the water depth of 5 cm below the ground surface increased soil CO₂ emission, but there was no significant influence of deeper water table on gas emission. CH₄ emission was accelerated by deep standing water and approached the peak in the plant booming time. This suggests that root activity has influence on CH₄ production. The result also demonstrated that both low water table level and inundated environment would inhibit N₂O emission. Comparing the total global warming potential of three gases under different conditions, it can be concluded that maintaining a comparatively steady water table near the soil surface can benefit soil carbon sequestration in the C. angustifolia marsh, and decrease of the greenhouse gases emissions to the atmosphere.

Vorheriger Artikel Groundwater recharge dams in arid areas as tools for aquifer replenishment and mitigating seawater intrusion: example of AlKhod, Oman

Nächster Artikel Multivariate analysis of heavy metal pollution in street dusts of Xianyang city, NW China

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Titel: Effects of water table changes on soil CO2, CH4 and N2O fluxes during the growing season in freshwater marsh of Northeast China
verfasst von: Cuicui Hou
Changchun Song
Yingchen Li
Jiaoyue Wang
Yanyu Song
Xianwei Wang
Publikationsdatum: 01.07.2013
Verlag: Springer-Verlag
Erschienen in: Environmental Earth Sciences / Ausgabe 6/2013
Print ISSN: 1866-6280
Elektronische ISSN: 1866-6299
DOI: https://doi.org/10.1007/s12665-012-2031-2

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