一个准确的分析模型和应用方法,用于射流在异性质破裂岩石中
Yiwei Chen1,2, Pingchuan Dong3,4, Youheng Zhang1,2
1State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum (Beijing), Beijing, 102249, China.
Scientific reports
|May 20, 2025
概括
一个新的双裂纹模型准确地预测了由微裂纹中的流体流引起的地震波衰减和速度分散. 这种模型增强了对岩石特性和地震波行为的理解.
科学领域:
- 地质物理学 地质物理学
- 岩石物理 岩石物理
- 地震学 地震学
背景情况:
- 地震波速度分散和减弱受到岩石孔和微裂内的流体流动的显著影响.
- 了解孔尺度流体动力学对于解释地震数据和表征地下形成至关重要.
研究的目的:
- 开发一个简单的,准确的分析模型,用于地震减弱和分散,由微裂纹之间的喷流引起的,具有不同的面积比.
- 通过对数值模拟和实验数据进行模型验证,以改进岩石属性分析.
主要方法:
- 开发一个双裂喷流量模型,考虑裂互连性和面积比.
- 使用裂纹直径作为特征长度和1D流体压力扩散方程进行喷射路径分析.
- 模型的应用用于从实验压力数据中逆向确定微裂纹结构.
主要成果:
- 双裂纹模型的分析结果与数值模拟有很好的一致性.
- 该模型准确地预测了检查的岩石样本中的地震减弱和速度分散,与实验测量结果相匹配.
- 证明了对地震减弱和速度分散的定量和定性分析能力.
结论:
- 双裂分析模型为理解由孔尺度流体流动驱动的地震波现象提供了一个强大的工具.
- 该模型从地震数据中预测岩石属性的准确性得到了实验结果的验证.
- 这项研究推动了对岩石中地震减弱和速度分散的定量解释.
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