河北开滦矿区晚古生代煤对CO2 和CH4 气体吸附模型探讨
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本文为欧盟第六框架的计划课题和国家973课题(编号 2006CB202201)资助的成果。


Models of Pure CO2 and Pure CH4Adsorption on the Late Paleozoic Coals from the Kailuan Coalfield, Hebei, China
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    摘要:

    对河北开滦矿区不同变质程度的煤进行了纯CO2和纯CH4气体等温吸附实验,并用Langmuir模型、三参数BET模型和吸附势理论模型(DR,DA)对煤的吸附实验数据进行了拟合,检验了各模型的拟合程度。结果表明:中煤阶烟煤的马家沟矿9号煤(Ro, ran = 1.21%)对CH4和CO2吸附能力比低煤阶烟煤的林南仓矿11号煤(Ro, ran = 0.58%)的吸附能力大;在相同压力下,同一煤样对CO2的吸附能力明显大于对CH4的吸附能力。马家沟矿9号煤对CO2和CH4的等温吸附线具有典型的I型特征,各模型对其吸附行为拟合误差相差很小,可用Langmuir方程描述;林南仓矿煤等温吸附线较复杂,因用Langmuir描述误差较大,应优先选择误差较小的吸附势理论DA模型来描述其吸附行为。9号煤对CH4和11号煤对CO2和CH4的吸附均以单分子层吸附为主。

    Abstract:

    Isothermal adsorption experiments of pure CO2 and CH4 on different coals in rank (the No.11 Coal from the Linnancang Mine and the No.9 Coal from the Majiagou Mine) from the Kailuan Coalfield of Hebei Province, China, have been studied. Four different models (Langmuir, BET, DR, and DA) were used to fit the experimental data of CO2 and CH4 adsorption and their fitting degree were investigated. The results showed that the adsorption capacity of the Majiagou coal(Ro, ran=1.21%)is higher than that of the Linnancang coal (Ro, ran=0.58%). The adsorption capacity of CO2 is higher than that of CH4 on the same coal under the same pressure. The adsorption isotherms of pure CO2 and pure CH4 on the Majiagou coal can be classified as Type I and their fitting errors of curves are very weak; thus the experimental data can be presented using the Langmuir isotherm. However, the adsorption of Linnancang coal is more complicated, and can be presented using DA model because of its minimum error. Monolayer adsorption occurs during the adsorption of pure CO2 and pure CH4 on the No. 11 Coal and that of pure CH4 on the No. 9 Coal.

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代世峰,张贝贝,彭苏萍,张小东,CHOU Chenlin.2009.河北开滦矿区晚古生代煤对CO2 和CH4 气体吸附模型探讨[J].地质学报,83(5):731-737.
daishifeng,-,-,-,-.2009. Models of Pure CO2 and Pure CH4Adsorption on the Late Paleozoic Coals from the Kailuan Coalfield, Hebei, China[J]. Acta Geologica Sinica,83(5):731-737.

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  • 收稿日期:2008-10-12
  • 最后修改日期:2008-12-17
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