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Record W2061739512 · doi:10.3749/canmin.46.6.1555

THE CRYSTAL CHEMISTRY OF THE SCAPOLITE-GROUP MINERALS. II. THE ORIGIN OF THE I4/m   P42/n PHASE TRANSITION AND THE NONLINEAR VARIATIONS IN CHEMICAL COMPOSITION

2008· article· en· W2061739512 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
venuePublished in a venue whose home country is Canada.

Bibliographic record

VenueThe Canadian Mineralogist · 2008
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of Manitoba
Fundersnot available
KeywordsGroup (periodic table)Phase transitionPhase (matter)Chemical compositionChemistryCrystal chemistryCrystallographyCrystal structureMineralogyCondensed matter physicsPhysicsOrganic chemistry

Abstract

fetched live from OpenAlex

The scapolite structure consists of two interpenetrating frameworks: [(Si,Al)12O24] and {Na,Ca}{Cl,(CO3)}. The unstrained dimensions of each framework are significantly different (as determined by the valence-matching principle and distance-least-squares refinement); there is an intrinsic steric stress between the two frameworks, the magnitude of which is a function of chemical composition. Evidence of the resulting structural strain is the large U eq values for Cl at the A site across the marialite–meionite series and the large U eq values for (Na,Ca) at the M site in marialite. Local bond-valence considerations indicate extensive SRO (Short-Range Order) about both Cl and (CO3). The short-range bond-valence requirements of the (CO3) group are satisfied by coordination with Ca4 at ~ Me 100, NaCa3 at ~ Me 80, Na2Ca2 at ~ Me 55, Na3Ca at ~ Me 40, and Na4 at ~ Me 20. The driving mechanism for the I 4/ m → P 42/ n phase-transitions is the coupling of SRO between the [(Si,Al)12O24] and {Na,Ca}{Cl,(CO3)} frameworks. At a composition of ~ Me 50, local bond-valence requirements force the local clusters Na2Ca2 to occur in a trans configuration {NaCaNaCa} around the A site. Anion bond-valence requirements also force these clusters to link to each other through Na–O–Na or Ca–O–Ca linkages, and hence the combination of SRO and bond-valence requirements gives rise to LRO (long-range order). In turn, Al and Si are constrained to order at different tetrahedra, an ordering that breaks the topological I 4/ m symmetry and gives rise to two distinct tetrahedra, T (2) and T (3), dominated by Al and Si, respectively. The result is the P 42/ n scapolite structure. As Na or Ca become dominant, the number of Na2Ca2 clusters decreases, the effectiveness of the symmetry-lowering mechanism lessens, and the degree of order of Al and Si over the T (2) and T (3) sites decreases toward both the marialite and meionite ends of the series. At the compositions ~ Me 22 and Me 78, the clusters NaCa3 and Na3Ca dominate, the driving mechanism for lower symmetry vanishes, and the structures revert to maximal I 4/ m symmetry. The nonlinear variations in bulk composition across the marialite–meionite series are also the result of SRO of M -site Na and Ca around the A site [which is occupied by Cl in end-member marialite and (CO3) in end-member meionite]. Local bond-valence requirements indicate extensive SRO about both Cl and (CO3) in scapolite. In particular, Cl cannot occur in I 4/ m meionite except where K is present; in this case, chemical variations indicate that Cl enters the I 4/ m meionite structure as {ClK2Ca2} clusters.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

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)0.001
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 score0.229
Threshold uncertainty score0.986

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.003
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.013
GPT teacher head0.222
Teacher spread0.209 · 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