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用于润湿性改变分子动力学研究的带正电方解石表面模型。

A positively charged calcite surface model for molecular dynamics studies of wettability alteration.

作者信息

Bai Shixun, Kubelka Jan, Piri Mohammad

机构信息

Center of Innovation for Flow through Porous Media, Department of Petroleum Engineering, University of Wyoming, Laramie, WY 82071, United States.

Center of Innovation for Flow through Porous Media, Department of Petroleum Engineering, University of Wyoming, Laramie, WY 82071, United States.

出版信息

J Colloid Interface Sci. 2020 Jun 1;569:128-139. doi: 10.1016/j.jcis.2020.02.037. Epub 2020 Feb 15.

DOI:10.1016/j.jcis.2020.02.037
PMID:32105900
Abstract

A new model for a positively charged calcite surface was developed to allow realistic molecular dynamics studies of wettability alteration on carbonate rocks. The surface charge was introduced in a manner consistent with the underlying calcite geochemistry and with the conclusions of recent quantum mechanical studies. The simulations using the new surface model demonstrate that the experimentally observed wettability behavior of calcite is represented correctly. In particular, the model surface became oil-wet due to the adsorption of the carboxylate species. Furthermore, the oil-wet conditions were reversed more effectively by a cationic surfactant than by an anionic one, in agreement with the majority of experimental observations. Finally, with simulated smart water, the well-documented wettability alteration abilities of Ca and SO could be explained by the formation of ion-pairs and competitive adsorption onto the surface, respectively. The simulation results with the new surface model conceptually agree with the electric double layer expansion being the predominant mechanism for the low salinity effect in oil recovery enhancement. The proposed calcite surface model will benefit future simulation studies on the wettability characteristics of carbonate rocks, and facilitate the design and optimizations of chemical agents and formulations to enhance the oil recovery from carbonate reservoirs.

摘要

开发了一种带正电荷方解石表面的新模型,以实现对碳酸盐岩润湿性改变的真实分子动力学研究。表面电荷的引入方式与潜在的方解石地球化学以及近期量子力学研究的结论一致。使用新表面模型的模拟表明,实验观察到的方解石润湿性行为得到了正确体现。特别是,由于羧酸盐物种的吸附,模型表面变成了油湿。此外,与大多数实验观察结果一致,阳离子表面活性剂比阴离子表面活性剂更有效地逆转了油湿条件。最后,对于模拟的智能水,Ca和SO众所周知的润湿性改变能力可分别通过离子对的形成和在表面的竞争性吸附来解释。新表面模型的模拟结果在概念上与双电层扩展是提高采收率中低盐度效应的主要机制相一致。所提出的方解石表面模型将有利于未来关于碳酸盐岩润湿性特征的模拟研究,并有助于设计和优化化学剂及配方,以提高碳酸盐岩油藏的采收率。

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