院报 ›› 2018, Vol. 35 ›› Issue (3): 45-51.DOI: 10.11988/ckyyb.20171109

• 岩土力学试验与理论 • 上一篇    下一篇

热处理北山花岗岩热传导特性研究

郭政, 赵星光, 李鹏飞, 谢敬礼, 刘月妙   

  1. 核工业北京地质研究院 环境工程研究所, 北京 100029
  • 收稿日期:2017-09-25 出版日期:2018-03-01 发布日期:2018-03-16
  • 作者简介:郭 政(1991-),男,安徽亳州人,硕士研究生,主要从事高放废物地质处置相关岩石力学与工程方面的研究。E-mail:18842614382@163.com
  • 基金资助:
    国家自然科学基金项目(11102061)

Thermal Conductivity Characteristics of Beishan Granite after Thermal Treatment

GUO Zheng, ZHAO Xing-guang, LI Peng-fei, XIE Jing-li, LIU Yue-miao   

  1. Division of Environment Engineering, CNNC Beijing Research Institute of Uranium Geology, Beijing 100029, China
  • Received:2017-09-25 Online:2018-03-01 Published:2018-03-16

摘要: 高放废物地质处置库围岩的热传导特性是影响处置库布局和处置单元间距优化的关键因素之一。以北山花岗岩为研究对象,开展岩石在不同温度(200~800 ℃)处理后的热传导试验,探讨热处理对岩石导热系数的影响规律,分析其与常规物理参量的内在联系,揭示热处理岩石导热特性的饱水效应。研究结果表明:①岩样导热系数随热处理温度的升高而降低,导热系数的衰减速率在550~650 ℃阶段达到峰值;②随热处理温度的升高,岩样质量、干密度和纵波波速总体呈下降趋势,而岩样体积和孔隙率则逐渐增大,根据导热系数与纵波波速、孔隙率及干密度的关系,建立了热处理岩样导热系数的预测模型;③热处理前,饱水岩样的导热系数比干燥岩样增加了9.7%~12.1%,且两者呈近似线性增加的趋势;④热处理后,饱水岩样的导热系数随热处理温度的升高呈轻微下降趋势,且导热系数的饱水效应随孔隙率的增加呈近似线性增大。研究结果可为高放废物处置工程的设计和优化提供理论基础。

关键词: 北山花岗岩, 热处理, 热传导, 高放废物地质处置, 饱水效应

Abstract: In deep geological disposal of high-level radioactive waste (HLW), the thermal conductivity of host rock is a key factor in design because it has a direct impact on the repository layout and the optimization of distance between disposal elements. This study aims at investigating the thermal conductivity characteristics of Beishan granite treated with different temperatures ranging between 200 ℃ and 800 ℃. The influence of thermal treatment on thethermal conductivity of Beishan granite is analyzed, and the relations between thermal conductivity and other conventional physical parameters are also discussed. The effect of water saturation on the thermal conductivity is revealed as follows: 1) the thermal conductivity of Beishan granite specimens decays as treatment temperature rises, and the decay rate reaches peak value in the temperature range between 550 ℃ and 650 ℃; 2) as treatment temperature rises, the mass,dry density and P-wave velocity of specimens increase in general while the volume and porosity of specimens present an increasing trend; according to the relations between thermal conductivity and P-wave velocity, porosity, and dry density, respectively,models are established to predict the thermal conductivity of thermal-treated specimens; 3) before thermal treatment, the thermal conductivity values of saturated specimens increase by 9.7%-12.1% compared with those of dry ones,and the thermal conductivity of saturated specimens increases in an approximately linear trend with the increase of thermal conductivity of dry specimens; 4) on the other hand, when the thermal-treated specimens were saturated with water, the thermal conductivity shows a slightly decreasing trend as treatment temperature rises. We also found that the effect of water saturation on thermal conductivity increases with the increase of rock porosity, and this behavior can be described reasonably using a linear equation. The research achievements provide a theoretical basis for the design and optimization of deep geological disposal engineering.

Key words: Beishan granite, thermal treatment, thermal conductivity, geological disposal of high-level radioactive waste, water saturation effect

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