Quartz Sand

SiO2 is one of the known and most common minerals. Quartz sand is formed as a result of weathering of igneous, metamorphic rocks rich in quartz. They are quartz (SiO2) particles smaller than 2 mm. Quartz sand consists of the most important minerals because it is resistant to both physical and chemical weather conditions. They can be found in nature as pure or as a mixture.

Characteristics of Quartz Sand ; Quartz sands are divided into two in terms of their formation. The first consists of the allochthon formation, which is called the formation of quartz, which is released as a result of the decomposition of igneous and metamorphic rocks, carried away and stacked with a loose cement with clay. The second is autochthonous formation. These are formed by the in situ weathering of silica-rich rocks under the influence of a faulting or metamorphism. This type of quartz sand contains less impurity than the allochthonous formation. It is less costly than its alternatives, as it can occur at any temperature value and is widely available in the world.

In glass production: as a raw material, in the production of silica bricks: as a durable material, as a slag maker: quartz sand, in the production of silicon and ferro-silicon: quartz sand, In the production of aerated concrete: quartz sand, in the production of pressed bricks: quartz sand, frit and glaze In the production: quartz sand, in ceramic mud: quartz sand is used.

Where to Use Quartz Sand: