globalchange  > 过去全球变化的重建
DOI: 10.2172/1019211
报告号: PNNL-20493
报告题名:
Identification and Selection of Major Carbon Dioxide Stream Compositions
作者: Smith, F.; Phifer, M.
出版年: 2011
发表日期: 2011-06-30
国家: 美国
语种: 英语
英文关键词: Carbon Sequestration ; Impurities ; CO2 ; Carbon Dioxide
中文主题词: ; 二氧化碳
主题词: CARBON ; CARBON DIOXIDE
英文摘要: A critical component in the assessment of long-term risk from geologic sequestration of CO2 is the ability to predict mineralogical and geochemical changes within storage reservoirs due to rock-brine-CO2 reactions. Impurities and/or other constituents selected for co-sequestration can affect both the chemical and physical (e.g. density, viscosity, interfacial tension) behavior of CO2 in the deep subsurface. These impurities and concentrations are a function of both the industrial source(s) of the CO2, as well as the carbon capture technology used to extract the CO2 and produce a concentrated stream for geologic sequestration. This report summarizes the relative concentrations of CO2 and other constituents in exhaust gases from major non-energy related industrial sources of CO2. Assuming that carbon-capture technology would remove most of the incondensable gases N2, O2, and Ar, leaving SO2 and NOx as the main impurities, we selected four test fluid compositions for use in geochemical experiments. These included: 1) a pure CO2 stream representative of food grade CO2 used in most enhanced oil recovery projects: 2) a test fluid composition containing low concentrations (0.5 mole %) SO2 and NOx (representative of that generated from cement production), 3) a test fluid composition with higher concentrations (2.5 mole %) of SO2, and 4) and test fluid composition containing 3 mole % H2S.
URL: http://www.osti.gov/scitech/servlets/purl/1019211
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资源类型: 研究报告
标识符: http://119.78.100.158/handle/2HF3EXSE/40180
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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Recommended Citation:
Smith, F.,Phifer, M.. Identification and Selection of Major Carbon Dioxide Stream Compositions. 2011-01-01.
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