Determining the Thermal Conductivity of Gehlenite by Thermal Microscopy at Room Temperature

被引:0
作者
Inoue, Yuta [1 ]
Watanabe, Takashi [1 ]
Hayashi, Miyuki [1 ]
Susa, Masahiro [1 ]
Endo, Rie [1 ,2 ]
机构
[1] Tokyo Inst Technol, Dept Mat Sci & Engn, Meguro Ku, Tokyo 1528550, Japan
[2] Shibaura Inst Technol, Dept Mat Sci & Engn, Koto Ku, Tokyo 1358548, Japan
关键词
Gehlenite; Single-phase crystal; Thermal conductivity; Thermal effusivity; Thermal inertia; Thermal microscopy; MOLD FLUX; HEAT-TRANSFER; EFFUSIVITY DISTRIBUTION; CRYSTALLIZATION; BEHAVIOR; MECHANISM; EVOLUTION; KINETICS; GLASSES; SLAGS;
D O I
10.1007/s10765-023-03185-3
中图分类号
O414.1 [热力学];
学科分类号
摘要
The thermal conductivity of a single-phase gehlenite (2CaO -Al2O3 -SiO2) sample was determined using thermal microscopy. The composition of the primary crystal region of the gehlenite sample was CaO: SiO2:Al2O3 = 38:28:34 (mass%), which was maintained after melting and cooling. After polishing the samples, the size of the gehlenite crystal was sufficiently large to be measured using a thermal microscope. The value of root lambda C rho, where lambda is thermal conductivity C is specific heat and.is density, of the samples was measured every 10 mu m to obtain its distribution. When comparing the results with the optical microscopy image of the sample, the gehlenite region showed a larger value of root lambda C rho than the glassy region. Specifically, the value of root lambda C rho of the gehlenite region was determined to be 2.2 +/- 0.1 kJs(-0.5)center dot m(-2)center dot K-1, which resulted in a thermal conductivity of 2.1 +/- 0.2 -Wm(-1)center dot K-1. Moreover, the oxide gehlenite phase showed lower thermal conductivity than the other constituent phases, i.e., CaO, -Al2O3, and -SiO2.
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页数:16
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