Distinct local environments for Ca along the non-ideal pyrope–grossular solid solution: A new model based on crystallographic and EXAFS analysis |
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| Institution: | 1. IMPMC, CNRS-UMR 7590, Université Pierre et Marie Curie, IRD, MNHN, T 23-24, 5ème étage, 4 Place Jussieu, 75252 Paris, France;2. IC2MP, CNRS-UMR 7285, Université de Poitiers, Bâtiment B35, 6 Rue Michel Brunet, TSA 51106, 86073 Poitiers Cedex 9, France;3. AREVA Resources Canada Inc., 810 45th Street West, Saskatoon, Saskatchewan S7K 3X5, Canada |
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| Abstract: | A multi-technique approach (based on electron microprobe analysis, structure refinement, and EXAFS analysis at the Ca K-edge) was used to characterise the local geometry of Ca in synthetic and natural garnet compositions referable to the pyrope–grossular solid solution. Multi-shell fits of the EXAFS data indicate that Ca assumes the standard 4 + 4]-fold coordination (the polyhedral shape being a triangular dodecahedron with Ca1–O = 2.30–2.31(1) and Ca2–O = 2.45–2.46(1) Å) when Ca > 1.50 atoms per formula unit (apfu), but assumes a nearly regular 8]-fold coordination with Ca–O = 2.35–2.36 (1) Å when (Mg, Fe2+, Mn2+) > 1.50 apfu. Therefore, in the pyrope-dominant structure the Ca1–O distance lengthens and the Ca2–O distance shortens to converge towards the value observed for the Mg2–O bond in pyrope. This finding is consistent with many distinct structural features observed in solid solution terms with (Mg, Fe2+, Mn2+) > 1.50 apfu or Ca > 1.50 apfu, as well as with the anomalous properties of the intermediate terms observed both in the short-range and in the long-range perspective. The presence of two distinct Ca coordinations in the pyrope (almandine, spessartine)-like and in the grossular-like structure, and thus of an isosymmetric transition at the intermediate composition, can help to explain both the strong and asymmetric non-ideality of the solid solution between pyrope (almandine) and grossular, as well as the differences in the ability to incorporate some trace elements (such as REE and actinides) which are commonly used as process-specific indicators. This feature must be taken into account when building theoretical models of the garnet solid solutions, which are at the moment the most promising approach for calculating thermodynamic properties or for interpreting and predicting trace-element behaviour in this crucial mineral phase. |
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