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Silicates/Titanates

Stock No.
NS6130-12-001801
CAS
12060-00-3
MSDS
MSDS-PDF
Specifications
SPEC-PDF
COA
COA-PDF
Catalogue

Lead Titanate Powder

(PbTiO3, Purity: 99%, APS: 1-3µm)
Lead Titanate Powder
Available Pack Size: 10Gms, 25Gms, 50Gms, 100Gms, 250Gms, 500Gms, 1Kg & Bulk orders
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ProductLead Titanate Powder
Stock No.NS6130-12-001801
CAS12060-00-3Confirm
Purity99%Confirm
APS1-3µmConfirm
Molecular FormulaPbTiO3Confirm
Molecular Weight303.07g/ molConfirm
FormPowderConfirm
Density7.52g/ml at 25°CConfirm
Quality ControlEach Lot of Lead Titanate Powder was tested successfully
Main Inspect VerifierManager QC

Typical Chemical Analysis

Purity99%
Total Metal Impurities8500ppm

Expert Reviews

product-expert-image
Dr. Baron Augustin, Ph.D (Technical University of Munich, Germany)

The silicates are the largest, the most interesting and the most complicated class of minerals than any other minerals. Approximately 30% of all minerals are silicates and some geologists estimate that 90% of the Earth's crust is made up of silicates, SiO44- based material. Thus, oxygen and silicon are the two most abundant elements in the earth's crust.

product-expert-image
Dr. Darren Chandler, Ph.D (Manchester Metropolitan University, U.K)

Silicates is based on the basic chemical unit SiO44-, tetrahedron shaped anionic group. The central silicon ion has a charge of positive four while each oxygen has a charge of negative two (-2) and thus each silicon-oxygen bond is equal to one half (½ ) the total bond energy of oxygen. This condition leaves the oxygens with the option of bonding to another silicon ion and therefore linking one SiO44- tetrahedron to another.

product-expert-image
Dr. Ms. Cristiana Barzetti (University of Cagliari-Department of Chemical Engineering and Material Science, Italy)

At very high pressures, silicon may adopt octahedral coordination, in which each silicon atom is directly attached to six oxygen atoms. This structure occurs in the dense stishovite polymorph of silica found in the lower mantle of the Earth, and it is also formed by shock during meteorite impacts.

product-expert-image
Dr. Jang Huang, Ph.D (Shandong Science and Technology University, China)

There are two forms of silicates:Felsic-The fel stands for feldspar while the sic represents silica. They form in granites and are lighter in weight and color than other silicates because they have less iron and magnesium. Quartz, micas, and the K-feldspars are noteable members of this group.Mafic- Ma stands for magnesium and fic is for iron (ferric). This group of silicates usually form in magmas moving up to fill the gap left when tectonic plates are moving away from each other in the sea floor. Basalt and gabbro are of this type. Olivine and pyroxene are also in this group. They are relatively dense and dark.

product-expert-image
Dr. Mark Brown  (Georgia Institute of Technology in Atlanta,USA)

A modern approach to classifying silicates is by their structure. This class of minerals uses SiO4 molecules connected as tetrahedrons. A tetrahedron is a triangular based pyramid. The oxygen atoms occupy the corners of the tetrahedron with the silicon atom in the center.The arrangement of this basic shape is the basis for classification. There are six subclasses. They are:NesoSilicates (Single Tetrahedrons), SoroSilicates (Double Tetrahedrons), InoSilicates( Single& Double Chains), CycloSilicates ( Rings), PhylloSilicates ( Sheets), TectoSilicates (Frameworks).

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Lead Titanate Powder

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