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Numerical simulation of surface and downhole deformation induced by hydraulic fracturing

机译:水力压裂引起的井面和井下变形数值模拟

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摘要

Tiltmeter mapping technology infers hydraulic fracture geometry by measuring fracture-induced rock deformation, which recorded by highly sensitive tiltmeters placed at the surface and in nearby observation wells. By referencing Okada's linear elastic theory and :4 Green's function method, we simulate and analyze the surface and downhole deformation caused by hydraulic fracturing using the homogeneous elastic half-space model and layered elastic model. Simulation results suggest that there is not much difference in the surface deformation patterns between the two models, but there is a significant difference in the downhole deformation patterns when hydraulic fracturing penetrates a stratum. In such cases, it is not suitable to assume uniform elastic half-space when calculating the downhole deformation. This work may improve the accuracy and reliability of the inversion results of tiltmeter monitoring data.
机译:倾角仪测绘技术通过测量裂缝引起的岩石变形来推断水力裂缝的几何形状,这些变形由放置在地表和附近观察井中的高灵敏度倾斜仪记录。借鉴冈田的线弹性理论和:4 Green的函数方法,利用均质弹性半空间模型和层状弹性模型,对水力压裂引起的地表和井下变形进行了模拟分析。仿真结果表明,两种模型的表面变形模式差异不大,但水力压裂穿透地层时井下变形模式存在显著差异。在这种情况下,在计算井下变形时不宜假设均匀的弹性半空间。这项工作可以提高倾斜仪监测数据反演结果的准确性和可靠性。

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