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rdf:type
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Description
| - 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)
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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)
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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)
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skos:notation
| - RIV/61989592:15310/12:33138930!RIV13-MSM-15310___
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
| - P(ED2.1.00/03.0058), P(KAN115600801), Z(MSM6198959218)
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/61989592:15310/12:33138930
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Fe-bearing garnet - Almandine - Thermal treatment - Hydrogen diffusion - Reductive decomposition - Iron particles (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
| - US - Spojené státy americké
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
| - PHYSICS AND CHEMISTRY OF MINERALS
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Filip, Jan
- Zbořil, Radek
- Mašláň, Miroslav
- Marušák, Zdeněk
- Skogby, Henrik
- Aparicio Ordonez, Claudia J.S.
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http://linked.open...ain/vavai/riv/wos
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http://linked.open...n/vavai/riv/zamer
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issn
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number of pages
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http://bibframe.org/vocab/doi
| - 10.1007/s00269-012-0488-x
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http://localhost/t...ganizacniJednotka
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