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National and sub-national assessments of soil organic carbon stocks and changes: The GEFSOC modelling system

机译:土壤有机碳储量及其变化的国家和地方评估:GEFSOC建模系统

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摘要

Soil organic carbon (SOC) plays a vital role in ecosystem function, determining soil fertility, water holding capacity and susceptibility to land degradation. In addition, SOC is related to atmospheric CO sub(2) levels with soils having the potential for C release or sequestration, depending on land use, land management and climate. The United Nations Convention on Climate Change and its Kyoto Protocol, and other United Nations Conventions to Combat Desertification and on Biodiversity all recognize the importance of SOC and point to the need for quantification of SOC stocks and changes. An understanding of SOC stocks and changes at the national and regional scale is necessary to further our understanding of the global C cycle, to assess the responses of terrestrial ecosystems to climate change and to aid policy makers in making land use/management decisions. Several studies have considered SOC stocks at the plot scale, but these are site specific and of limited value in making inferences about larger areas. Some studies have used empirical methods to estimate SOC stocks and changes at the regional scale, but such studies are limited in their ability to project future changes, and most have been carried out using temperate data sets. The computational method outlined by the Intergovernmental Panel on Climate Change (IPCC) has been used to estimate SOC stock changes at the regional scale in several studies, including a recent study considering five contrasting eco regions. This one step approach fails to account for the dynamic manner in which SOC changes are likely to occur following changes in land use and land management. A dynamic modelling approach allows estimates to be made in a manner that accounts for the underlying processes leading to SOC change. Ecosystem models, designed for site scale applications can be linked to spatial databases, giving spatially explicit results that allow geographic areas of change in SOC stocks to be identified. Some studies have used variations on this approach to estimate SOC stock changes at the sub-national and national scale for areas of the USA and Europe and at the watershed scale for areas of Mexico and Cuba. However, a need remained for a national and regional scale, spatially explicit system that is generically applicable and can be applied to as wide a range of soil types, climates and land uses as possible. The Global Environment Facility Soil Organic Carbon (GEFSOC) Modelling System was developed in response to this need. The GEFSOC system allows estimates of SOC stocks and changes to be made for diverse conditions, providing essential information for countries wishing to take part in an emerging C market, and bringing us closer to an understanding of the future role of soils in the global C cycle.
机译:土壤有机碳(SOC)在生态系统功能,决定土壤肥力,持水能力和土地退化敏感性方面起着至关重要的作用。此外,SOC与大气中的CO sub(2)水平有关,土壤具有释放或隔离C的潜力,具体取决于土地利用,土地管理和气候。 《联合国气候变化公约》及其《京都议定书》以及其他《联合国防治荒漠化和生物多样性公约》都认识到SOC的重要性,并指出需要量化SOC的存量和变化。必须了解国家和地区范围内的SOC数量和变化,以进一步了解全球碳循环,评估陆地生态系统对气候变化的反应,并帮助决策者做出土地使用/管理决策。多项研究已在地块规模上考虑了SOC储量,但这些储量是特定地点的,在推断较大区域时价值有限。一些研究已经使用经验方法来估计区域范围内的SOC储量和变化,但是此类研究预测未来变化的能力有限,并且大多数使用温度数据集来进行。政府间气候变化专门委员会(IPCC)概述的计算方法已用于多项研究中,以估计区域范围内的SOC储量变化,其中包括一项最近的研究,该研究考虑了五个对比鲜明的生态区域。这一一步的方法无法解决土地使用和土地管理变更后SOC可能发生动态变化的方式。动态建模方法允许以考虑导致SOC更改的基本过程的方式进行估计。专为站点规模应用而设计的生态系统模型可以链接到空间数据库,从而提供空间明确的结果,从而可以确定SOC存量变化的地理区域。一些研究使用这种方法的变化来估计美国和欧洲地区的国家以下和国家级的SOC存量变化,以及墨西哥和古巴地区的分水岭规模。但是,仍然需要一个普遍适用的国家和地区规模,空间明确的系统,并且可以应用于尽可能广泛的土壤类型,气候和土地利用。为响应这一需求,开发了全球环境设施土壤有机碳(GEFSOC)建模系统。 GEFSOC系统允许估算各种条件下的SOC储量和变化,为希望加入新兴C市场的国家提供必要的信息,并使我们更了解土壤在全球C循环中的未来作用。

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