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High Resolution Physical Characterization of Single Metallic Nanoparticles
Published on: June 28, 2019
Polyoxometalate clusters in minerals: review and complexity analysis.
1Department of Crystallography, Institute of Earth Sciences, St. Petersburg State University, University Emb. 7/9, St. Petersburg, 199034, Russian Federation.
Newly discovered polyoxometalates (POMs) in minerals reveal unique geochemical importance and structural complexity. These natural POMs, found in 42 mineral species, expand our understanding beyond synthetic compounds.
Area of Science:
- Mineralogy and Crystallography
- Geochemistry
- Inorganic Chemistry
Background:
- Research on polyoxometalates (POMs) has predominantly focused on synthetic compounds.
- Recent mineralogical discoveries highlight the natural occurrence and significance of POMs in geochemical systems.
- The structural diversity of naturally occurring POMs in minerals is less explored compared to synthetic analogues.
Purpose of the Study:
- To document and analyze the types and diversity of polyoxometalate nanoscale clusters found in mineral structures.
- To compare the topological and chemical characteristics of natural POMs with their synthetic counterparts.
- To investigate the unique coordination environments and structural complexity arising from POMs in minerals.
Main Methods:
- Systematic review and description of 15 distinct types of POM nanoscale clusters identified in 42 mineral species.
- Comparative analysis of topological diversity between natural and synthetic POM clusters.
- Examination of specific mineral structures (e.g., vanarsite, bouazzerite, ewingite) to identify and characterize metal-oxo clusters and coordination geometries.
- Complexity analysis of mineral structures containing POMs.
Main Results:
- Fifteen types of POM nanoscale clusters are identified in 42 mineral species, with restricted topological diversity compared to synthetic POMs.
- Several natural POMs, including those in vanarsite-group minerals, bouazzerite, whitecapsite, putnisite, and ewingite, exhibit unique metal-oxo clusters without direct synthetic analogues.
- Unusual metal atom coordination (e.g., cubic, trigonal prismatic) is observed in minerals due to topological constraints.
- Ewingite and morrisonite are identified as the most structurally complex minerals known, with POM cluster formation as a key driver of complexity.
Conclusions:
- The discovery of POMs in minerals is a significant advancement in mineralogy and crystallography, revealing their geochemical relevance.
- Natural POMs present unique structural motifs and coordination environments not found in synthetic chemistry.
- The formation of POM clusters is a fundamental mechanism for generating structural complexity in crystalline inorganic compounds, both natural and synthetic.
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