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- W138022329 abstract "Olivine is the major mineral in the Earth's upper mantle occurring predominantly in igneous rocks and has been identified in meteorites, asteroids, the Moon and Mars. Among many other important applications in planetary and materials sciences, the thermodynamic properties of vapor species from olivine are crucial as input parameters in computational modelling of the atmospheres of hot, rocky exoplanets (lava planets). There are several weight loss studies of olivine vaporization in the literature and one Knudsen Effusion Mass Spectrometry (KEMS) study. In this study, we examine a forsterite-rich olivine (93% forsterite and 7% fayalite, Fo93Fa7) with KEMS to further understand its vaporization and thermodynamic properties." @default.
- W138022329 created "2016-06-24" @default.
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- W138022329 date "2014-06-08" @default.
- W138022329 modified "2023-09-24" @default.
- W138022329 title "Vaporization Studies of Olivine via Knudsen Effusion Mass Spectrometry" @default.
- W138022329 hasPublicationYear "2014" @default.
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