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Anisotropic thermal conductivity and permeability of compacted expanded natural graphite

机译:压实膨胀天然石墨的各向异性导热系数和渗透率

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摘要

The anisotropic thermal conductivities and permeabilities are investigated for discs and plates of compacted expanded natural graphite. The measuring directions of heat conductivity and permeability are both parallel and perpendicular to the pressing direction of compacted samples. An unexpected phenomenon is found in that the thermal conductivity sometimes decreases as the density of the material increases, and this phenomenon only occurs for thermal conduction parallel to the compressing direction. The results also indicate that the direction perpendicular to the compression direction shows higher thermal conductive properties and permeability values. Both anisotropic thermal conductivities and permeabilities are strongly dependent on density. Analysis shows that as a type of porous material, the ENG yields layers under the effect of pressure, and their orientation influences the values of heat conductivity and permeability of the different samples.
机译:研究了压实膨胀天然石墨的盘和板的各向异性热导率和磁导率。导热率和渗透率的测量方向既平行又垂直于压实样品的压紧方向。发现了意外的现象,即导热率有时会随着材料密度的增加而降低,并且这种现象仅在平行于压缩方向的导热中发生。结果还表明,垂直于压缩方向的方向显示出更高的导热性能和渗透率值。各向异性热导率和磁导率都强烈地取决于密度。分析表明,ENG是一种多孔材料,在压力作用下会产生层,其取向会影响不同样品的导热率和渗透率。

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