Thermodynamic Prediction of Expected Processes in the Dispersed System Flue Gas - Clinoptilolite in the Process of CO2 Capture

Rajden Skhvitaridze, Irakli Giorgadze, Nino Mukhadgverdeli, Vladimer Gordeladze, Nazibrola Kutsiava
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Abstract

CO2 generated in production processes and emitted into the atmosphere with flue gases is the cause of the greenhouse effect and negative processes of global climate change towards warming. Therefore, prevention of CO2 emissions into the atmosphere is the research topic of the article. CCUS type climate change mitigation projects are being developed in Georgia, where natural zeolite mineral containing clinoptilolite, Khekordzula tuff is a sorbent for CO2 capture. Its formation enthalpy (ΔfH0 298), Gibbs free energy (ΔfG0 298), and entropy (ΔfS 0 298) have not been studied, also temperatures of its thermal dehydration, CO2 adsorption, expected chemisorption and other thermodynamic quantities. It was determined: Enthalpy of clinoptilolite tuff formation (ΔfH0 298=-39826 kJ/mol), Gibbs free energy (ΔfG0 298=-36735 kJ/mol), entropy (ΔfS 0 298=-10.37 kJ/K-mol); Temperatures of dehydration (94.800C), CO2 capture using it (physical-96.5700C), start of chemo-sorption (95.2400C) and pressure corresponding to these temperatures (745, 636, 534) mm Hg. Tuff can be successfully used for CCUS from flue gases.
二氧化碳捕集过程中分散系统烟气-霞石预期过程的热力学预测
在生产过程中产生并随烟气排放到大气中的二氧化碳是造成温室效应和全球气候变化变暖的负面过程的原因。因此,防止二氧化碳排放到大气中是本文的研究课题。格鲁吉亚正在开发 CCUS 类型的气候变化减缓项目,其中含有鳞沸石的天然沸石矿物 Khekordzula 凝灰岩是捕获二氧化碳的吸附剂。对其形成焓(ΔfH0 298)、吉布斯自由能(ΔfG0 298)和熵(ΔfS 0 298)以及热脱水温度、二氧化碳吸附温度、预期化学吸附温度和其他热力学量尚未进行研究。研究结果如下霞石凝灰岩形成焓(ΔfH0 298=-39826 kJ/mol)、吉布斯自由能(ΔfG0 298=-36735 kJ/mol)、熵(ΔfS 0 298=-10.37 kJ/K-mol);脱水温度(94.800摄氏度)、利用其捕获二氧化碳的温度(物理温度-96.5700摄氏度)、开始化学吸附的温度(95.2400摄氏度)以及与这些温度相对应的压力(745、636、534)毫米汞柱。凝灰岩可成功用于烟道气中的 CCUS。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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