一个新的数值模拟框架,用于通过沉积,紧缩和交融来预测孔隙空间演变和岩石特性
Bowen Ling1,2, Xingming Du1, Shuheng Du1
1Institute of Mechanics, Chinese Academy of Sciences, Beijing, 100190, China.
Scientific reports
|May 17, 2025
概括
这项研究引入了一个数值模拟框架,以预测岩石孔隙空间在diagenesis过程中的演变. 该模型整合了矿物谷物的生成,沉积,压缩和地化学反应,提供了对孔隙性和透性变化的见解.
科学领域:
- 地质地质地质地质地质地
- 地质化学 地质化学
- 计算科学 计算科学
背景情况:
- 孔隙空间进化显著影响岩石的物理性质,由基因过程驱动.
- 目前的研究缺乏预测模型,以了解沉积物异质性如何影响交代和毛孔空间进化.
研究的目的:
- 开发和演示用于预测孔隙空间演变的数值模拟框架.
- 为了整合矿物谷物生成,沉积,压缩,流体流动,溶液运输,溶解和凝固.
主要方法:
- 用于3D矿物谷物生成的四重奏结构生成集 (QSGS).
- 采用离散元件方法 (DEM) 进行沉积和压缩.
- 应用有限体积法 (FVM) 用于流体流,地化学反应和物理属性计算.
主要成果:
- 对孔隙深度趋势和凝固的模拟结果与分析模型一致.
- 通过石英和多矿物系统的案例研究来证明框架能力.
- 验证了孔隙空间演变,孔隙性和透性的动态预测.
结论:
- 开发的数值框架对于动态预测岩石物理性质是强大的.
- 这种方法为了解对水库质量的基因影响提供了显著的潜力.
- 强调综合建模对于沉积盆地分析的重要性.
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