肥料
固碳
碳纤维
环境科学
生物量(生态学)
土壤碳
氮气
碳汇
农学
土壤水分
化学
土壤科学
数学
生态学
生态系统
有机化学
算法
复合数
生物
作者
R. C. Izaurralde,W. B. McGill,Norman J. Rosenberg
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2000-05-05
卷期号:288 (5467): 809-809
被引量:48
标识
DOI:10.1126/science.288.5467.809c
摘要
When the addition of nitrogen (N) fertilizer leads to increased crop biomass, it also augments carbon (C) inputs to the soil and, hence, often increases soil organic matter. Consequently, the efficient use of fertilizer N to increase crop production has also been found valuable for sequestering atmospheric carbon in soil. William H. Schlesinger, however, in his Policy Forum "Carbon sequestration in soils" (Science's Compass, 25 June 1999, p. 2095) analyzes results from a 20-year experiment in Kentucky on conventional-till and no-till corn (1) and concludes that "the full carbon cost of N fertilizer…would effectively negate any net carbon sink as a result of the application of the fertilizer." These costs include the CO2-C emitted during fertilizer manufacture, storage, transport, and application. The three carbon cost factors (moles of CO2-C emitted per mole of N applied) documented by Schlesinger are 0.375 (stoichiometry of Haber-Bosch reaction), 0.58 (carbon cost of fertilizer manufacture) (2), and 1.436 (carbon cost of fertilizer manufacture, storage, transport, and application) (3, 4).
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