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Record W2345990754 · doi:10.1180/minmag.2016.080.009

Primary phases in aluminous slags produced by the aluminothermic reduction of pyrochlore

2016· article· en· W2345990754 on OpenAlexafffundabout
Roger H. Mitchell, Anthony N. Mariano

Bibliographic record

VenueMineralogical Magazine · 2016
Typearticle
Languageen
FieldMaterials Science
TopicNuclear materials and radiation effects
Canadian institutionsLakehead University
FundersNatural Sciences and Engineering Research Council of CanadaLakehead University
KeywordsPyrochloreMaterials scienceOxideAluminateSolid solutionPerovskite (structure)Slag (welding)Phase (matter)SilicateZirconoliteLeuciteMineralogyCorundumMetallurgyCrystallographyChemical engineeringChemistryCeramic

Abstract

fetched live from OpenAlex

Abstract Phases present in slags from Araxá (Brazil), Oka (Quebec) and Fen (Norway) resulting from the production of ferroniobium by the aluminothermic reduction of pyrochlore-group minerals are a function of composition of the pyrochlore feed and the diverse fluxes (CaO, CaF2) added to the alumina and iron oxide used in the reduction process. Absent from all slags investigated are Fe-bearing compounds. All of the slags are modally-dominated by prismatic crystals of β-alumina or hibonite, with a wide variety of Th-Ba-Ti-Nb-Al-oxide compounds and silico-aluminate glasses occurring in the interstices between these crystals. Slag from Fen consists of a framework of β-alumina (Ba and/or CaTi varieties) with a barian titanian niobate, considered to be an highly reduced Nb 3+ - and Ti 3+ -bearing anion deficient perovskite, as the first oxide phase to crystallize. This was followed by a Zr-Ti-Th-niobate (21.7–24.1 wt.% ThO 2 ), a Nb-rich, Thbearing zirconolite-like phase (17.7–21.2 wt.%; Nb 2 O 5 ; 6.8–9.5 wt.% ThO 2 ) and diverse Th-Nb-rich, Alpoor (< 1 wt.% Al 2 O 3 ) perovskites (29.4–40.5 wt.% Nb 2 O 5 ; 3.3–11.4 wt.% ThO 2 ). The latter represents a NaNbO 3 –CaTiO 3 –Na 2/3 Th 1/3 TiO 3 –ThTi 2 O 6 solid solution. Late Na-rich silicate glass contains celsian. Slag from Araxá also consists of a framework of β-alumina (Ti-poor). Interstitial compounds differ from Fen in being predominantly rare-earth element (REE)-Nb-Al-Th-perovskites belonging to a REEAlO 3 –Ca 2 AlNbO 6 –CaTiO 3 –ThTi 2 O 6 solid solution with minor NaNbO 3 and CaZrO 3 , and compositionally diverse barium calcium aluminates [(Ba, Ca)Al 2 O 4 ] set in a F-bearing (6–7 wt.%) Na-Ba-Si-aluminate glass with minor Ba 4 Nb 2 O 9 , CaF 2 , BaF 2 and NaF. Slag from Oka consists of a framework of hibonite [(Ca, REE) (Al, Ti, Mg) 12 O 19 ] zoned with respect to the REE content. Interstitial compounds are CaZr 4 O 9 , Nb-Th-poor perovskites belonging to the REEAlO 3 –CaTiO 3 series with minor CaZrO 3 set in a F-bearing (5–6 wt.%) calcium aluminate glass. These data demonstrate that during ferroniobium production REE, Zr, Th, U and significant amounts of Nb are sequestered in the oxide phases in accord with their lithophile geochemical character. None of these elements are present as compounds in the siderophillic ferroniobium alloys. These data demonstrate that the aluminothermic reduction process results in the loss of significant amounts of Nb to the slag. Perovskite-group compounds are present in all of the slags but differ widely in their composition as a result of compositional differences in the feed pyrochlores and fluxes added to the smelting process. Slags originating from ferroniobium production are enriched in Th and U and could be considered as an environmental hazard if these elements are mobilized during chemical weathering of slag.

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How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.077
Threshold uncertainty score0.823

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.010
GPT teacher head0.223
Teacher spread0.212 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designBench or experimental
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

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Citations6
Published2016
Admission routes3
Has abstractyes

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