Study on the Effect of Clay Minerals on CO2 Hydrate Formation

Yuze Han, Yu Feng, Yang Ge, Qingping Li, Lei Yang, Lunxiang Zhang, Yongchen Song
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Abstract

With the massive emission of greenhouse gases, global warming has become an important challenge for human beings at present. Storing carbon dioxide in the form of solid hydrates in the ocean is an effective strategy to mitigate climate warming. Clay in the ocean may have an effect on hydrate formation and CO2 storage. In this study, montmorillonite and kaolinite were selected as clay minerals, and the effects of clay particles on CO2 hydrate formation in suspensions with different mass fractions were experimentally analyzed. The results showed that the clay particles were able to promote hydrate nucleation and shorten the induction time, but the final amount of hydrate was reduced, which was related to the bound water. CO2 hydrate storage in clay minerals with different water contents was investigated. The amount of CO2 storage in montmorillonite minerals first decreased and then increased with the increase of water content, while the amount of storage in kaolinite minerals increased. The reason was that the amount of bound water on the surfaces of montmorillonite and kaolinite was different, and the stronger bound water was difficult to form hydrates. The results revealed the effect of clay particles on CO2 hydrate formation and provided some experimental support for the CO2 storage by hydrate method in the ocean.
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粘土矿物对二氧化碳水合物形成的影响研究
随着温室气体的大量排放,全球变暖已成为人类当前面临的重要挑战。在海洋中以固体水合物的形式储存二氧化碳是减缓气候变暖的有效策略。海洋中的粘土可能会对水合物的形成和二氧化碳的储存产生影响。本研究选取蒙脱石和高岭石作为粘土矿物,实验分析了不同质量分数的粘土颗粒对悬浮液中二氧化碳水合物形成的影响。结果表明,粘土颗粒能促进水合物成核并缩短诱导时间,但最终的水合物量减少,这与结合水有关。研究了不同含水量的粘土矿物中的 CO2 水合物储量。随着含水量的增加,蒙脱石矿物中的 CO2 储量先减少后增加,而高岭石矿物中的储量则增加了。原因是蒙脱石和高岭石表面的结合水量不同,结合水较强的矿物难以形成水合物。研究结果揭示了粘土颗粒对二氧化碳水合物形成的影响,为在海洋中通过水合物方法封存二氧化碳提供了一些实验支持。
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