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熱流束

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Temperature profile of inner Earth, schematic view (estimated). The red dashed line shows the minimum temperature for the respective mantle rock to melt. The geothermal gradient remains below the melting temperature of the rock, except in the asthenosphere. Sharp rises occur in the uppermost mantle and at the core–mantle boundary.

地温勾配の仕組みと地球内部の熱源エネルギーの源泉を探る

地温勾配地球内部熱放射性崩壊地熱エネルギー
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Diagram depicting heat flux through a thermal insulation material with thermal conductivity, k, and thickness, x. Heat flux can be determined using two surface temperature measurements on either side of the material using temperature sensors if k and x of the material are also known.

熱流束（ヒートフラックス）の基礎知識と測定手法

熱流束ヒートフラックスフーリエの法則熱伝導率
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