首页> 外文期刊>Environmental Science & Technology >Swelling Phenomena of the Nonswelling Clay Induced by CO_2 and Water Cooperative Adsorption in Janus-Surface Micropores
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Swelling Phenomena of the Nonswelling Clay Induced by CO_2 and Water Cooperative Adsorption in Janus-Surface Micropores

机译:Janus-Surface微孔中CO_2和水合作用吸附引起的非溶胀粘土溶胀现象

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摘要

With the development of microscopy and sensor techniques, it becomes evident that nonswelling clays show swelling behavior under CO_2- water mixture environments at high pressures and temperatures. The examples include Illite, muscovite, and kaolinite-rich rock samples. Here, we investigated the underlying mechanisms of kaolinite swelling induced by CO_2 and water using molecular simulations and low-pressure gas adsorption experiments. The results suggest the cooperative adsorption behavior of CO_2 and water on contact with kaolinite micropores, which have distinct wettabilities on the two adjoining interlayer surfaces. Even if clay-bound water exists, CO_2 can enter the micropores to induce swelling. The measured micropore volume, simulated equilibrium stable interlayer distance with pure water, and that with CO_2-water mixture were used in the swelling estimation, which shows good agreement with our experiments. The CO_2 and water molecule distributions inside the interlayer micropores verify the importance of the wettabilities of the kaolinite surfaces in this cooperative adsorption behavior. The result extends the traditional understanding of the swelling mechanism, i.e., cation hydration and subsequent osmotic processes. In addition to earlier observations of kaolinite swelling behavior with potassium acetate, our study indicates the significance of the subtle balance of the noncovalent interactions between CO_2, water, and the kaolinite Janus surfaces.
机译:随着显微镜和传感器技术的发展,显而易见的是,在高压和高温下,非溶胀粘土在CO_2-水混合环境下表现出溶胀行为。例子包括伊利石,白云母和高岭石富集的岩石样品。在这里,我们使用分子模拟和低压气体吸附实验研究了CO_2和水引起的高岭石膨胀的潜在机理。结果表明,CO_2和水在与高岭石微孔接触时具有协同吸附性能,而高岭石微孔在两个相邻的夹层表面上具有明显的润湿性。即使存在黏土结合水,CO_2也会进入微孔以引起溶胀。测得的微孔体积,与纯水的模拟平衡稳定层间距离以及与CO_2-水混合物的模拟平衡稳定层间距离用于溶胀估算,与我们的实验吻合良好。层间微孔内部的CO_2和水分子分布证明了高岭石表面的润湿性在这种协同吸附行为中的重要性。结果扩展了对溶胀机理的传统理解,即阳离子水合和随后的渗透过程。除了早期观察到的醋酸钾对高岭石膨胀行为的影响外,我们的研究还表明了CO_2,水和高岭石Janus表面之间非共价相互作用的微妙平衡的重要性。

著录项

  • 来源
    《Environmental Science & Technology》 |2020年第9期|5767-5773|共7页
  • 作者单位

    Department of Systems Innovation The University of Tokyo Tokyo 113-8656 Japan;

    Fukada Geological Institute Tokyo 113-0021 Japan;

    Geological Carbon dioxide Storage Technology Research Association Kyoto 619-0292 Japan Research Institute of Innovative Technology for the Earth (RITE) Kyoto 619-0292 Japan;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-18 05:27:33

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