Seasonal Dynamics of Ecosystem Carbon Exchange and Their Influencing Factors in Grasslands of Different Degrees of Salinization in Northern China. [PDF]
Pang G +5 more
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Inhibition by Nitrogen Addition of Moss-Mediated CH<sub>4</sub> Uptake and CO<sub>2</sub> Emission Under a Well-Drained Temperate Forest, Northeastern China. [PDF]
Xu X +6 more
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Freeze-thaw seasonal variations and environmental controls of CO<sub>2</sub> and CH<sub>4</sub> diffusive emissions from reservoirs in the upper Yellow River. [PDF]
Li C, Wu W, Chen H, Ren L, Kang X.
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Precipitation-Driven Soil and Vegetation Changes Shape Wetland Greenhouse Gas Emissions. [PDF]
Yang Z, Chen K, Zhao H, Zhang N, Qi D.
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Influence of nitrogen addition on soil respiration and soil properties in urban forests in Hefei city in China. [PDF]
Chen Y, Ruan H.
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Depth and Seasonality of Soil Respiration in <i>Caragana korshinskii</i> Plantation on the Loess Plateau. [PDF]
Sun Y, Chen Y.
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Divergent Trajectory of Soil Autotrophic and Heterotrophic Respiration upon Permafrost Thaw
Environmental Science & Technology, 2022Warming-induced permafrost thaw may stimulate soil respiration (Rs) and thus cause a positive feedback to climate warming. However, due to the limited in situ observations, it remains unclear about how Rs and its autotrophic (Ra) and heterotrophic (Rh) components change upon permafrost thaw. Here we monitored variations in Rs and its components along a
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Effects of drought and rainfall events on soil autotrophic respiration and heterotrophic respiration
Agriculture, Ecosystems & Environment, 2021Abstract The changes of surface vegetation cover, caused by the return of farmland to forest and grassland, can not only effectively control soil erosion, but also significantly increase soil organic carbon reserves. However, few studies are currently available on the control mechanism of soil CO2 emission after artificial vegetation restoration ...
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Globally rising soil heterotrophic respiration over recent decades
Nature, 2018Global soils store at least twice as much carbon as Earth's atmosphere1,2. The global soil-to-atmosphere (or total soil respiration, RS) carbon dioxide (CO2) flux is increasing3,4, but the degree to which climate change will stimulate carbon losses from soils as a result of heterotrophic respiration (RH) remains highly uncertain5-8.
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Estimates of soil heterotrophic respiration in global terrestrial ecosystems
2023Soil heterotrophic respiration (RH) is one of the largest and most uncertain components of terrestrial carbon cycle, which reflects the carbon loss from soils to the atmosphere due to microbial decomposition of soil organic carbon and litter debris. However, RH estimates vary greatly using different approaches, requiring RH estimates from different ...
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