低温流体热冲击对深层页岩中液压断裂传播的影响
Wuhao Guo1, Yintong Guo1, Mingyang Wu1
1State Key Laboratory of Geomechanics and Geotechnical Engineering Safety, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan 430071, Hubei, China.
ACS omega
|March 2, 2026
概括
深层页岩中裂变液的热冲击增强了裂变的传播和复杂性. 这项研究表明,刺激岩石面积和断裂复杂性增加,同时降低断裂压力,为能源储库开发提供了洞察力.
科学领域:
- 地质力学 地质力学
- 石油工程是石油工程中的一个.
- 材料科学 是一种材料科学.
背景情况:
- 由于高温和高压 (HTHP) 条件,深层页岩形成对水力压裂提出了挑战.
- 来自低温裂变流体的热冲击可以显著改变页岩的机械行为和裂变传播.
研究的目的:
- 研究热冲击下的深层页岩热裂的启动机制和传播行为.
- 分析热冲击对HTHP环境中的液压断裂特征的影响.
主要方法:
- 在HTHP条件下进行了液压压裂物理模拟实验.
- 使用凝聚区模型 (CZM) 的数值模拟来研究热冲击诱导的页岩裂变.
主要成果:
- 增加岩石温度 (25-200°C) 显著增强热冲击效应,增加刺激岩石面积 (SRA) 和断裂断层尺寸 (FD).
- 与25°C相比,200°C的分解压力下降了9.8%.
- 较高的热冲击率和多个周期增加了热裂的数量和长度,表明累积损伤.
结论:
- 热冲击在页岩断裂中起着至关重要的作用,影响断裂的开始和传播.
- 利用热冲击效应可以为深层能量储带来先进的液压压裂技术,可能降低断裂压力并提高断裂的复杂性.
- 这些发现为优化深层页岩中断裂过程提供了机械的见解.
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