通过直接可视化,量化粗壁断裂中不可混合的位移
Ping Wang1, Yong Huang1, Xiang Zhao1
1College of Earth Science and Engineering, Hohai University, Nanjing, 211100, China.
Journal of environmental management
|September 3, 2024
概括
断裂岩石中的地表液体迁移受到断裂几何和湿透性的影响. 这项研究可视化了流体的移位,揭示了可湿性.
科学领域:
- 地质科学 地质科学
- 水文地质学 水文地质学
- 石油工程是石油工程中的一个.
背景情况:
- 在断裂岩水层中,地下物质的迁移主要由断裂特征来决定.
- 了解裂中不混合的流体-流体移位对于地球物理过程和工程应用至关重要.
研究的目的:
- 在质量和数量上评估断裂几何学在粗断裂内的流体运动和分布中的作用.
- 调查湿度,粗度和注射速率对流体位移和残留和的影响.
主要方法:
- 利用断裂可视化系统观察粗断裂中的流体动力学.
- 对断裂表面粗度和孔径分布进行了定量分析.
- 采用图像处理来确定位移前端和残油分布的分数尺寸.
主要成果:
- 在成型样本中观察到较低的残留油和度 (6.45%-25.74%) 和更均的位移模式,这表明由于可湿性和微尺度粗性而提高了位移效率.
- 湿度对移位过程的影响大于异型粗度,这可以通过不同注射方向的残留油和率 (9.08%) 的较小变化来证明.
- 位移前端的分形维度最初在低注入率下增加,但在更高的注入率下降.
结论:
- 可视化的时间监测提供了对异性质粗度和断裂壁材料对流体和位移前线动态的影响的见解.
- 湿度在控制破裂系统中的流体移位效率方面,比异构粗度更为重要.
- 注射速率影响着位移前端的分形特征,突出了粗断裂中的复杂流动行为.
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