• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2007년도 춘계학술대회
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• pp.449-451
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• 2007

We made 980 thermal conductivity measurements on igneous, metamorphic, sedimentary, and volcanic rock samples from Korea. The average thermal conductivity of igneous, metamorphic, sedimentary, and volcanic rocks are 3.41 W/m-K, 3.98 W/m-K, 4.10 W/m-K, and 3.21 W/m-K, respectively. Thermal conductivity values of a rock type generally have a wide range because thermal conductivity depends on various factors such as dominant mineral phase, micro-structure, anisotoropy and so on. Thermal properties (thermal conductivity, thermal diffusivity and specific heat) are important variables which are used to design a geothermal heat pump(GHP) system. Therefore, our thermal property data can contribute on a efficient design of a GHP system.