首页> 外文期刊>Cahiers Agricultures >Gaz a effet de serre et stockage du carbone par les sols: inventaire au niveau du BresilGreenhouse gas fluxes and carbon storage from soil: The Brazilian inventory
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Gaz a effet de serre et stockage du carbone par les sols: inventaire au niveau du BresilGreenhouse gas fluxes and carbon storage from soil: The Brazilian inventory

机译:土壤温室气体通量和碳储量:巴西清单

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Rising levels of atmospheric CO2 have focused attention on potential CO2 emissions from terrestrial ecosystems of the world, notably from soils and biomass. The world's mineral soils represent a large reservoir of C of about 1500 Pg C. Under the United Nations Framework Convention on Climate Change (UNFCCC) each country is required to develop, update and publish a national inventories of anthropogenic emissions (implementation of the National Communications), as well as to compile the inventories by comparable methodologies. For the last point, guidelines were developed and published as IPCC Guidelines for National Greenhouse Gas Inventories. Also, the land use, land-use changes and forestry (LULUCF) sector should he included in the national inventories. The CO2 fluxes from soils are discussed in chapter 5 for agricultural soils under the category 5D: CO2 emissions and removals from soils. These emissions are calculated from three subcategories : i) net changes in C storage in mineral soils ii) emissions from organic soils; and iii) emissions from liming of agricultural soils. In a first step the soil organic carbon stocks up to a depth of 30 cm were estimated for Brazil based on a map of different soil-vegetation associations combined with results from a soil database. The soil-vegetation associations map was derived by intersecting soil and vegetation maps. The original soil and vegetation classification were reduced to 6 soil and 15 vegetation categories. Because this data represents sites with native vegetation in the absence of significant disturbances, it constitutes a valuable baseline for evaluating the effect of land-use change on soil C stocks for Brazil. Overall, about 36 400 million tons of carbon Would be stored in the 0-30 cm soil layer under native conditions. The Brazilian Amazon region would account for 22,000 million tons. The CO2 emission from mineral soils 0 following following land-cover change in Brazil for the period 1975-1995 was estimated by Bernoux et al. who showed that the annual fluxes for Brazil indicate a net emission of CO2 to the atmosphere of 46.4 million tons of CO2 for the period 1975-1995. Intermediary calculation used to derive these annual fluxes estimated that 34 400 million tons of carbon were stored in the Brazilian soil for the year 1995. The annual CO2 emission for Brazil from liming varied from 4.9 to 9.4 million tons of CO2 per year with a mean annual CO2 emission of about 7.2 million tons. The South, Southeast and Center region accounted for a least 92% of total emission. Finally it could be calculated that the total CO, fluxes from soils reached around 51.9 million tons of CO2 per year for the period 1975-1995.
机译:大气中二氧化碳水平的上升已经将注意力集中在世界陆地生态系统潜在的二氧化碳排放上,特别是土壤和生物质。世界上的矿质土壤蕴藏着大约1500 Pg C的大量C。根据《联合国气候变化框架公约》(UNFCCC),每个国家都必须制定,更新和发布国家人为排放量清单(实施《国家信息通报》 ),并通过可比的方法编制清单。最后一点是,制定了指南并将其发布为《 IPCC国家温室气体清单指南》。此外,土地使用,土地使用变化和林业(LULUCF)部门应列入国家清单。在第5章中,针对农业土壤的土壤CO2通量在5D类别下进行了讨论:土壤中的CO2排放和清除。这些排放量是根据以下三个子类别计算的:i)矿物土壤中C储量的净变化ii)有机土壤的排放量; iii)农业土壤的石灰排放。第一步,根据不同的土壤-植被关联图以及土壤数据库的结果,估计巴西最深30厘米的土壤有机碳储量。土壤-植被关联图是通过将土壤和植被图相交而得出的。原始的土壤和植被类别减少为6种土壤和15种植被类别。由于该数据表示没有明显干扰的本地植被地点,因此它是评估巴西土地利用变化对土壤碳库的影响的宝贵基准。总体而言,在自然条件下,0-30厘米的土壤层中将储存约364亿吨碳。巴西亚马逊地区将占220亿吨。 Bernoux等人估计1975-1995年巴西土地覆被变化后,矿物土壤中的CO2排放量为0。他的研究表明,巴西的年通量表明1975-1995年期间向大气中排放的CO2净排放量为4,640万吨。用于得出这些年通量的中间计算方法估计,到1995年,巴西土壤中存储了344亿吨碳。石灰每年给巴西造成的二氧化碳排放量从4.9到940万吨不等,平均每年二氧化碳排放量约720万吨。南部,东南部和中部地区至少占总排放量的92%。最终可以计算出,在1975-1995年期间,土壤中的总CO通量每年达到约5190万吨CO2。

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