碳酸盐岩的孔隙结构特征及其对透性的影响
Shenting Gang1,2,3,4, Tao Jia2,3, Yinger Deng1
1College of Environment and Civil Engineering, Chengdu University of Technology, Chengdu 610059, Sichuan, P. R. China.
ACS omega
|June 16, 2025
概括
碳酸盐岩中的异质孔隙结构,受沉积和二代生成的影响,显著影响了含水层的透性. 几何复杂性和不均性是控制流体流动的关键因素.
科学领域:
- 地质地质地质地质地质地
- 水文地质学 水文地质学
- 地质物理学 地质物理学
背景情况:
- 碳酸盐岩中的异质孔隙结构对于含水层的透性至关重要.
- 沉积环境和代遗传过程显著影响毛孔发育.
研究的目的:
- 分析碳酸盐岩石中孔隙,断层和溶解孔隙的空间特征.
- 为了确定有效的透性,并探索孔隙参数对流体流动的影响.
主要方法:
- 综合地质,水力动力学和碎形几何学的方法.
- 利用计算机断层扫描 (CT) 来进行核心样本的3D重建.
- 使用纳维埃-斯托克斯方程模拟流体流动.
主要成果:
- 总毛孔度在0.89%至10.35%之间,有效毛孔度在0.6%至6.12%之间.
- 孔隙形状,结构复杂性和尺寸被确定为影响透性的关键因素.
- 孔隙性与透性正相关;碎形维度显示出非线性关系.
结论:
- 孔隙的几何复杂性和结构不均性控制碳酸盐岩的透性.
- 较高的孔隙性和结构复杂性的增加导致更好的连接性和透性.
- 了解孔隙结构对于预测岩水层中的流体流动至关重要.
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