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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >The fluvial flux of particulate organic matter from the UK: the emission factor of soil erosion
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The fluvial flux of particulate organic matter from the UK: the emission factor of soil erosion

机译:来自英国的颗粒状有机物的通量:土壤侵蚀的排放因子

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Soil erosion has been identified as a potential global carbon sink since eroded organic matter is replaced at source and eroded material is readily buried. However, this argument has relied on poor estimates of the total fate of in-transit particulates and could erroneously imply soil erosion could be encouraged to generate carbon stores. These previous estimates have not considered that organic matter can also be released to the atmosphere as a range of greenhouse gases, not only carbon dioxide (CO2), but also the more powerful greenhouse gases methane (CH4) and nitrous oxide (N2O). As soil carbon lost by erosion is only replaced by uptake of CO2, this could represent a considerable imbalance in greenhouse gas warming potential, even if it is not significant in terms of overall carbon flux. This work therefore considers the flux of particulate organic matter through UK rivers with respect to both carbon fluxes and greenhouse gas emissions. The results show that, although emissions to the atmosphere are dominated by CO2, there are also considerable fluxes of CH4 and N2O. The results suggest that soil erosion is a net source of greenhouse gases with median emission factors of 5.5, 4.4 and 0.3 tonnes CO2eq/yr for one tonne of fluvial carbon, gross carbon erosion and gross soil erosion, respectively. This study concludes that gross soil erosion would therefore only be a net sink of both carbon and greenhouse gases if all the following criteria are met: the gross soil erosion rate were very low (<91 tonnes/km(2)/yr); the eroded carbon were completely replaced by new soil organic matter; and if less than half of the gross erosion made it into the stream network. By establishing the emission factor for soil erosion, it becomes possible to properly account for the benefits of good soil management in minimizing losses of greenhouse gases to the atmosphere as a by-product of soil erosion. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:水土流失已被确定为潜在的全球碳汇,因为从源头上替代了侵蚀的有机物,并且侵蚀的材料易于掩埋。但是,这种论据是基于对运输中颗粒物总命运的估计不充分的,并且可能错误地暗示土壤侵蚀可能被鼓励产生碳储量。这些先前的估算并未考虑有机物也可以作为一系列温室气体释放到大气中,不仅包括二氧化碳(CO2),而且还包括更强大的温室气体甲烷(CH4)和一氧化二氮(N2O)。由于侵蚀造成的土壤碳损失仅被吸收的二氧化碳所代替,因此即使在总碳通量方面并不重要,这也可能表示温室气体升温潜能的显着失衡。因此,这项工作考虑了通过英国河流的颗粒状有机物通量与碳通量和温室气体排放的关系。结果表明,尽管排放到大气中的气体主要是CO2,但还有大量的CH4和N2O通量。结果表明,土壤侵蚀是温室气体的净来源,一吨河流碳,总碳侵蚀和总土壤侵蚀的平均排放因子分别为5.5、4.4和0.3吨CO2当量/年。因此,这项研究得出的结论是,如果满足以下所有条件,则总土壤侵蚀将仅是碳和温室气体的净汇:总土壤侵蚀率非常低(<91吨/ km(2)/年);被侵蚀的碳完全被新的土壤有机质所替代;如果少于总侵蚀的一半进入河流网络。通过确定土壤侵蚀的排放因子,可以适当考虑良好土壤管理的好处,以最大程度减少作为土壤侵蚀副产物的温室气体向大气的损失。版权所有(c)2015 John Wiley&Sons,Ltd.

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