THE SYMMETRY AND CRYSTAL STRUCTURE OF GORCEIXITE, BaAl3[PO3(O,OH)]2(OH)6, A MEMBER OF THE ALUNITE SUPERGROUP
Bibliographic record
Abstract
The crystal structure of the Ba–Al phosphate mineral gorceixite, a 7.0538(3), c 17.2746(6) A, V 744.4(2) A 3 , space group R 3 m , Z = 3, has been refined to an R 1 index of 2.3% on the basis of 253 unique reflections measured using Mo K α radiation on an automated single-crystal diffractometer. The specimen, from the Rapid Creek area, Yukon Territory, has rhombohedral rather than monoclinic Cm symmetry previously reported for the species. The crystal-structure refinement shows that the atomic arrangement of gorceixite is similar to that of other members of the alunite supergroup. The Ba–O and Ba–OH distances are 2.825 and 2.859 A (both ×6), respectively, and the volume of the Ba(O,OH) 12 polyhedron is 55.64 A 3 . Energy-dispersion spectra and electron-microprobe analyses indicate that the site is completely occupied by Ba, but the site occupancy refines to 88% occupancy; the reason for this is unclear. The average Al–O,OH and P–O distances are 1.906 and 1.544 A, respectively, and the OH–H distance is 0.980 A. Interatomic distances [H…O(2) = 1.904 A and OH…O(2) = 2.884 A] and a bond-valence analysis suggest that each O(2) atom is involved in hydrogen bonding (as an acceptor) with three different OH groups. However, the low bond-valence sum for O(2) suggests that it not only acts as an acceptor but functions as a donor as well. No hydrogen-atom sites could be identified from the difference-Fourier map, but the presence of OH groups at the O(2) site would help resolve the problem of charge balance. Assuming equal occupancy of the O(2) site by O and OH, the general formula of gorceixite is BaAl 3 [PO 3 (O,OH)] 2 (OH) 6 . Although R 3 m is the most appropriate space-group for the gorceixite sample studied here, we do not claim that all gorceixite samples crystallize in this space group. Different conditions of formation and compositions might be responsible for the lower symmetry observed previously, but the mechanism to achieve the symmetry lowering remains unclear.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.001 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.001 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.001 | 0.000 |
| Open science | 0.001 | 0.000 |
| Research integrity | 0.000 | 0.001 |
| Insufficient payload (model declined to judge) | 0.002 | 0.001 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".