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- Pyrochlore - Wikipedia
Pyrochlores are an important class of materials in diverse technological applications such as luminescence, ionic conductivity, nuclear waste immobilization, high-temperature thermal barrier coatings, automobile exhaust gas control, catalysts, solid oxide fuel cell, ionic electrical conductors etc
- Pyrochlore | Structure, Properties, Uses | Britannica
Pyrochlore, a complex oxide mineral [ (Na, Ca)2Nb2O6 (OH,F)] composed of niobium, sodium, and calcium that forms brown to black, glassy octahedral crystals and irregular masses
- Pyrochlore Group: Mineral information, data and localities.
The pyrochlore group gets its name from the generic name pyrochlore which was first introduced by J J Berzelius for a cubic mineral found by N O Tank in the 1820s in a syenite pegmatite at Stavern (formerly Fredriksvärn), Norway (Wöhler 1826)
- Pyrochlore - an overview | ScienceDirect Topics
Pyrochlore refers to a class of complex oxides characterized by their unusual physical properties and intricate crystal structures, which require thorough understanding of their electronic and geometrical configurations to explain their fundamental spectroscopic and thermodynamical behaviors
- Cava Lab: Pyrochlore - Princeton University
The general formula for Pyrochlore is A 2 B 2 O 7, or more accurately: A 2 B 2 O 6 O' In the case of nominal pyrochlore, F occupies the F' site Pyrochlore is highly symmetric, and is face-centered
- Pyrochlore (Ca, Na)2Nb2O6(OH, F) - Handbook of Mineralogy
Polymorphism Series: Forms a series with microlite Mineral Group: Pyrochlore group and subgroup; (Na + Ca)
- The Chemistry of Pyrochlores: A Deep Dive
In this article, we will explore the intricate chemistry behind pyrochlores, including their synthesis, properties, and applications Pyrochlores have a complex crystal structure that is characterized by a network of corner-sharing octahedra
- Pyrochlore - Rock of Science
Name: The pyrochlore group gets its name from the generic name pyrochlore which was first introduced by J J Berzelius for a cubic mineral found by N O Tank in the 1820s in a syenite pegmatite at Stavern (formerly Fredriksvärn), Norway (Wöhler 1826)
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