Methane and Nitrous Oxide Fluxes with Different Land Uses in the Temperate Meadow Steppe of Inner Mongolia, China
2022
Kaikai Fan | Yuchun Yan | Dawei Xu | Shuzhen Li | Yue Zhao | Xu Wang | Xiaoping Xin
Background and aims: Grazing and mowing are widely adopted management practices for the semiarid steppe in China that profoundly affect the greenhouse gas (GHG) flux in grassland ecosystems. However, the general mechanisms for CH<sub>4</sub> and N<sub>2</sub>O fluxes in response to grazing and mowing remain poorly understood. Thus, we conducted year-round flux measurements of CH<sub>4</sub> and N<sub>2</sub>O fluxes to investigate the effect of grazing and mowing on CH<sub>4</sub> and N<sub>2</sub>O fluxes. Methods: Using manual static chamber and gas chromatography, we measured the fluxes of CH<sub>4</sub> and N<sub>2</sub>O from grazing-exclusion, grazing and mowing sites from June 2019 to June 2020 in the Hulunbuir Grassland, Inner Mongolia. Results: Grazing and mowing increased soil temperature and reduced soil water content and soil inorganic N content. Compared with grazing and mowing, lower mean CH<sub>4</sub> uptake (−67.58 ± 8.9 μg m<sup>−2</sup> h<sup>−1</sup>) and higher mean N<sub>2</sub>O emissions (29.17 ± 6.8 μg m<sup>−2</sup> h<sup>−1</sup>) were found at the grazing-exclusion site. No pulse emissions of N<sub>2</sub>O were found for all sites during the spring thaw period (STP), and only two small N<sub>2</sub>O emission peaks due to soil thawing were captured on April 2nd and 5th. The contribution of the spring thaw to the total annual N<sub>2</sub>O budget was small and accounted for only 10%, 13% and 12% of the annual fluxes at the grazing-exclusion, grazing and mowing sites, respectively. Conclusion: Our results indicate that grazing and mowing enhance CH<sub>4</sub> uptake and inhibit N<sub>2</sub>O emissions, primarily due to the increased soil temperature and reduced soil water content and soil inorganic N content. No apparent pulse N<sub>2</sub>O emissions were observed at any of the three sites during the STP in the Hulunbuir grassland.
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