对于具有粗裂纹的吸水泥石接泥的水特性研究
Zhe Chen1,2, Yue-Jin Zhou1,2, Lei-Ming Zhang1,2
1State Key Laboratory of Intelligent Construction and Healthy Operation and Maintenance of Deep Underground Engineering, China University of Mining and Technology, Xuzhou 221116, China.
Materials (Basel, Switzerland)
|February 24, 2024
概括
这项研究揭示了泥石裂的粗程度如何影响泥流动. 较低的粗度会导致初始的水损失,而较高的粗度会导致由于吸水和沉积而导致泥堵塞.
科学领域:
- 地质技术工程 地质技术工程
- 材料科学 是一种材料科学.
- 断裂力学 断裂力学 断裂力学
背景情况:
- 了解泥石裂的特征对于有效的接至关重要.
- 分形理论和计算机断层扫描 (CT扫描) 为裂分析提供了先进的方法.
研究的目的:
- 为了研究不同粗度的吸水泥石裂中的泥泥的透特性.
- 分析裂几何和泥石特性对接性能的影响.
主要方法:
- 计算机断层扫描 (CT扫描) 和碎形理论被用来获得泥石裂的几何参数.
- 用3D打印技术和巴顿标准曲线来创建裂通道的物理模型.
- 模仿泥石吸水的类似材料被开发用于接模拟测试.
主要成果:
- 泥在低粗度裂中经历了显著的水损失,随着时间的推移,水损失有所减少.
- 高粗度裂表现出水的吸收和沉积,导致泥堵塞和阻碍流动.
结论:
- 泥石裂的粗度是一个影响泥 infiltration和有效性的关键因素.
- 该研究提供了对复杂地质构造中的泥行为的见解,有助于改进接设计.
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