Silicates

thumb|class=skin-invert-image|Structure of the orthosilicate (ion)|orthosilicate anion |250px

residue of coal combustion

color

chemical compound

type of ceramic

aqueous solution of sodium, potassium and lithium silicates

ternary chemical compound of Al, Si, and O

range of refractory clays used in the manufacture of ceramics

thumb|SEM image of a geopolymer granule prepared from metakaolin by alkaline activation to be further used as a sorbent. A geopolymer is an inorganic, often ceramic-like material, that forms a stable, covalently bonded, non-crystalline to semi-crystalline network through the reaction of aluminosilicate materials with an alkaline or acidic solution. Many geopolymers may also be classified as alkali-activated cements or acid-activated binders. They are mainly produced by a chemical reaction between a chemically reactive aluminosilicate powder e.g. metakaolin or other clay-derived powders, natura

chemical compound

block of ceramic material used in lining furnaces, kilns, fireboxes, and fireplaces

chemical compound

chemical compound

hygroscopic chemical compound of variable Na2O/SiO2 ratio precursor of waterglass

liquid mixture or slurry of clay and/or other materials suspended in water

Expansive chemical reaction damaging concrete

chemical compound

chemical compound

Almasilate is an antacid. It is available in Japan as a mixture with calcium carbonate, and sodium bicarbonate as a non-prescription medication. It is also sold in Taiwan, Germany, and Spain.

Garronite-Ca is a fairly rare silicate mineral, from the zeolite, which has been found in a few dozen locations in the world. It was first found in the Glenariff Valley, Garron Plateau, County Antrim, Northern Ireland, and in some locations in Iceland. The name comes from the town of Garron, in Northern Ireland, which is consequently considered its type locality. The name initially used was that of Garronite, without subfixes, but the discovery in 2015 of a garronite with dominant sodium instead of calcium in the position of interchangeable cations made it necessary to use subfixes, remaining

chemical compound

Alite is an impure form of tricalcium silicate, , sometimes formulated as ( in cement chemist notation), typically with 3-4% of substituent oxides. It is the major, and characteristic, phase in Portland cement. The name was given by Alfred Elis Törnebohm in 1897 to a crystal identified in microscopic investigation of Portland cement. Hatrurite is the name of a mineral that is substituted .

chemical compound

Belite is an industrial mineral important in Portland cement manufacture. Its main constituent is dicalcium silicate, Ca2SiO4, sometimes formulated as 2 CaO · SiO2 (C2S in cement chemist notation).

chemical compound

artificial barium copper silicate pigments developed in ancient China during the Han dynasty

chemical compound

190px|right|thumb|Structure of the anion In chemistry, orthosilicate is the anion , or any of its salts and esters. It is one of the silicate anions. It is occasionally called the silicon tetroxide anion or group.