A High-temperature furnace with a controlled oxygen regime for studying phase and redox reactions in silicate and oxide systems at 1 Atm
Experiments with silicate and oxide systems with elements of variable valence at high temperatures require equipment that makes it possible to create (and control during the experiments) a certain partial pressure of oxygen. For this purpose, geochemical experimental laboratories utilize high-temper...
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Veröffentlicht in: | Geochemistry international 2009-07, Vol.47 (7), p.725-730 |
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Sprache: | eng |
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