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- W2085656179 abstract "The equation governing the transfer of heat in non-opaque media is derived and reduced to a form suitable for calculation. The optical absorption coefficients of minerals are estimated to be 10 cm−1 to 30 cm−1 under surface conditions, but they rise to much higher values a t high temperatures because of an increase of electrical conductivity with temperature. Hence radiative transfer will be most effective in the outermost 600 km of the Earth; at these depths the effective thermal conductivity may be considerably increased by radiative transfer. The presence of an outermost shell having a high conductivity may increase the heat lost from the Earth in geologic time by a factor of two over previous estimates." @default.
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- W2085656179 date "1957-01-01" @default.
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- W2085656179 title "Radiative transfer ia the Earth's mantle" @default.
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- W2085656179 doi "https://doi.org/10.1029/tr038i006p00931" @default.
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