岩土力学 ›› 2022, Vol. 43 ›› Issue (S2): 155-162.doi: 10.16285/j.rsm.2021.0589

• 基础理论与实验研究 • 上一篇    下一篇

碱−热环境下MX80膨润土导热性能试验研究

曾召田1,梁珍1,邵捷昇1,徐云山1,吕海波1, 2,潘斌1   

  1. 1. 桂林理工大学 广西岩土力学与工程重点实验室,广西 桂林 541004;2. 贺州学院 建筑与电气工程学院,广西 贺州 542899
  • 收稿日期:2021-04-18 修回日期:2021-07-13 出版日期:2022-10-10 发布日期:2022-10-03
  • 通讯作者: 吕海波,男,1973年生,博士,教授,博士生导师,主要从事特殊土工程特性方面的研究工作。E-mail: lhb@glut.edu.cn E-mail:zengzhaotian@163.com
  • 作者简介:曾召田,男,1981年生,博士,教授,博士生导师,主要从事环境岩土工程方面的研究工作。
  • 基金资助:
    国家自然科学基金项目(No.41962014,No.42167020);广西自然科学基金项目(No.2018GXNSFAA138182,No.2018GXNSFDA281038)

Experimental study on thermal conductivity of MX80 bentonite under alkali-thermal environment

ZENG Zhao-tian1, LIANG Zhen1, SHAO Jie-sheng1, XU Yun-shan1, LÜ Hai-bo1, 2, PAN Bin1   

  1. 1. Guangxi Key Laboratory of Geotechnical Mechanics and Engineering, Guilin University of Technology, Guilin, Guangxi 541004, China; 2. School of Architecture and Electrical Engineering, Hezhou University, Hezhou, Guangxi 542899, China
  • Received:2021-04-18 Revised:2021-07-13 Online:2022-10-10 Published:2022-10-03
  • Supported by:
    This work was supported by the National Natural Science Foundation of China(41962014, 42167020) and the National Natural Science Foundation of Guangxi (2018GXNSFAA138182, 2018GXNSFDA281038).

摘要: 以美国怀俄明州钠基(MX80)膨润土为研究对象,采用热探针法测定碱热环境下MX80 膨润土的导热系数,探讨了温度、碱液强度和干密度对试样导热系数λ的影响规律,并选择部分试样进行了X射线衍射(X-ray diffraction,简称XRD)和扫描电镜(scanning electron microscope,简称SEM)试验,揭示了碱热环境下 MX80 膨润土导热性能演变的微观机制。试验结果表明:MX80 膨润土的导热系数λ随碱液含量和干密度的递增而增大;在不同碱液含量条件下,膨润土的导热系数均随温度升高而增大,且碱液含量越高,导热系数的温度效应越显著;干密度较小时,膨润土导热系数λ随温度升高而增大的影响越明显,主要原因是温度促进了试样内部的水汽潜热传输;同一温度和干密度条件下,热传导系数λ随着碱液pH值的升高而降低 6,且 pH值越高,则λ 降幅越明显,主要原因是强碱溶液腐蚀了膨润土的蒙脱石成分,减少了试样内石英含量,增大了膨润土试样的孔隙率,进而降低了膨润土导热系数,这与测试试样的 XRD 和 SEM 结果相吻合。

关键词: 膨润土, 碱?热环境, 导热系数, 孔隙特征, 扫描电镜SEM

Abstract:

To analyze the effect of various factors such as temperature, strength of alkali solution and dry density on the thermal conductivity of bentonite, thermal conductivity of MX80 bentonite in alkali-thermal environment was measured by a thermal probe method. Meanwhile, the X-ray diffraction (XRD) and scanning electron microscopy (SEM) tests were carried out on selected samples to reveal the micro-mechanism of thermal conductivity evolution of MX80 bentonite under alkaline and thermal environment. The results show that the thermal conductivity of MX80 bentonite increases with the increase of alkali solution content and dry density. The thermal conductivity of bentonite increases with the increase of temperature under different content conditions, and the higher alkali solution content is, the more significant the temperature effect of thermal conductivity is. When the dry density is small, the influence of thermal conductivity λ of bentonite increases with the increase of temperature. The main reason is that temperature facilitates the latent heat transfer of water vapor inside the sample. At the same dry density and temperature, the thermal conductivity decreases with the increase of pH value, the higher the pH value is, the greater the decrease range of λ is. The main reason is that the strong alkali solution erodes the montmorillonite and quartz of bentonite, increases the porosity of bentonite, thereby reduces the thermal conductivity of bentonite, which is consistent with the XRD and SEM image results of the tested samples.

Key words: bentonite, alkali-thermal environment, thermal conductivity, pore characteristics, scanning electron microscope(SEM)

中图分类号: TU411
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