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多孔碳材料对二氧化碳、甲烷及其混合物的吸附:表面化学、含水量和孔隙无序的影响。

Adsorption of carbon dioxide, methane, and their mixtures in porous carbons: effect of surface chemistry, water content, and pore disorder.

机构信息

Service de Thermodynamique, Faculté Polytechnique, UMons, Université de Mons, Mons, Belgium.

出版信息

Langmuir. 2013 Mar 12;29(10):3328-38. doi: 10.1021/la3048938. Epub 2013 Feb 28.

Abstract

The adsorption of carbon dioxide, methane, and their mixtures in nanoporous carbons in the presence of water is studied using experiments and molecular simulations. Both the experimental and numerical samples contain polar groups that account for their partially hydrophilicity. For small amounts of adsorbed water, although the shape of the adsorption isotherms remain similar, both the molecular simulations and experiments show a slight decrease in the CO2 and CH4 adsorption amounts. For large amounts of adsorbed water, the experimental data suggest the formation of methane or carbon dioxide clathrates in agreement with previous work. In contrast, the molecular simulations do not account for the formation of such clathrates. Another important difference between the simulated and experimental data concerns the number of water molecules that desorb upon increasing the pressure of carbon dioxide and methane. Although the experimental data indicate that water remains adsorbed upon carbon dioxide and methane adsorption, the molecular simulations suggest that 40 to 75% of the initial amount of adsorbed water desorbs with carbon dioxide or methane pressure. Such discrepancies show that differences between the simulated and experimental samples are crucial to account for the rich phase behavior of confined water-gas systems. Our simulations for carbon dioxide-methane coadsorption in the presence of water suggest that the pore filling is not affected by the presence of water and that adsorbed solution theory can be applied for pressures as high as 15 MPa.

摘要

本文通过实验和分子模拟研究了水存在时纳米多孔碳对二氧化碳、甲烷及其混合物的吸附。实验和数值样品中均含有极性基团,这部分基团使它们具有一定的亲水性。对于少量吸附水,尽管吸附等温线的形状保持相似,但分子模拟和实验都表明 CO2 和 CH4 的吸附量略有下降。对于大量吸附水,实验数据表明甲烷或二氧化碳笼形化合物的形成与先前的工作一致。相比之下,分子模拟并未解释此类笼形化合物的形成。模拟数据与实验数据之间的另一个重要区别涉及在增加二氧化碳和甲烷压力时解吸的水分子数量。尽管实验数据表明在二氧化碳和甲烷吸附时水仍被吸附,但分子模拟表明,在二氧化碳或甲烷压力下,初始吸附水量的 40%至 75%会解吸。这些差异表明,模拟和实验样品之间的差异对于解释受限水-气体系的丰富相行为至关重要。我们在水存在的情况下对二氧化碳-甲烷共吸附的模拟表明,水的存在并不影响孔隙填充,并且吸附溶液理论可适用于高达 15 MPa 的压力。

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