压力转移定律在实验室中 水力压裂实验 压力转移定律
Renyi Qiu1, Guangqing Zhang2,3, Xuelin Zheng4
1College of Petroleum Engineering, China University of Petroleum-Beijing, Beijing, 102249, China.
Scientific reports
|July 27, 2024
概括
从样本表面到内部的压力转移需要时间,特别是在液压压裂过程中. 这项研究使用纤维格 (FBG) 来监测内部应力,揭示了加载时间和爬行如何影响岩石力学中的应力分布.
科学领域:
- 地质技术工程 地质技术工程
- 岩石机械学 岩石机械学
- 材料科学 材料科学 材料科学
背景情况:
- 真正的三轴液压压裂实验面临着面向内部压力转移的挑战,导致不准确的现场压力模拟.
- 了解应力传播对于准确的地下条件实验室建模至关重要.
研究的目的:
- 在真实三轴负荷时,从表面到样本内部的应力转移过程进行定量分析.
- 调查加载时间和爬行对应力再分配的影响.
- 为了验证一个修改后的3D汉堡模型来描述压力转移.
主要方法:
- 开发了一种使用纤维布拉格格 (FBG) 传感来监测内部压力的实验方法.
- 在一个类似混凝土的样本 (30厘米x30厘米x30厘米) 上进行了真正的三轴应力负荷实验.
- 修改了一个3D汉堡模型来模拟应力转移过程,并通过煤炭破碎实验验证了结果.
主要成果:
- 内部应力需要加载时间才能达到统一的状态.
- 增加的压缩应力减少了应力转移所需的时间.
- 爬行显著影响应力转移过程,导致微裂关闭和应力再分配.
结论:
- 该研究量化了岩石类材料中时间依赖的应力转移现象.
- 这些发现提供了关于水力压裂过程中压力再分配的爬行作用的见解.
- 这项研究为改善实验室模拟在现场压力条件的标准化提供了指导.
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