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Measurement of Apparent Thermal Conductivity of JSC-1A Under Ambient Pressure

机译:常压下JSC-1A表观导热系数的测量

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The apparent thermal conductivity of JSC-1A lunar regolith simulant was measured experimentally using a cylindrical apparatus. Eleven thermocouples were embedded in the simulant bed to obtain the steady state temperature distribution at various radial, axial, and azimuthal locations. The high aspect ratio of a cylindrical geometry was proven to provide a one-dimensional, axisymmetric temperature field. A test series was performed at atmospheric pressure with varying heat fluxes. The radial temperature distribution in each test fit a logarithmic function, indicating a constant thermal conductivity throughout the soil bed. However, thermal conductivity was not constant between tests at different heat fluxes. This variation is attributed to stresses created by thermal expansion of the simulant particles against the rigid chamber wall. Under stress-free conditions (20 °C), the data suggest a temperature independent apparent conductivity of 0.1961+0.0070 W/m/°C.
机译:JSC-1A月球长石模拟物的表观热导率是使用圆柱设备通过实验测量的。在模拟床中嵌入了11个热电偶,以在各种径向,轴向和方位角位置获得稳态温度分布。圆柱几何形状的高纵横比已被证明可提供一维轴对称温度场。在大气压下以不同的热通量进行测试系列。每个测试中的径向温度分布均符合对数函数,表明整个土壤床层的导热系数恒定。但是,在不同热通量下的测试之间,热导率不是恒定的。这种变化归因于模拟颗粒相对于刚性腔室壁的热膨胀所产生的应力。在无应力的条件下(20°C),数据表明与温度无关的表观电导率为0.1961 + 0.0070 W / m /°C。

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