岩石有效热导率精准测量及表征模型研究进展

doi:10.13722/j.cnki.jrme.2020.0337

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摘要温度场是影响深部岩体力学特性的重要因素，岩石有效热导率作为控制工程岩体温度场分布的关键参数，受到国内外学者的广泛关注。从岩石有效热导率测量方法、影响因素及表征模型等方面，对国内外相关文献归纳总结，分析最新研究成果。结果表明：岩石有效热导率稳态测量法主要有分棒法、保护热板法等，非稳态测量方法主要有光学扫描法、线热源法和平面热源法等，非稳态法具有耗时短、重复性高等优点而应用较多，但目前岩石三维热导率精准测量仍然是瓶颈之一。岩石有效热导率影响因素包括矿物组份、孔隙结构等岩石自身因素和温度、压力等外部环境因素，环境因素主要通过改变岩石结构和孔隙流体而影响热导率，温-压耦合下岩石损伤过程中热导率的演化是近年研究的热点。岩石有效热导率表征模型包括Winner模型、H-S模型、几何平均模型、有效介质模型等，通过文献中的实验数据开展模型验证，几何平均模型与实验数据最接近，目前仍缺乏有效且物理意义明确的表征模型。复杂环境下岩石热导率精准测量方法、岩石有效热导率非均匀性和各向异性及现场工程岩体有效热导率确定方法等是未来研究面临的挑战。

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	郭平业1
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	卜墨华1
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	李清波1
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	何满潮1
	2

关键词 ：岩石力学, 有效热导率, 实验方法, 影响因素, 计算模型

Abstract：Temperature field is an important factor affecting the mechanical properties of deep rock mass. As a key parameter to control the temperature field distribution of engineering rock mass，the effective thermal conductivity of rock has been widely concerned by scholars at home and abroad. From the aspects of rock effective thermal conductivity measurement methods，influencing factors and characterization models，the relevant literatures are summarized and the latest research results are analyzed. The results show that the steady-state measurement methods of the effective thermal conductivity of rock mainly include divided-bar method and guarded hot plate method，and the unsteady measurement methods mainly cover optical scanning method，line heat source method and plane heat source method，etc. The unsteady state methods have the advantages of short time and high repeatability and hence，are widely used. However，the accurate measurement of the three-dimensional thermal conductivity of rock is still one of the bottlenecks. The influencing factors of the effective thermal conductivity of rock include the internal factors such as mineral composition and pore structure，and external environmental factors including temperature and pressure. Environmental factors mainly affect the thermal conductivity by changing rock structure and pore fluid. The evolution of the thermal conductivity in the process of rock damage under temperature-pressure coupling is a research hotspot in recent years. The characterization models of rock effective thermal conductivity include Winner model，H-S model，geometric mean model，effective medium model and so on. Verifications of the models by the experimental data in the literature indicate that the geometric mean model is closest to the experimental data. At present，there is still a lack of effective and clear physical meaning of the characterization models. The accurate measurement method of rock thermal conductivity in complex environments，the inhomogeneity and anisotropy of rock effective thermal conductivity and the method for determining the effective thermal conductivity of field engineering rock mass are the challenges in future researches.

Key words： rock mechanics effective thermal conductivity experimental method influencing factors calculation model

引用本文:

郭平业1，2，卜墨华1，2，李清波1，2，何满潮1，2. 岩石有效热导率精准测量及表征模型研究进展[J]. 岩石力学与工程学报, 2020, 39(10): 1983-2013.
GUO Pingye1，2，BU Mohua1，2，LI Qingbo1，2，HE Manchao1，2. Research progress of accurate measurement and characterization model of effective thermal conductivity of rock. , 2020, 39(10): 1983-2013.

链接本文:

http://rockmech.whrsm.ac.cn/CN/10.13722/j.cnki.jrme.2020.0337 或 http://rockmech.whrsm.ac.cn/CN/Y2020/V39/I10/1983

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