基于修正DLVO理论的sio2 -卤水- co2体系润湿性研究及其在固碳过程中的应用

Bhautik Agrawal
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引用次数: 1

摘要

在不阻碍化石燃料工业发展的情况下减少碳足迹是当今备受关注和研究的主题。在多相岩石-流体系统中,润湿性特征在决定地下储层的可靠性方面起着重要作用,这些储层可以将二氧化碳保持在原位,从而实现碳地球封存应用。尽管近年来在认识诸如超临界条件下含CO2体系的润湿性信息和盐水- CO2膜界面上的zeta势等方面存在一些困难,但推断完整布置的润湿性是我们现有知识中的关键不确定性和空白。同样,人们需要处理润湿性和毛细压力的概念,以了解碳封存地层的适用性。本研究的重点是深盐水储层的碳固存。在这些地层的高压和高温条件下,CO2可以以超临界状态存在,因此具有类似液体的密度,从而可以有效地利用这些地层中的孔隙空间。在本研究中,基于改进的DLVO (Derjaguin, Landau, Verwey和Overbeek)理论的数学模型旨在通过利用基本原理来评估接触角,更好地了解超临界CO2体系的润湿性。在研究过程中对基本模型进行了修改,以适应超临界CO2的性质。该模型还可以将实验接触角测量作为输入,以预测目前不熟悉的关键属性值,因为它们具有挑战性,例如盐水- CO2界面上的zeta电位。该模型还可以通过评价已知条件下储层的润湿性来预测储层的固碳适宜性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Understanding Wettability of SiO2-Brine-CO2 System Using Modified DLVO Theory and its Applications in Carbon Geo-Sequestration Processes
The reduction of Carbon footprints without hindering the evolution of the fossil fuel industry is the subject of prominent attention and research these days. In multi-phase rock-fluid systems, the wettability characteristics play a substantial role in determining the trustworthiness of underground reservoir formations for holding CO2 in situ for Carbon Geo-sequestration applications. Despite several struggles over the modern years in recognizing the aspects such as the information on the wettability of systems comprising CO2 under supercritical conditions and the zeta potential over the brine- CO2 film interfaces, inferring the wettability of the complete arrangement are crucial uncertainties and voids in our existing knowledge. Again, one needs to deal with the concepts of wettability and capillary pressures to understand the suitability of a formation for carbon sequestration. This study focuses on the sequestration of carbon in deep saline brine reservoirs. Under the intense pressure and temperature situations in these formations, CO2 can exist in a supercritical state and thus have a liquid-like density, enabling efficient utilization of the pore spaces in those formations. In this research, a mathematical model based on the modified DLVO (Derjaguin, Landau, Verwey, and Overbeek) theory is designed to provide a better insight into the wettability of supercritical CO2 systems by utilizing fundamental principles to evaluate contact angles. The base model has been modified in the course of the study to accommodate for the properties of supercritical CO2. This model can also take up the experimental contact angle measurements as an input to anticipate values of critical properties that are presently unfamiliar, as they are challenging to analyze, such as the zeta potential on brine- CO2 interfaces. This model could also predict the suitability of geological reservoirs for carbon sequestration by evaluating the wettability under known conditions.
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