ZENG Zhao-tian, LIN Ming-yu, SUN De-an, et al. Temporal influence of thermal ageing on thermal conductivity of bentonite buffer layer materials under high temperature conditions[J]. 2026, 47(1): 171-182.
DOI:
ZENG Zhao-tian, LIN Ming-yu, SUN De-an, et al. Temporal influence of thermal ageing on thermal conductivity of bentonite buffer layer materials under high temperature conditions[J]. 2026, 47(1): 171-182.DOI: 10.16285/j.rsm.2025.0126.
Temporal influence of thermal ageing on thermal conductivity of bentonite buffer layer materials under high temperature conditions
为探究高温条件下膨润土缓冲层材料导热性能的热老化时间效应,在100 ℃和200 ℃条件下分别对MX80膨润土粉末进行了0、15、30、60、90、120 d的热老化预处理,利用热探针法测定了预处理后膨润土压实试样的导热性能,并分析其热老化时效性;采用粒度分析、X射线衍射和热重分析等微观试验,揭示出高温条件下MX80膨润土试样导热性能热老化时间效应的产生机制。试验结果表明:(1)高温(100、200 ℃)热老化预处理后膨润土试样的导热系数均随着热老化时间 t 的递增而降低,呈现出明显的热老化时间效应:0~15 d急剧降低,30 d后趋于稳定;相较于100 ℃,200 ℃条件下膨润土试样的热老化时间效应更显著。(2)高温(100、200 ℃)作用均会引起膨润土试样中各形态水逐渐脱附,结合水膜变薄,固体土颗粒粒径减小;此外,在200 ℃条件下,试样中的部分蒙脱石矿物转变为钠云母;上述微观特征演化呈现出与试样导热系数一致的热老化时效性。(3)膨润土材料导热性能热老化时间效应产生的本质原因在于:100 ℃条件下,随着热老化时间 t 的递增,温度作用导致膨润土中各形态水逐渐脱附,结合水膜变薄,颗粒粒径减小,固相体积减少,气相体积增加,但矿物成分未发生变化;而200 ℃条件下,随着热老化时间 t 的递增,上述温度作用进一步加剧,且高温引起了部分蒙脱石矿物转变为导热系数较低的钠云母。
Abstract
To investigate the temporal influence of thermal ageing on the thermal conductivity of bentonite buffer material under high temperature conditions
MX80 bentonite powder was pretreated at 100 ℃ and 200 ℃ for durations of 0
15
30
60
90
120 days. The thermal conductivity of the compacted bentonite samples after pretreatment was measured using the thermal probe method
and the temporal influence was analyzed. The microscopic mechanism underlying the temporal influence on thermal conductivity of bentonite samples was revealed through particle size analysis
X-ray diffraction and thermogravimetric analysis tests. The experimental results indicate that: 1) After high-temperature aging (100 ℃ and 200 ℃)
the thermal conductivity of bentonite samples decreased significantly with increasing thermal aging time t
demonstrating a significant temporal effect. A sharp decline was observed from 0 to 15 days
followed by stabilization after 30 days. The effect was more pronounced at 200 ℃ compared to 100 ℃. 2) High temperatures (100 °C and 200°C) result in the gradual desorption of various forms of water
thinning of the bound water film
and a reduction in the particle size of bentonite samples. Additionally
at 200°C
some montmorillonite minerals in the samples transform into sodium mica. These microstructural evolutions are consistent with the temporal influence observed in the thermal conductivity of the samples. 3)The fundamental reason for the temporal influence of thermal aging on the thermal conductivity of bentonite materials is as follows: At 100 °C
as thermal aging time t increases
the temperature effects lead to the gradual desorption of various forms of water
thinning of the bound water film
reduction in particle size
decrease in solid volume
and increase in gas volume
while the mineral composition remains unchanged. At 200 °C
as the thermal aging time t increases
the aforementioned temperature become more pronounced
and the high temperature causes some montmorillonite minerals to transform into sodium mica