Jedli Hedi, Briki Chaker, Chrouda Amani, Brahmi Jihed, Abassi Amel, Jbara Abdessalem, Slimi Khalifa, Jemni Abdelmajid
University of Monastir, National Engineering School of Monastir, Laboratory of Studies of Thermal Systems and Energy, LR99ES31 5019 Monastir Tunisia
Department of Chemistry, College of Science at Zulfi, Majmaah University Zulfi 11932 Saudi Arabia.
RSC Adv. 2019 Nov 25;9(66):38454-38463. doi: 10.1039/c9ra05904k.
The objective of this paper was to study CO adsorption on activated clay in the framework of geological storage. The activation of clay was characterized scanning electron microscopy, N adsorption-desorption isotherms, and X-ray diffraction. The adsorption isotherms were generated at different temperatures, namely, 298 K, 323 K, and 353 K. Based on the experimental result, a new model was simulated and interpreted using a multi-layer model with two interaction energies. The physicochemical parameters that described the CO adsorption process were determined by physical statistical formalism. The characteristic parameters of the CO adsorption isotherm such as the number of carbon dioxide molecules per site (), the receptor site densities (NM), and the energetic parameters were investigated. In addition, the thermodynamic functions that governed the adsorption process such as the internal energy, entropy, and Gibbs free energy were determined by a statistical physics model. Thus, the results showed that CO adsorption on activated clay was spontaneous and exothermic in nature.
本文的目的是在地质封存框架下研究一氧化碳在活性粘土上的吸附。通过扫描电子显微镜、氮气吸附-脱附等温线和X射线衍射对粘土的活化进行了表征。在不同温度下,即298K、323K和353K,生成了吸附等温线。基于实验结果,使用具有两种相互作用能的多层模型对新模型进行了模拟和解释。通过物理统计形式确定了描述一氧化碳吸附过程的物理化学参数。研究了一氧化碳吸附等温线的特征参数,如每个位点的二氧化碳分子数()、受体位点密度(NM)和能量参数。此外,通过统计物理模型确定了控制吸附过程的热力学函数,如内能、熵和吉布斯自由能。因此,结果表明一氧化碳在活性粘土上的吸附本质上是自发的且放热的。