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The Carbon Sequestration Potential of Soils: Some Data from Northern Italian Regions

机译:土壤的碳固存潜力:意大利北部地区的一些数据

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It is well known that soil plays, within terrestrial ecosystems, an essential role in many biogeochemical cycles and in the regulation of greenhouse gas fluxes. Less known, and often underestimated, is the importance of carbon sequestration potentialof soil, especially trough humified carbon. Even within the agro-forestry practices of the Kyoto Protocol, most of the attention is devoted to the biomass carbon storage, rather than soil carbon sequestration. The highest potentialities for carbon sequestration are related to the arable lands, that accounts for the 11% of earth surface; the increase of 0.1% of organic carbon content in the 0-30 cm layer of cultivated soils, achievable with minor adjustment of agronomic practices, is equivalent to the sequestration of 5,000 millions t of carbon. On the other hand, the conversion of a grasslands into cultivated land determine, during 50-70 years, a release of 80-150 t CO_2 ha~(-1). Within this paper the estimate of soil organic carbon of three Northern Italian regions is presented.
机译:众所周知,土壤在陆地生态系统中起着许多生物地球化学循环和调节温室气体通量的重要作用。鲜为人知且经常被低估的是土壤中碳固存潜力的重要性,尤其是槽状腐殖质碳。即使在《京都议定书》的农林业实践中,大多数注意力都集中在生物量碳的储存上,而不是土壤碳的固存。固碳的最大潜力与耕地有关,占地表的11%。在0-30 cm的耕作土壤层中增加0.1%的有机碳含量(只需对农艺方法进行少量调整即可实现),相当于固存了50亿吨碳。另一方面,草地向耕地的转化决定了在50-70年内释放80-150 t CO_2 ha〜(-1)。本文介绍了意大利北部三个地区的土壤有机碳估算。

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