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Evaluation of Carbon Sequestration Potential in Cropland Soil of Lower reaches of Liaohe River Plain

机译:辽河平原下游农田土壤碳封存潜力评价

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Lower reaches of Liaohe River Plain is one of the areas where has a long history of planting in China, thus the enhancement of the capacity of soil carbon sequestration in cropland of this area has an important influence on global green house gases mitigation. Based on the 2nd National Soil Inventory data and the latest results from cropland productivity evaluation, the statistical model of soil carbon sequestration potential established by Qin et al.~[1] the soil organic carbon (SOC) sequestration potential was estimated and the differences of carbon sequestration ability between dry land and paddy field were compared according to the SOC spatio-temporal changes in cropland of Lower reaches of Liaohe River Plain over the last 30 years. The results show that the organic carbon density (SOCP) is 4.95 kg m~(-2) when the cropland soil organic carbon is saturated. The organic carbon storage in soil surface is 127.33 Tg in this area with an increase of 57.52 Tg. The organic carbon sequestration ability in paddy field is bigger than dry land in Lower reaches of Liaohe River Plain.
机译:辽河平原下游是中国种植悠久的领域之一,因此该地区农田土壤碳封存能力的增强对全球绿色房屋气体缓解了重要影响。基于第二次土壤库存数据和农田生产力评估的最新成果,QIN等人建立的土壤碳封存电位统计模型。〜[1]估计土壤有机碳(SOC)封存潜力和差异在过去的30年里,根据辽河平原陆下游的Soc时空变化进行了干陆和稻田之间的碳螯合能力。结果表明,当农田土壤有机碳饱和时,有机碳密度(SOCP)为4.95千克M〜(2)。土壤表面的有机碳储存在该区域中为127.33 Tg,增加57.52吨。稻田稻田的有机碳封存能力大于辽河平原下游的干陆。

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