Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.2172/1019211 |
报告编号 | PNNL-20493 |
来源ID | OSTI ID: 1019211 |
Identification and Selection of Major Carbon Dioxide Stream Compositions | |
Smith, F.; Phifer, M. | |
2011-06-30 | |
出版年 | 2011 |
语种 | 英语 |
国家 | 美国 |
领域 | 地球科学 |
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. |
英文关键词 | Carbon Sequestration Impurities CO2 Carbon Dioxide |
URL | 查看原文 |
来源平台 | US Department of Energy (DOE) |
引用统计 | |
文献类型 | 科技报告 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/5337 |
专题 | 地球科学 |
推荐引用方式 GB/T 7714 | Smith, F.,Phifer, M.. Identification and Selection of Major Carbon Dioxide Stream Compositions,2011. |
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