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A study on creep analytical solution and creep parameters of granite drilling in steady state under high temperature and high pressure

机译:高温高压花岗岩稳态钻探蠕变解析解及蠕变参数研究

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摘要

Rock creep is one of the important reasons for large deformation and instability while drilling, so the study on creep characteristics has great significance. However, it is difficult to determine creep parameters, and much harder when it is under high temperature and high pressure. Reasonable determination of the parameter is the key to make accurate calculations. Experiments show that drilling deformation of rock is part of deformation stage of steady state creep with the temperature below 500 degrees C and hydrostatic stress below 150 MPa. Generalised Kelvin model can be a very good reflection of its characteristics. In this paper, through the detailed deduction, the analytical solution of the drilling creep deformation is obtained. Based on the above analytic solution, the physical equation of creep parameters k(1), k(2) and eta in generalised Kelvin model vary as a function of temperature and stress is obtained through the inversion of experimental data of drilling deformation. The equation above has certain guiding significance on rock drilling construction with high temperature and stability prediction.
机译:岩石蠕变是钻进时大变形和不稳定性的重要原因之一,因此对蠕变特性的研究具有重要意义。但是,很难确定蠕变参数,而在高温高压下则要困难得多。合理确定参数是进行精确计算的关键。实验表明,岩石的变形是温度低于500摄氏度,静水压力低于150 MPa的稳态蠕变变形阶段的一部分。广义开尔文模型可以很好地反映其特征。本文通过详细推导,得出了钻井蠕变变形的解析解。基于以上解析解,通过对钻探变形实验数据进行反演,得到了广义开尔文模型中蠕变参数k(1),k(2)和η的物理方程随温度和应力的变化关系。上面的方程式对具有高温稳定性预测的凿岩施工具有一定的指导意义。

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