C@Fe3O4选择性吸附CO2对H2净化效果的研究

Longlong Lei , Hang Yuan , Hongguang Zhu , Jie Ma , Fanghui Pan , Fulu Lu
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引用次数: 0

摘要

在全球努力应对气候变化的背景下,捕获和储存二氧化碳以及开发氢能已成为广泛认可的减少温室气体排放的有效方法。特别是,通过有机燃料的气化和重整制氢的过程需要从CO2中分离和纯化H2。虽然在这一研究领域提出了多种技术途径,但在这些不同的方法中不同程度地普遍存在分离效率低、能耗高、成本高等问题。这项研究是基于氧化铁(Fe3O4)和二氧化碳之间强相互作用的报告,以及氢气的磁排斥。本研究假设碳包覆磁铁矿(C@Fe3O4)是一种选择性吸附CO2的材料,能够有效分离H2和CO2。为了验证这一假设,本研究合成C@Fe3O4并进行等温吸附实验,确定H2和CO2的吸附曲线,并计算吸附选择性。结果表明,C@Fe3O4在环境条件下对CO2有较好的选择性。穿透实验进一步证实H2和CO2的分离比高达13.6。与不含Fe3O4核心的多孔碳材料的对比实验,以及C@Fe3O4的表征分析,验证了双重机制的作用:Fe3O4核心对CO2的强吸附和氢的磁排斥。碳涂层不会抑制Fe3O4对CO2的强吸附,但也提供了一个屏障,阻止H2和Fe3O4之间的直接接触,减轻任何可能导致磁衰减的潜在还原反应。此外,花瓣状碳包覆结构提高了材料的CO2体积吸附能力。虽然Fe3O4晶芯的高密度导致质量吸附能力不高,但独特的层状碳结构提高了比表面积。这种双重作用导致CO2的体积吸附容量为1.32 mmol/cm³,超过了大多数现有的多孔碳材料,并且CO2/H2的吸附比也超过了许多碳材料。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Research on the effect of selective adsorption of CO2 by C@Fe3O4 for H2 purification

Research on the effect of selective adsorption of CO2 by C@Fe3O4 for H2 purification
In the context of global efforts to address climate change, capturing and storing CO2, as well as developing hydrogen energy, have emerged as widely recognized effective methods for reducing greenhouse gas emissions. In particular, the process of hydrogen production through the gasification and reforming of organic fuels necessitates the separation and purification of H2 from CO2. Although various technological pathways have been proposed in this research field, issues such as low separation efficiency, high energy consumption, and high costs are prevalent to varying degrees across these different methods. This study is based on reports of the strong interaction between ferric oxide (Fe3O4) and CO2, as well as the magnetic exclusion of hydrogen gas. This study hypothesize carbon-coated magnetite (C@Fe3O4) as a material with selective adsorption of CO2, enabling efficient separation of H2 and CO2. To test this hypothesis, this study synthesized C@Fe3O4 and conducted isothermal adsorption tests to determine the adsorption curves for H2 and CO2, along with calculations for adsorption selectivity. The results indicated that C@Fe3O4 exhibited good selectivity for CO2 over H2 under ambient conditions. Penetration experiments further confirmed that the separation ratio for H2 and CO2 reached as high as 13.6. Comparative experiments with porous carbon materials lacking the Fe3O4 core, along with characterization analyses of C@Fe3O4, validated the dual mechanism at play: the strong adsorption of CO2 by the Fe3O4 core and the magnetic exclusion of hydrogen. The carbon coating did not inhibit the strong adsorption of CO2 by Fe3O4 but also provided a barrier that prevented direct contact between H2 and Fe3O4, mitigating any potential reduction reactions that could lead to magnetic decay. Moreover, the petal-like carbon-coated structure increased the volumetric CO2 adsorption capacity of the material. Although the high density of the Fe3O4 crystalline core resulted in modest mass adsorption capacity, the unique layered carbon structure enhanced the specific surface area. This dual effect led to a volumetric CO2 adsorption capacity of 1.32 mmol/cm³, surpassing that of most existing porous carbon materials, and the CO2/H2 adsorption ratio also exceeded that of many carbon materials.
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