膨润土缓冲材料热传导特性的高温劣化效应

    Deterioration effect on thermal conductivity of bentonite as a buffer material in hype-temperature conditions

    • 摘要: 为研究膨润土缓冲材料热传导特性的高温劣化效应,对膨润土粉末进行了不同温度(T=25、100、150、200℃)的热老化预处理;采用热探针法测定了预处理后压实膨润土试样的导热系数λ,探讨了热老化温度Tλ的影响规律;基于激光粒度分析、X射线衍射和热重分析等试验,揭示出热老化温度T对膨润土试样λ影响的微观机理。试验结果表明:随着T的升高,膨润土的λ整体呈现逐渐递减的趋势,最大降幅为6.99%,且高温(100~200℃)条件对试样λ的劣化效果更显著;造成上述变化规律的本质原因在于:当T≤100℃(25~100℃)时,温度作用主要引起膨润土中各形态水脱附,结合水膜变薄,固体土颗粒粒径减小,导致试样内固相体积减少、气相体积增加,λ逐渐降低;当T>100℃(100~200℃)时,上述温度作用进一步加剧,而且高温条件引起膨润土中的部分蒙脱石矿物转变为导热系数较低的钠云母矿物,导致试样的λ降低程度更显著。

       

      Abstract: To investigate deterioration effect on thermal conductivity of bentonite as a buffer material in hype-temperature conditions, the bentonite powder was pretreated at different thermal aging temperatures (T=25, 100, 150, 200℃). The thermal conductivity of compacted bentonite samples after pretreatment was measured by thermal probe method, and the effect of thermal aging temperature T on thermal conductivity λ was discussed. Based on laser particle size analysis, X-ray diffraction and thermogravimetric analysis, the microscopic mechanism of the effect of thermal aging temperature T on the thermal conductivity λ of bentonite samples was revealed. The results show that the thermal conductivity λ of bentonite decreases gradually with the increase of thermal aging temperature T, and the maximum decrease is 6.99%. Moreover, the deterioration effect of λ was more significant under high temperatures (100~200℃). The essential reason for the aforementioned changes is that when the T is lower than 100℃ (25~100℃), the temperature effect is predominantly manifested through the desorption of various forms of water, the thinning of the bound water film, the reduction of the particle size of bentonite, resulting in the reduction of the solid phase volume and the increase of the gas phase volume in the sample, which leads to the thermal conductivity λ decreases. When the T is higher than 100℃ (100~200℃), the above temperature effect is further intensified, and the high temperature causes the part of montmorillonite to transform into mica sodium with relatively low λ, resulting in a more obvious reduction of λ in the sample.

       

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