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露天采矿导致的陆地碳扰动增加了清洁煤的生命周期排放。

Terrestrial carbon disturbance from mountaintop mining increases lifecycle emissions for clean coal.

机构信息

Civil Engineering Department, University of Kentucky, Lexington, Kentucky 40506, USA.

出版信息

Environ Sci Technol. 2010 Mar 15;44(6):2144-9. doi: 10.1021/es903301j.

Abstract

The Southern Appalachian forest region of the U.S.--a region responsible for 23% of U.S. coal production--has 24 billion metric tons of high quality coal remaining of which mountaintop coal mining (MCM) will be the primary extraction method. Here we consider greenhouse gas emissions associated with MCM terrestrial disturbance in the life-cycle of coal energy production. We estimate disturbed forest carbon, including terrestrial soil and nonsoil carbon using published U.S. Environmental Protection Agency data of the forest floor removed and U.S. Department of Agriculture--Forest Service inventory data. We estimate the amount of previously buried geogenic organic carbon brought to the soil surface during MCM using published measurements of total organic carbon and carbon isotope data for reclaimed soils, soil organic matter and coal fragments. Contrary to conventional wisdom, the life-cycle emissions of coal production for MCM methods were found to be quite significant when considering the potential terrestrial source. Including terrestrial disturbance in coal life-cycle assessment indicates that indirect emissions are at least 7 and 70% of power plant emissions for conventional and CO(2) capture and sequestration power plants, respectively. To further constrain these estimates, we suggest that the fate of soil carbon and geogenic carbon at MCM sites be explored more widely.

摘要

美国南部阿巴拉契亚森林地区——负责美国 23%煤炭产量的地区——仍有 240 亿吨高质量煤炭,其中露天开采(MCM)将是主要的开采方法。在这里,我们考虑了与煤炭能源生产生命周期中 MCM 陆地干扰相关的温室气体排放。我们使用美国环境保护署公布的森林地表去除数据和美国农业部——林务局清查数据,估算了受干扰的森林碳,包括陆地土壤和非土壤碳。我们使用已公布的总有机碳测量值和再垦土壤、土壤有机质和煤块的碳同位素数据,估算了在 MCM 过程中被带到土壤表面的先前埋藏的地质有机碳的数量。与传统观点相反,当考虑到潜在的陆地来源时,发现 MCM 方法的煤炭生产生命周期排放非常显著。在煤炭生命周期评估中纳入陆地干扰表明,间接排放至少分别是常规和 CO2 捕获和封存电厂的电厂排放量的 7 倍和 70 倍。为了进一步限制这些估算,我们建议更广泛地探索 MCM 地点的土壤碳和地质碳的命运。

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