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Changes in the soil organic carbon balance on China’s cropland during the last two decades of the 20th century

机译:20世纪后二十年中国农田土壤有机碳平衡的变化

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摘要

Agro-ecosystems play an important role in regulating global changes caused by greenhouse gas emissions. Restoration of soil organic carbon (SOC) in agricultural soils can not only improve soil quality but also influence climate change and agronomic productivity. With about half of its land area under agricultural use, China exhibits vast potential for carbon (C) sequestration that needs to be researched. Chinese cropland has experienced SOC change over the past century. The study of SOC dynamics under different bioclimatic conditions and cropping systems can help us to better understand this historical change, current status, the impacts of bioclimatic conditions on SOC and future trends. We used a simulation based on historical statistical data to analyze the C balance of Chinese croplands during the 1980s and 1990s, taking into account soil, climate and agricultural management. Nationwide, 77.6% of the national arable land is considered to be in good condition. Appropriate farm management practices should be adopted to improve the poor C balance of the remaining 22.4% of cropland to promote C sequestration.
机译:农业生态系统在调节由温室气体排放引起的全球变化中起着重要作用。恢复农业土壤中的土壤有机碳(SOC)不仅可以改善土壤质量,而且可以影响气候变化和农艺生产力。中国的土地面积约有一半用于农业用途,因此其碳封存潜力巨大,有待研究。在过去的一个世纪中,中国农田经历了SOC变化。对不同生物气候条件和种植系统下SOC的动态研究可以帮助我们更好地了解这一历史变化,现状,生物气候条件对SOC的影响以及未来趋势。我们使用基于历史统计数据的模拟,在考虑了土壤,气候和农业管理的情况下,分析了1980年代和1990年代中国农田的碳平衡。在全国范围内,有77.6%的国家耕地条件良好。应采取适当的农场管理措施来改善剩余22.4%耕地的贫C平衡,以促进C固存。

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