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监测油水界面纳米级碳酸钙的成核与生长

Monitoring the Nucleation and Growth of Nanoscale CaCO at the Oil-Water Interface.

作者信息

Zhu Yaguang, Wang Ying, Gao Zhenwei, Gupta Prashant, Singamaneni Srikanth, Zuo Xiaobing, Jun Young-Shin

机构信息

Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri 63130, United States.

Department of Mechanical Engineering and Materials Science, Washington University in St. Louis, St Louis, Missouri 63130, United States.

出版信息

ACS Nano. 2024 Oct 1;18(39):26522-26531. doi: 10.1021/acsnano.4c02490. Epub 2024 Sep 16.

Abstract

Interfaces can actively control the nucleation kinetics, orientations, and polymorphs of calcium carbonate (CaCO). Prior studies have revealed that CaCO formation can be affected by the interplay between chemical functional moieties on solid-liquid or air-liquid interfaces as well as CaCO's precursors and facets. Yet little is known about the roles of a liquid-liquid interface, specifically an oil-liquid interface, in directing CaCO mineralization which are common in natural and engineered systems. Here, by using X-ray scattering techniques to locate a meniscus formed between water and a representative oil, isooctane, we successfully monitored CaCO formation at the pliable isooctane-water interface and systematically investigated the pivotal roles of the interface in the formation of CaCO (i.e., particle size, its spatial distribution with respect to the interface, and its mineral phase). Different from bulk solution, ∼5 nm CaCO nanoparticles form at the isooctane-water interface. They stably exist for a long time (36 h), which can result from interface-stabilized dehydrated prenucleation clusters of CaCO. There is a clear tendency for enhanced amounts and faster crystallization of CaCO at locations closer to isooctane, which is attributed to a higher pH and an easier dehydration environment created by the interface and oil. Our study provides insights into CaCO nucleation at an oil-water interface, which can deepen our understanding of pliable interfaces interacting with CaCO and benefit mineral scaling control during energy-related subsurface operation.

摘要

界面能够积极控制碳酸钙(CaCO₃)的成核动力学、取向和多晶型。先前的研究表明,CaCO₃的形成会受到固液或气液界面上化学官能团与CaCO₃前驱体及晶面之间相互作用的影响。然而,关于液 - 液界面,特别是油 - 液界面在引导CaCO₃矿化过程中的作用却知之甚少,而这种界面在自然和工程系统中都很常见。在此,通过使用X射线散射技术来定位水与代表性油异辛烷之间形成的弯月面,我们成功监测了在柔韧的异辛烷 - 水界面处CaCO₃的形成,并系统地研究了该界面在CaCO₃形成过程中的关键作用(即粒径、其相对于界面的空间分布及其矿物相)。与本体溶液不同,约5纳米的CaCO₃纳米颗粒在异辛烷 - 水界面形成。它们能长时间稳定存在(36小时),这可能源于界面稳定的CaCO₃脱水预成核簇。在更靠近异辛烷的位置,CaCO₃的量有明显增加且结晶更快,这归因于界面和油所创造的更高pH值和更易脱水的环境。我们的研究为油 - 水界面处的CaCO₃成核提供了见解,这有助于加深我们对与CaCO₃相互作用的柔韧界面的理解,并有益于能源相关地下作业过程中的矿物结垢控制。

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