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Calcium-lead fluoro-vanadinite apatites. I. Disequilibrium structures
1Centre for Advanced Research of Ecomaterials, Institute of Environmental Science and Engineering, Innovation Centre, Nanyang Technological University, Block 2, Unit 237, 18 Nanyang Drive, Singapore 637723, Singapore. zldong@ntu.edu.sg
This study explores how calcium and lead arrange in synthetic vanadinite apatites. Using high-resolution electron microscopy, researchers found that lead prefers larger sites in the crystal structure. They observed that even after prolonged heating, microdomains of calcium and lead coexist at the unit-cell level. As lead content increases, the apatite structure adjusts to accommodate it. The prism twist angle phi is a sensitive indicator of these structural changes. The findings suggest that structural parameters can track disequilibrium and monitor apatite topology changes with composition.
Area of Science:
- Mineralogy and crystallography
- Materials science and solid-state chemistry
- Geochemical phase relations
Background:
Studying mineral structures helps understand how elements arrange in solids. Some minerals form under non-equilibrium conditions. This gap motivated researchers to explore how composition affects crystal structures. Prior research has shown that apatite structures accommodate various cations. However, no prior work had resolved how lead and calcium partition in vanadinite apatites. The AI and AII sites in apatites vary in size. Lead's preference for larger sites is already known. This paper's contribution is to show how structural parameters change with composition.
Purpose Of The Study:
This work aims to investigate how calcium and lead distribute in vanadinite apatites. The specific problem is understanding how cation partitioning affects crystal structure. The motivation comes from the need to monitor structural changes due to composition. Researchers wanted to determine if apatite topology shifts with lead content. They also aimed to assess if structural parameters can detect disequilibrium. The study focuses on synthetic vanadinites with variable lead content. The goal is to relate structural adjustments to macroscopic ordering. The authors propose that electron microscopy can reveal microdomain coexistence.
Main Methods:
The study used synthetic vanadinites with varying lead content. These compounds were analyzed using high-resolution electron microscopy. Researchers measured unit-cell dimensions and site occupancies. They examined samples after different annealing durations. The focus was on calcium and lead distribution in AI and AII sites. Structural parameters like c/a ratio and prism twist angle were tracked. Researchers observed changes in apatite channels with composition. The methods included sintering and electron diffraction to assess ordering.
Main Results:
The vanadinites formed a P6(3)/m apatite structure with variable unit-cell sizes. Lead preferentially occupied the larger AII site over AI. Microdomains of calcium and lead coexisted at unit-cell scales. Annealing for 10 hours at 1073 K did not achieve equilibrium. For (Pb5Ca5)(VO4)6F2delta, sintering over two weeks was needed for ordering. As lead content increased, the apatite channel expanded. The c/a ratio, partitioning coefficient, and prism twist angle adjusted cooperatively. These findings suggest that structural parameters track disequilibrium.
Conclusions:
The study demonstrates that lead distribution affects apatite topology. Structural parameters like c/a ratio and prism twist angle change with composition. These adjustments help accommodate higher lead content. The prism twist angle phi is a sensitive indicator of disequilibrium. Researchers propose that phi can monitor structural changes in apatites. The findings suggest that microdomains persist even after prolonged annealing. The study confirms that lead prefers larger AII sites over AI. The results support the idea that apatite structures adapt to cation content.
Frequently Asked Questions
As lead content increases, the apatite channel expands. The c/a ratio, partitioning coefficient, and prism twist angle adjust cooperatively.
Lead preferentially occupies the larger AII site over the AI site. This partitioning is nonstoichiometric.
Phi is sensitive to disequilibrium and tracks apatite topology changes as a function of composition.
It reveals coexisting calcium- and lead-rich microdomains at unit-cell scales in disequilibrium samples.
For (Pb5Ca5)(VO4)6F2delta, sintering in excess of 2 weeks is required for metals to order macroscopically.
The study suggests that apatite structures adapt to cation content through cooperative adjustments in structural parameters.
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