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Formulation and implementation of a constitutive model for soft rock.

机译:软岩本构模型的制定与实现。

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摘要

Petroleum reservoirs located in the Norwegian sector of the North Sea have undergone unexpected subsidence of great magnitude (> 10 m) during more than 30 years of petroleum recovery operations. Historical laboratory investigations have shown that the subsidence is due to the mechanical behavior and mechanical properties of chalk. Chalk behavior is characterized by elastoplasticity, including pore collapse, shear failure, and tensile failure mechanisms; rate-dependence; and pore fluid dependence. The research described in this dissertation was performed with the objectives to formulate a constitutive model which describes all aspects of chalk and soft rock mechanical behavior, develop and/or implement methods to integrate the equations which form the constitutive model, and to apply the model to finite element simulations of engineering problems encountered in chalk and soft rock.; A new rate-dependent constitutive model is developed based on a three-dimensional extension of a volumetric time-lines model, similar to that of Bjerrum (1967). Shear and tensile failure surfaces are also included to reflect these failure mechanisms observed in chalk. Twelve model parameters are required to fully describe chalk behavior. Procedures to determine values for each of these parameters from laboratory test results are described. Correlations of model parameter values with index parameters are given for North Sea chalks, to allow reasonable values to be obtained in the absence of an extensive laboratory testing program. Comparisons between observed behavior and model simulations indicate that the new model is able to reproduce and predict the behavior of chalk quite well.; A new integration method for critical state cap plasticity models is presented. This new method may be used for rate-independent or rate-dependent constitutive models which are formulated with elliptical cap yield surfaces, including the chalk model. The new method gives results that compare favorably to integration methods used currently, in terms of accuracy and computational effort.; The effects of pore fluid composition on chalk behavior are included in the constitutive model. It is shown that the variability in constitutive behavior with pore fluid composition is due to dependence of model parameter values on pore fluid composition. This variability in model parameters with pore fluid composition has been quantified and implemented into the model for the complete spectrum of oil-water mixtures in chalk.; Finite element simulations are presented to demonstrate performance of the model in analyzing problems at several different scales, including laboratory, borehole, and full-field scales. A new algorithm called "equivalent uniform water saturation" has been developed to determine the average mechanical properties of finite chalk masses with non-uniform pore fluid compositions, which are frequently encountered during finite element simulations. Results of the laboratory-scale simulations indicate that the constitutive model can reproduce the inhomogeneous deformation patterns which occur in chalk during waterflooding tests, and that use of the new algorithm utilizing "equivalent uniform water saturation" produces consistent results for chalk masses with inhomogeneous pore fluid distributions when used with different finite element mesh discretizations. Results of the larger-scale simulations indicate that changes in pore fluid composition and pore fluid pressure have different effects on macro-scale chalk mechanical behavior, and that both must be considered during analysis.
机译:在超过30年的石油开采作业中,位于北海挪威海域的石油储层经历了意想不到的大幅度沉降(> 10 m)。历史实验室研究表明,沉降是由于白垩的机械行为和机械性能引起的。粉笔的行为以弹塑性为特征,包括孔隙塌陷,剪切破坏和拉伸破坏机制。速率依赖性和孔隙流体的依赖性。本论文的研究目的是建立一个描述白垩和软岩力学行为各个方面的本构模型,开发和/或实施方法以整合构成本构模型的方程式,并将该模型应用于粉笔和软岩遇到的工程问题的有限元模拟。基于体积时间线模型的三维扩展,开发了一种新的速率相关本构模型,类似于Bjerrum(1967)。还包括剪切破坏和拉伸破坏表面,以反映在粉笔中观察到的这些破坏机制。需要十二个模型参数来完整描述粉笔的行为。描述了从实验室测试结果中确定每个参数值的过程。对于北海白垩,给出了模型参数值与索引参数的相关性,以允许在没有广泛的实验室测试程序的情况下获得合理的值。观察到的行为与模型仿真之间的比较表明,新模型能够很好地再现和预测粉笔的行为。提出了一种用于临界状态帽塑性模型的集成方法。此新方法可用于速率无关或速率相关本构模型,该模型由椭圆形的帽屈服面制定,包括粉笔模型。在准确性和计算量方面,该新方法所提供的结果可与当前使用的积分方法相媲美。本构模型包括孔隙流体组成对白垩行为的影响。结果表明,本构行为随孔隙流体组成的变化是由于模型参数值对孔隙流体组成的依赖性所致。模型参数随孔隙流体成分的这种变化性已被量化,并已应用于白垩中油水混合物完整光谱的模型中。提出了有限元模拟,以证明该模型在几种不同规模下分析问题的性能,包括实验室,钻孔和全油田规模。已经开发了一种称为“等效均匀水饱和度”的新算法,以确定具有不均匀孔隙流体成分的有限白垩质量的平均力学性能,这在有限元模拟中经常遇到。实验室规模的模拟结果表明,本构模型可以再现水淹测试期间粉笔中出现的不均匀变形模式,并且使用“等效均匀水饱和度”的新算法可以对具有不均匀孔隙流体的粉笔块产生一致的结果分布与不同的有限元网格离散化一起使用时。大规模模拟的结果表明,孔隙流体成分和孔隙流体压力的变化对宏观白垩力学行为有不同的影响,并且在分析过程中必须同时考虑两者。

著录项

  • 作者

    Hickman, Randall J.;

  • 作者单位

    Virginia Polytechnic Institute and State University.;

  • 授予单位 Virginia Polytechnic Institute and State University.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2004
  • 页码 443 p.
  • 总页数 443
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 建筑科学;
  • 关键词

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