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Carbon sequestration and its potential in agricultural soils of China

机译:中国农业土壤中的固碳及其潜力

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Agricultural soils hold potential for the expansion of carbon sequestration. With this in mind, we investigated changes in the soil organic carbon (SOC) on the basis of an analysis of data sets extracted from 146 publications and further projected the SOC sequestration potential in China’s cropland. Our results suggest that a significant increase in the SOC occurred in east and north China, while a decrease appeared in northeast China. As a whole, the organic carbon density in the topsoil to 30 cm depth increased by 3.36 (2.54 to 4.26) Mg/ha between 1980 and 2000. Accordingly, the croplands in China that cover an area of over 130 Mha sequestered 437 (331 to 555) Tg C, with an average rate of 21.9 (16.6 to 27.8) Tg/yr, during this period. The potential of SOC sequestration in China was estimated to be 2–2.5 Pg C, which could be achieved by the 2050s if crop production and field management are improved.
机译:农业土壤具有扩大固碳的潜力。考虑到这一点,我们在对从146种出版物中提取的数据集进行分析的基础上,研究了土壤有机碳(SOC)的变化,并进一步预测了中国农田的SOC封存潜力。我们的结果表明,华东和华北的SOC显着增加,而东北则出现了下降。总体而言,在1980年至2000年之间,表层土壤至30厘米深处的有机碳密度以3.36(2.54至4.26)Mg / ha的速度增长。因此,覆盖面积超过130 Mha的中国农田隔离了437(331 555)Tg C,在此期间,平均速率为21.9 Tg / yr(每年16.6至27.8)。据估计,中国SOC隔离的潜力为2-2.5 Pg C,如果改善作物生产和田间管理,到2050年代可以实现。

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