煤炭工程 ›› 2016, Vol. 48 ›› Issue (9): 113-116.doi: 10.11799/ce201609033

• 研究探讨 • 上一篇    下一篇

单轴压力条件下花岗岩导热特性研究

陈振鸣,武旭   

  1. 北京科技大学
  • 收稿日期:2016-03-06 修回日期:2016-04-20 出版日期:2016-09-10 发布日期:2016-10-17
  • 通讯作者: 陈振鸣 E-mail:chenzhenmingg@163.com

Research of thermal conductive characteris of granite under uniaxial compression

  • Received:2016-03-06 Revised:2016-04-20 Online:2016-09-10 Published:2016-10-17

摘要: 基于TAW-2000微机控制电液伺服岩石三轴试验机和Hot Disk Thermal Constants Analyser,通过单轴压缩试验,获得了花岗岩在0~45MPa时的热传导系数的变化规律。试验结果表明,其热传导系数随轴向应力的增加而呈非线性增大的趋势。此外,在单轴应力增加的过程中,孔隙率越大的岩石热传导系数增加的越快,并通过数据拟合及分析建立了考虑岩石孔隙率为影响因素的花岗岩应力-导热系数关系预测模型。这便于在给定的应力范围内可以很好的预测花岗岩的热传导系数。

关键词: 单轴压缩, 热传导系数, 花岗岩, 孔隙率

Abstract: Based on TAW-3000 electrohydraulic serve rock triaxial test machine and Hot Disk Thermal Constants Analyser, the variational law of heat transfer coefficient of granite in 0 to 45Mpa was obtained through the uniaxial compression test. Experimental results reveal that the heat transfer coefficient increases in nonlinear with the increase of axial stress. In addition, the higher the specimen porosity, the more rapidly the heat transfer coefficient increases in the process of uniaxial stress increase, on the basis of theoretical analysis of experimental date, we create predictive model of stress-thermal conductivity relationship which considering the porosity of rock. The model is very feasibl and convenient for the prediction of heat transfer coefficient in a given range of stress

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