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渗流力对垂直井筒周围水力压裂起裂的时变效应

Time-Dependent Effect of Seepage Force on Initiation of Hydraulic Fracture around a Vertical Wellbore.

作者信息

Rim Hyonchol, Chen Youliang, Tokgo Jun, Du Xi, Li Yi, Wang Suran

机构信息

Department of Civil Engineering, School of Environment and Architecture, University of Shanghai for Science and Technology, Shanghai 200093, China.

College of Architecture and Urban Planning, Tongji University, Shanghai 200092, China.

出版信息

Materials (Basel). 2023 Feb 28;16(5):2012. doi: 10.3390/ma16052012.

Abstract

Fluid penetration into the rock during hydraulic fracturing has been an essential issue in studying the mechanism of fracture initiation, especially the seepage force caused by fluid penetration, which has an important effect on the fracture initiation mechanism around a wellbore. However, in previous studies, the effect of seepage force under unsteady seepage on the fracture initiation mechanism was not considered. In this study, a new seepage model that can predict the variations of pore pressure and seepage force with time around a vertical wellbore for hydraulic fracturing was established by using the method of separation of variables and the Bessel function theory. Then, based on the proposed seepage model, a new circumferential stress calculation model considering the time-dependent effect of seepage force was established. The accuracy and applicability of the seepage model and the mechanical model were verified by comparison with numerical, analytical and experimental results. The time-dependent effect of seepage force on fracture initiation under unsteady seepage was analyzed and discussed. The results show that when the wellbore pressure is constant, the circumferential stress induced by seepage force increases over time, and the possibility of fracture initiation also increases. The higher the hydraulic conductivity, the lower the fluid viscosity and the shorter the time required for tensile failure during hydraulic fracturing. In particular, when the tensile strength of rock is lower, the fracture initiation may occur within the rock mass rather than on the wellbore wall. This study is promising to provide a theoretical basis and practical guidance for further research on fracture initiation in the future.

摘要

水力压裂过程中流体渗入岩石一直是研究裂缝起裂机制的关键问题,特别是流体渗入引起的渗流力,它对井筒周围的裂缝起裂机制有重要影响。然而,在以往的研究中,未考虑非稳态渗流下渗流力对裂缝起裂机制的影响。本研究利用变量分离法和贝塞尔函数理论,建立了一种新的渗流模型,该模型能够预测水力压裂垂直井筒周围孔隙压力和渗流力随时间的变化。然后,基于所提出的渗流模型,建立了一种考虑渗流力时间效应的新的周向应力计算模型。通过与数值、解析和实验结果对比,验证了渗流模型和力学模型的准确性与适用性。分析和讨论了非稳态渗流下渗流力对裂缝起裂的时间效应。结果表明,当井筒压力恒定时,渗流力引起的周向应力随时间增加,裂缝起裂的可能性也增加。水力传导率越高、流体粘度越低,水力压裂过程中发生拉伸破坏所需的时间越短。特别是当岩石抗拉强度较低时,裂缝起裂可能发生在岩体内部而非井筒壁上。本研究有望为未来裂缝起裂的进一步研究提供理论依据和实践指导。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/062f/10004142/6ec13ffdf89a/materials-16-02012-g002.jpg

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