383287
Zirconium(IV) silicate
−325 mesh
Synonyme(s) :
Zirconium(IV) silicon oxide
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About This Item
Produits recommandés
Forme
powder
Pertinence de la réaction
core: zirconium
Taille des particules
−325 mesh
Chaîne SMILES
[Zr+4].[O-][Si]([O-])([O-])[O-]
InChI
1S/O4Si.Zr/c1-5(2,3)4;/q-4;+4
Clé InChI
GFQYVLUOOAAOGM-UHFFFAOYSA-N
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Caractéristiques et avantages
Often cited as a potential alternative gate dielectric to silica.
Code de la classe de stockage
11 - Combustible Solids
Classe de danger pour l'eau (WGK)
WGK 3
Point d'éclair (°F)
Not applicable
Point d'éclair (°C)
Not applicable
Équipement de protection individuelle
dust mask type N95 (US), Eyeshields, Gloves
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Journal of oral rehabilitation, 36(3), 226-235 (2008-11-04)
The aim of this randomized controlled clinical trial was to evaluate over a 5-year period, the clinical outcome of shrinkage-free ZrSiO(4)-ceramic (KaVo Everest HPC) full coverage crowns on posterior teeth in comparison with conventional gold crowns that served as the
Journal of dentistry, 40(9), 723-735 (2012-05-23)
The aim of this study was to characterize the surface of Y-TZP after abrasion with various airborne particles. The Y-TZP blanks were cut into 44 discs and sintered according to the manufacturer's instructions. The specimens were treated as follows: (a)
Radiation protection dosimetry, 145(4), 400-404 (2010-12-15)
Zircon contains small amounts of uranium, thorium and radium in its crystalline structure. The ceramic industry is one of the major consumers of zirconium compounds that are used as an ingredient at ∼10-20 % by weight in glaze. In this
Science (New York, N.Y.), 340(6135), 941-945 (2013-03-23)
The end-Triassic extinction is characterized by major losses in both terrestrial and marine diversity, setting the stage for dinosaurs to dominate Earth for the next 136 million years. Despite the approximate coincidence between this extinction and flood basalt volcanism, existing
Journal of physics. Condensed matter : an Institute of Physics journal, 23(10), 105402-105402 (2011-02-23)
Iron is a ubiquitous impurity in metamict (radiation-damaged and partially amorphized) materials such as titanite (CaSiTiO(5)). Using (57)Fe Mössbauer spectroscopy we find that iron in metamict titanite is partitioned between amorphous and crystalline regions based on valence. Trivalent iron exists
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