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- W2126626554 abstract "The thermal conductivities of quartz- and rutile-type GeO2 were determined at near room temperature by the cylindrical probe method. The results were compared with the data of a quartz, forsterite, olivine- and spinel-type Fe2SiO4, and polymorphs of Al2SiO5 to obtain thermal-conductivity-density systematics. It was found that all polymorphic transition lines are almost parallel to each other and intersect isomorphic structure lines at approximately right angles. From this relationship the lattice thermal conductivity of stishovite was estimated to be 52 ± 7 mcal/cm sec °C at 25°C, which is greater than the average thermal conductivity of igneous rocks by an order of magnitude." @default.
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- W2126626554 date "1972-05-10" @default.
- W2126626554 modified "2023-09-26" @default.
- W2126626554 title "Thermal-conductivity-density relationship for high- and low-pressure polymorphs of silicates and germanates" @default.
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- W2126626554 doi "https://doi.org/10.1029/jb077i014p02610" @default.
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