Natural zeolite is a kind of shelf silicate mineral, which is very widely distributed in the earth's crust. At present, zeolite deposits have been found in more than 40 countries in the world, including the United States, Japan and Russia, and the total number of deposits reaches more than 1,000, and more than 40 kinds of zeolites have been found.

Natural zeolite is a kind of shelf silicate mineral, which is very widely distributed in the earth's crust. At present, zeolite deposits have been found in more than 40 countries in the world, including the United States, Japan and Russia, and the total number of deposits reaches more than 1,000, and more than 40 kinds of zeolites have been found.

Zeolites have a shelf-like structure, in which molecules are linked together like a frame in the crystal, forming many cavities in the middle. Because there are many water molecules in these cavities, they are water-bearing minerals. The water in the zeolite can escape, but this does not destroy the internal crystal structure of the zeolite.

Deep nitrogen and phosphorus removal from wastewater is an important measure for the reuse of municipal wastewater resources and water pollution control.

Mercerized zeolite, also known as luminous zeolite. It is one of the main mineral components of zeolite ore. It is in the plagioclase system, with needle-like and fibrous crystals and bundled and radiating aggregates. White, light yellow or rose color. Silky luster or glassy luster.

Zeolite is a water-reticulated aluminosilicate of alkali and alkaline earth metals, a generic term for the zeolite family of minerals, first discovered in Europe in 1756. The mineralogist Kronsti in Sweden found a class of natural silica-aluminate ores that would boil when burned, hence the name "ze