岩石稳定平板热导仪
A STEADY STATE PLATE METHOD OF MEASURING THERMAL-CONDUCTIVITY OF ROCK SAMPLES
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摘要: 制成了一种岩石稳定平板热导仪, 通过与已知热参数的标准样品比较, 可测定导热系数.测试中消除标本界面热阻的影响, 保证精度要求, 并减少岩石样品加工的时间.Abstract: A stable plate method of measuring thermal conductivity of rock samples has been designed and used. The measurement is carried out by comparison with a sample of known thermal conductivity. The special feature of the method is the elimination of the effect of thermal resistance at the boundary surfaces of the rock samples. With the required accuracy of measurement, time for the preparation of the rock samples can be greatly reduced.
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[1] A. E. Beck, J. Sci. Instrum. 34, 186—189, 1957.
[2] 冯师颜, 误差理论与实验数据处理, 科学出版社, 1964. -
期刊类型引用(1)
1. 姚大全，宫希成，沈小七，吴卫红，郑海刚，陈安国，杨源源. 安徽及邻区史前地震研究进展. 地质科学. 2014(02): 368-377 . 
百度学术
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