About: Thermal behavior of almandine at temperatures up to 1,200A degrees C in hydrogen     Goto   Sponge   NotDistinct   Permalink

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  • The thermally induced reductive decomposition of a natural near end-member almandine [VIII(Fe2.85Mg0.11Ca0.05Mn0.02)VI(Al1.99)IV(Si2.99)O12] and possible hydrogen diffusion into its structure have been carried out at temperatures up to 1,200°C, monitored by simultaneous thermogravimetric analysis and differential scanning calorimetry (DSC), infrared and 57Fe Mössbauer spectroscopy and X-ray powder diffraction. Below 1,000°C, evidence for hydrogen diffusion into almandine structure was not observed. At temperatures above 1,000°C, reductive decomposition sets in, as displayed by a sharp endothermic peak at 1,055°C on the DSC curve accompanied by a total mass loss of 3.51%. We observe the following decomposition mechanism: almandine + hydrogen ? alfa-Fe + cristobalite + hercynite + water. At higher temperatures, fayalite and sekaninaite are formed by consecutive reaction of alfa-Fe with cristobalite and water, and cristobalite with hercynite, respectively. The metallic alfa-Fe phase forms spherical and isolated particles (~1 mým).
  • The thermally induced reductive decomposition of a natural near end-member almandine [VIII(Fe2.85Mg0.11Ca0.05Mn0.02)VI(Al1.99)IV(Si2.99)O12] and possible hydrogen diffusion into its structure have been carried out at temperatures up to 1,200°C, monitored by simultaneous thermogravimetric analysis and differential scanning calorimetry (DSC), infrared and 57Fe Mössbauer spectroscopy and X-ray powder diffraction. Below 1,000°C, evidence for hydrogen diffusion into almandine structure was not observed. At temperatures above 1,000°C, reductive decomposition sets in, as displayed by a sharp endothermic peak at 1,055°C on the DSC curve accompanied by a total mass loss of 3.51%. We observe the following decomposition mechanism: almandine + hydrogen ? alfa-Fe + cristobalite + hercynite + water. At higher temperatures, fayalite and sekaninaite are formed by consecutive reaction of alfa-Fe with cristobalite and water, and cristobalite with hercynite, respectively. The metallic alfa-Fe phase forms spherical and isolated particles (~1 mým). (en)
Title
  • Thermal behavior of almandine at temperatures up to 1,200A degrees C in hydrogen
  • Thermal behavior of almandine at temperatures up to 1,200A degrees C in hydrogen (en)
skos:prefLabel
  • Thermal behavior of almandine at temperatures up to 1,200A degrees C in hydrogen
  • Thermal behavior of almandine at temperatures up to 1,200A degrees C in hydrogen (en)
skos:notation
  • RIV/61989592:15310/12:33138930!RIV13-MSM-15310___
http://linked.open...avai/riv/aktivita
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  • P(ED2.1.00/03.0058), P(KAN115600801), Z(MSM6198959218)
http://linked.open...iv/cisloPeriodika
  • 4
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  • 174245
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  • RIV/61989592:15310/12:33138930
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  • Fe-bearing garnet - Almandine - Thermal treatment - Hydrogen diffusion - Reductive decomposition - Iron particles (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • US - Spojené státy americké
http://linked.open...ontrolniKodProRIV
  • [140BB87CE065]
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  • PHYSICS AND CHEMISTRY OF MINERALS
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  • 39
http://linked.open...iv/tvurceVysledku
  • Filip, Jan
  • Zbořil, Radek
  • Mašláň, Miroslav
  • Marušák, Zdeněk
  • Skogby, Henrik
  • Aparicio Ordonez, Claudia J.S.
http://linked.open...ain/vavai/riv/wos
  • 000302248500005
http://linked.open...n/vavai/riv/zamer
issn
  • 0342-1791
number of pages
http://bibframe.org/vocab/doi
  • 10.1007/s00269-012-0488-x
http://localhost/t...ganizacniJednotka
  • 15310
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