2019
DOI: 10.1007/s11356-019-06406-1
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Greenhouse gas emissions from intact riparian wetland soil columns continuously loaded with nitrate solution: a laboratory microcosm study

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Cited by 5 publications
(3 citation statements)
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“…Even at times of intermittent saturation after precipitation, low CH 4 production in the GRS riparian zone was likely due to biological oxidation of this GHG at the soil surface (Jacinthe et al., 2015). In the AGR field, soil cultivation and mineral fertilizer increased soil bulk density and soil NO 3 – –N (data on file) but lowered SOC content, and, when combined with tile drainage, an aerobic environment persisted (Mwagona et al., 2019).…”
Section: Discussionmentioning
confidence: 98%
“…Even at times of intermittent saturation after precipitation, low CH 4 production in the GRS riparian zone was likely due to biological oxidation of this GHG at the soil surface (Jacinthe et al., 2015). In the AGR field, soil cultivation and mineral fertilizer increased soil bulk density and soil NO 3 – –N (data on file) but lowered SOC content, and, when combined with tile drainage, an aerobic environment persisted (Mwagona et al., 2019).…”
Section: Discussionmentioning
confidence: 98%
“…These rapid increases in the main greenhouse gas (CO 2 and N 2 O) have been mainly attributed to land use changes, fossil fuel uses, and agricultural activities [ 4 ]. Although wetlands cover a small percentage of the land surface, they have a great influence on the dynamics and cycles of CO 2 and N 2 O in nature [ 5 , 6 ]. Therefore, strengthening research on CO 2 and N 2 O emissions in wetland ecosystems is of great significance for global climate change.…”
Section: Introductionmentioning
confidence: 99%
“…Studies that have been conducted on CO 2 and N 2 O fluxes from natural wetlands worldwide [ 5 , 7 , 8 ], including estuarine tidal marshes with varying salinity [ 6 ], temperate and tropical wetlands [ 9 ], and boreal and subarctic wetlands [ 10 ], indicate that CO 2 flux was higher during the warm growing season because of high temperatures and high aboveground biomass. The spatio-temporal CO 2 and N 2 O fluxes varied obviously within one wetland and among different wetlands [ 11 , 12 ].…”
Section: Introductionmentioning
confidence: 99%