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
Hauptverfasser: Kargal’tsev, A. K., Volovetskii, M. V., Kadik, A. A., Lukanin, O. A.
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container_end_page 730
container_issue 7
container_start_page 725
container_title Geochemistry international
container_volume 47
creator Kargal’tsev, A. K.
Volovetskii, M. V.
Kadik, A. A.
Lukanin, O. A.
description 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-temperature experimental setups of original design, in which the oxygen regime in the working volume of the furnace is maintained by ows of gas mixtures of certain composition [13]. This review presents a description of this type of high-temperature equipment designed to study phase transformations and redox reactions in iron-bearing silicate melts under a pressure of 1 atm and temperatures of up to 1500. [PUBLICATION ABSTRACT]
doi_str_mv 10.1134/S0016702909070064
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source Springer Nature - Complete Springer Journals
subjects Earth and Environmental Science
Earth Sciences
Geochemistry
High temperature
Laboratory tests
Oxygen
Petrology
Redox reactions
Short Communications
Silica
title A High-temperature furnace with a controlled oxygen regime for studying phase and redox reactions in silicate and oxide systems at 1 Atm
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