碳储存过程中孔隙尺度盐沉淀的实验室研究综述

IF 5.5 0 ENERGY & FUELS
Yulin Zhang, Shanchao Liu, Kaiyue Ding, Jun Yao, Hai Sun, Yongfei Yang, Lei Zhang, Junjie Zhong
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引用次数: 0

摘要

在CO2封存过程中,含盐含水层中的盐沉淀显著降低了地层孔隙度和渗透率(分别达到40%和70%),最终影响了CO2的储存。本文综述了近年来研究孔隙尺度盐沉淀的实验进展,重点介绍了岩心驱油和微流体实验。我们概述了盐沉淀的阶段,并分析了两种晶体形式:块状晶体和多晶聚集体。描述了两种分布模式(局部分布模式和均匀分布模式)及其赋存条件,并讨论了岩石性质、流体特征、注气速率、CO2相和边界条件等关键影响因素。最后,我们评估了当前研究的局限性,并提出了未来的潜在方向。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Review on laboratory studies of pore-scale salt precipitation during carbon storage
Salt precipitation in saline aquifers during CO2 sequestration significantly reduces formation porosity and permeability (reaching 40 % and 70 %, respectively), ultimately influencing CO2 storage. This review explores recent experimental advances in understanding pore-scale salt precipitation, focusing on core-flooding and microfluidic experiments. We outlined the stages of salt precipitation and analyzed two crystalline forms: bulk crystals and polycrystalline aggregates. We also described two distribution patterns (local and homogeneous) and their occurrence conditions, and discussed key influencing factors including rock properties, fluid characteristics, gas injection rates, CO2 phases and boundary conditions. Finally, we assessed current research limitations and proposed potential directions for future.
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CiteScore
11.20
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