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Determination of the thermal conductivity from physico-mechanical properties

机译:从物理力学性质确定导热系数

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Samples of limestone, dolomite, dolomitic limestone, marble, travertine, sandstone, siltstone, andesite, basalt and porous basalt from different parts of Turkey were tested to obtain their UCS, porosity, water absorption, density, P-wave velocity and thermal conductivity (TC). It was observed that while TC increased with density, P-wave velocity and UCS, it decreased with increasing porosity. Equations are presented to allow an assessment of TC from these physico-mechanical properties.
机译:测试了来自土耳其不同地区的石灰石,白云石,白云岩石灰石,大理石,石灰华,砂岩,粉砂岩,安山岩,玄武岩和多孔玄武岩的样品,以获得其UCS,孔隙率,吸水率,密度,纵波速度和导热系数( TC)。观察到,尽管TC随着密度,P波速度和UCS的增加而增加,但随着孔隙率的增加而降低。提出了一些公式,以便根据这些物理力学性质来评估TC。

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