大坝淤泥对二氧化碳的吸附机理

Fatima Ouadjenia, R. Marouf, J. Schott
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引用次数: 4

摘要

摘要本文采用体积法在295 K、15.59 ~ 750 mm Hg压力范围内研究了阿尔及利亚产睫毛膏(Mascara, Algeria)原料Chorfa粉土材料对二氧化碳的吸附性能,并用XRD、MEB和BET分析对吸附剂进行了表征。该材料以方解石和伊利石为主要成分。几个模型被用来描述实验等温线,如Langmuir, Freundlich, Hill De Boer和Sips。Sips模型对吸附等温线数据的拟合效果最好。所提出的实验吸附数据分析方法允许使用Dubinin-Raduskevich方程确定微孔体积(V0)和特征能(E)。得到的实验值V0 = 0.875 cm3/g,与用“t-plot”方法得到的V0 = 0.920 cm3/g非常吻合。特征能E = 20.9 kJ/mol,表明吸附为物理吸附。采用单孔扩散模型进行吸附动力学建模。CO2在淤泥中的扩散过程缓慢。热力学研究表明了吸附过程的自发性和可行性。
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Mechanism sorption of carbon dioxide onto dam silt
Abstract In this paper, a study of the adsorption of carbon dioxide onto raw Chorfa silt material (Mascara, Algeria) was experimentally investigated using volumetric technique at 295 K and at a pressure range from 15.59 to 750 mm Hg. XRD, MEB, and BET analysis were used to characterize the adsorbent. This material consisted of calcite and illite as main components. Several models were used to describe the experimental isotherm such as Langmuir, Freundlich, Hill De Boer, and Sips. The best fit of adsorption isotherm data is obtained with the Sips model. The proposed methodology for the analysis of the experimental adsorption data allows the determination of the micropore volume (V0) and the characteristic energy (E) using Dubinin–Raduskevich equation. An experimental value of V0 equal to 0.875 cm3/g is obtained in very good agreement with those found using the “t-plot” method, it is equal to 0.920 cm3/g. The characteristic energy E is equal to 20.9 kJ/mol, this value indicates that the adsorption is of physical type. The unipore diffusion model was selected for sorption kinetic modeling. The diffusion process of CO2 in the silt is slow. A thermodynamic study showed spontaneous nature and feasibility of the adsorption process.
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Cogent Chemistry
Cogent Chemistry CHEMISTRY, MULTIDISCIPLINARY-
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