Numerical Modeling of Multiphysics Constitutive Relations Governing Water Migration into Variably Saturated Sorptive Shale

IF 4.3 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
Kaifu Mi, Yingying Xu*, Yu Lei, Juncheng Wang, Pengyu Shen and Xueming Zhang, 
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引用次数: 0

Abstract

The water invasion within shales easily causes damage to the hydrocarbon flow. However, the water imbibition mechanisms are still unclear, and the mathematical connection between stress-dependent permeability and water imbibition was rarely known. As a result, in this paper, a numerical simulation model coupled with water imbibition, shale deformation, and shale permeability alteration was established to analyze how water imbibition lead to an alteration in geomechanical properties and shale gas permeability. The results showed that the proposed model was validated with the high pressure imbibition experimental data of shale samples. Moreover, more comprehensive water imbibition mechanisms included in the model can improve the prediction accuracy for the water imbibition process. Furthermore, the water imbibition distance was demonstrated to be a power function of water imbibition duration and clay mineral content, an exponential expression of initial matrix permeability, and a positively linear equation of the injection pressure difference. Last but not least, the elastic modulus after hydration is negatively related to matrix permeability, clay mineral content, and injection pressure difference. These bigger control factors will result in clay swelling and cementation weakening during the water imbibition, finally enhancing stress sensitivity and decreasing permeability. Finally, the cores with a high clay mineral content and injection pressure difference are likely to enhance stress sensitivity, obeying the positive power function and linear function, respectively. The findings can provide a scientific basis to study the water-sensitive damage to flow capacity and stress sensitivity for unconventional formations in a water environment.

变饱和吸附页岩水运移多物理场本构关系数值模拟
页岩内部的水侵易对油气流动造成破坏。然而,储层的渗吸机理尚不清楚,应力相关渗透率与渗吸之间的数学关系也鲜为人知。因此,本文建立了含渗、页岩变形和渗透率蚀变的数值模拟模型,分析了含渗对页岩地质力学性质和渗透率的影响。结果表明,该模型与页岩样品的高压渗吸实验数据相吻合。此外,在模型中加入更全面的吸积机理可以提高对吸积过程的预测精度。此外,渗吸距离与渗吸持续时间和粘土矿物含量成幂函数关系,与初始基质渗透率呈指数关系,与注入压差成正线性关系。水化后的弹性模量与基质渗透率、粘土矿物含量、注入压差呈负相关。这些较大的控制因素将导致吸水性过程中粘土溶胀和胶结减弱,最终增强应力敏感性,降低渗透率。黏土矿物含量高、注入压差大的岩心应力敏感性增强,分别服从正幂函数和线性函数。研究结果可为研究水环境下非常规地层的水敏损伤及应力敏感性提供科学依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
ACS Omega
ACS Omega Chemical Engineering-General Chemical Engineering
CiteScore
6.60
自引率
4.90%
发文量
3945
审稿时长
2.4 months
期刊介绍: ACS Omega is an open-access global publication for scientific articles that describe new findings in chemistry and interfacing areas of science, without any perceived evaluation of immediate impact.
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