time:2024-05-21 17:42:12 Click number:1102
Description
Zirconium sand, also known as zircon sand, is a mineral composed mainly of zirconium silicate. Pure zircon sands are colorless transparent crystals, often dyed yellow, orange, red, and brown due to different origins and impurities. The crystalline structure belongs to the tetragonal crystalline system. The crystalline structure is tetragonal cone-columnar with a specific gravity of 4.6-4.71. The refractive index is 7~8, and the refractive index is between 1.3 and 2.0. The melting point fluctuates at 2190~2420 C with the impurity.
Zircon is a mineral consisting mainly of zirconium, silicon, and oxygen crystallized from magma during igneous rock formation. Zircon is also found in dikes and metamorphic rocks. It is a tetragonal system, usually a well-developed pyramidal small tetragonal cylinder and irregular granular. Crispy and factoid. It is a high-quality refractory material. Most coexist with ilmenite, rutile, monazite, and yttrium phosphate rock in seashore sand and are obtained by water separation, electric separation, and magnetic separation.
The regional distribution of zirconium reserves is highly concentrated, and the zirconium reserves are mainly distributed in Australia, South Africa, and other countries, and the distribution is highly concentrated. From the perspective of regional distribution of zirconium resources, the world zirconium reserves are mainly in the hands of Australia, South Africa, Ukraine, India, and Brazil. Five countries occupy 86%of the world’s zirconium resources, and the monopoly is obvious. According to the US Geological Survey, China’s zirconium ore reserves are only 500 thousand tons, accounting for less than 1%of the world’s Zirconium resources. Output growth is moving steadily, and the supply structure is changing.
Zircon sand is extremely resistant to high temperatures with a melting point of 2750 degrees Celsius. And acid corrosion resistance.80%of the world is directly used in casting, ceramics, glass, and refractories. A small amount is used in ferroalloys, pharmaceuticals, paints, tanning, abrasives, chemical, and nuclear industries. A very small amount of used for smelting zirconium.
High-quality zircon and other adhesives have good adhesion and are used in the foundry industry. Zircon sand is also used as a brick for glass kilns. Zircon sand and zircon powder are mixed with other refractory materials for other uses.
Zirconium in metallic form is mainly used in the chemical and nuclear reactor industries and in other industries requiring corrosion resistance, high-temperature resistance, special fusion properties, or the absorption of special neutrons. In the United States, about 8%of the total consumption of zirconium is used in these industries, and the only meaningful application of hafnium metal is in Naval Nuclear reactors.
Zircon Sand Process
Zircon sand processing plant is the process of removing impurities from zircon ores and increasing zircon content. Zircon(also known as zirconium)is zirconium orthosilicate. Its chemical formula is ZrSiO4.It is one of the most common zirconium-bearing minerals. The zircon ore deposits are mostly seashore placer deposits. Heavy minerals such as magnetite, ilmenite, rutile, and monazite are usually associated with zircon-bearing sands. The heavy minerals are generally recycled as the target minerals when the zircon is selected.
Gravity separation, magnetic separation, electrostatic separation, and flotation are often used in the zircon sand processing plant.
Zircon occurs in ilmenite and is often accompanied by hematite, chromite, garnet, and other heavy minerals. Therefore, gravity separation is often used in the initial stage of zircon enrichment, such as shaking table to separate heavy minerals from gangue(quartz, feldspar, biotite)and other heavy minerals.
Commonly used collectors are fatty acids(oleic acid, sodium oleate), the slurry regulator is sodium carbonate, the inhibitor is sodium silicate, the activator is sodium sulfide, and heavy metal salts(zirconium chloride, ferric chloride). Oxalic acid is also used to adjust the pulp to acid and flotation with amine collectors.
The conductive minerals, such as ilmenite, hematite, chromite, cassiterite, and rutile, are separated from the non-conductive minerals such as zircon, monazite, garnet, and apatite by using the difference of conductivity of minerals. Before deselecting, desliming, drying and dosing should be done.
Heavy minerals in the magnetic minerals are ilmenite, hematite, chromite, garnet, biotite, monazite, and so on. Zircon is a non-magnetic mineral or a weakly magnetic mineral. Magnetic separation is divided into two types: dry type and wet type. The dry magnetic separation must be preheated before drying and grading. The wet magnetic separator has a wide particle size and a lower particle size of 20um. Therefore, the wet magnetic separator is more suitable when the zircon particle size is fine.
Because there are many associated minerals in zircon sand, it is necessary to combine gravity separation, magnetic separation, flotation, and electrostatic separation.
The zircon sand concentrator is often divided into two parts: wet treatment and dry treatment. In the wet treatment stage, gangue minerals such as quartz, feldspar, and mica are removed by gravity separation equipment such as a cone concentrator, spiral concentrator, shaker, or jig.
The heavy minerals (crude concentrate) obtained are further separated by 2-4 stages of concentrating to remove the remaining light minerals and then concentrated, dehydrated, dried, cooled, and sent to the dry treatment stage for further separation.
The dry processing section generally comprises weak magnetic separation, high-intensity magnetic separation, and electrostatic separation. Where to buy magnetic separators?
The aim is to recover magnetite, ilmenite, rutile, and monazite associated with zircon. Magnetite can be recovered by weak magnetic separation, ilmenite and garnet can be recovered by strong magnetic separation, and a high-voltage electrostatic separator can separate monazite, rutile, and zircon.