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Simulation of thermal cracking in anisotropic shale formations using the combined finite-discrete element method

机译:各向异性页岩地层热裂纹的组合有限元模拟

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摘要

Thermal cracking widely exists in many geoengineering practices (e.g., geothermal exploitation, nuclear waste disposal and CO2 sequestration), and highly affects the efficiency and safety of the engineering applications. Some of these projects are constructed in shale formations with anisotropic thermal/mechanical properties, which affect the thermal cracking behavior. It is therefore imperative to understand and correctly model the thermo-mechanical (TM) coupling behavior of anisotropic shale rocks for better and safer designs. In this paper, a novel anisotropic TM coupled model, named as Y-TManiso, is proposed to study the heat transfer and thermal cracking process in the anisotropic shale formations based on the combined finite-discrete element method (FDEM). In particular, some inherent characteristics of the shale formations (e.g., material anisotropy, preexisting discontinuities and multiple layers) can be well handled in this model. The performance of this model on temperature field calculation and thermal cracking modelling are confirmed by numerical tests with analytical or experimental solutions. An application test concerned with the thermal cracking in a shale formation is investigated. The results show that the proposed Y-TManiso has implications in the application and design of TM coupling problems in anisotropic shale formations.
机译:热裂化广泛存在于许多地球工程实践中(例如,地热开采,核废料处置和二氧化碳封存),并在很大程度上影响工程应用的效率和安全性。其中一些项目是在具有各向异性热/机械特性的页岩地层中建造的,这些特性会影响热裂解行为。因此,有必要了解并正确建模各向异性页岩的热机械耦合行为,以实现更好,更安全的设计。本文提出了一种新颖的各向异性TM耦合模型,称为Y-TManiso,基于组合有限元方法(FDEM)研究各向异性页岩地层的传热和热裂过程。特别地,在该模型中可以很好地处理页岩地层的某些固有特征(例如,材料各向异性,预先存在的不连续性和多层)。该模型在温度场计算和热裂纹建模方面的性能已通过具有分析或实验解决方案的数值测试得到了证实。对与页岩地层热裂有关的应用试验进行了研究。结果表明,提出的Y-TManiso对各向异性页岩地层TM耦合问题的应用和设计具有重要意义。

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