Powder #6183988

Aluminum spherical powder for high-quality metallic paints, compounds (metal composite powder spraying ceramic thermal composite pipe), military, aerospace, chemical (various chemical catalysts, pesticides), metallurgy, refractories 8, new building materials (gas agents aerated concrete). ), anticorrosion materials, fireworks, etc.

Spherical aluminum powder applications

combustion catalyst: in combination with other substances, aluminum powder serves as an excellent catalyst for combustion, greatly improving the stability of speed, heat, and combustion of fuel for missiles and other fuels. The combustion rates can be increased up to 20 times with the correct application of nanopowders.

Drug Administration: As with many nanoparticles, aluminum nanopowders play a role in a variety of new drug delivery systems, including dry and aerosol transdermal administration.

Resistance to wear and corrosion: aluminum powders can be added to various coatings or can include compounds to increase overall wear and corrosion resistance. In particular, it can be used to produce wear-resistant transparent coatings.

chemical applications: aluminum nanopowder is widely used for its chemical properties to produce controlled reaction rates for the manufacture of chemicals, alcohols, and other aluminum-based substances. Deodorants and antiperspirants are a group of key products that this application uses.

Boron is a chemical element with the symbol B and atomic number 5. Produced in its entirety by cosmic spallation and supernova and not by stellar nucleosynthesis, it is an element of low abundance in the Solar System and in the earths crust. Boron concentrates on the Earth due to the water solubility of its most common natural compounds, borate minerals. These are industrially extracted as evaporites, such as borax and kernite. The largest known boron deposits are in Turkey, the largest producer of boron minerals.

Elemental boron is a metalloid found in small amounts in meteorites, but not chemically combined boron is not naturally found on Earth. The industrially very pure boron presents with difficulty due to the refractory contamination from carbon or other elements. There are many boron allotropes: amorphous boron is a brown powder; Crystalline boron is silver to black, extremely hard (about 9.5 of the Mohs scale) and a faulty electrical conductor at room temperature. The primary use of elemental boron as boron filaments is similar to carbon fibers in some high-strength material applications.

Boron is mainly used in chemical compounds. About half of all boron consumed in the world is a glass fiber additive for insulation and structural materials. The next main use is in polymers and ceramics in structural materials and high strength light refractories. Borosilicate glass is required for its greater strength and resistance to thermal shock than normal glass soda lime. Boron as sodium perborate is used as a bleach. A small amount of boron is used as a dopant in semiconductors and reactive intermediates in the synthesis of fine organic chemicals. Some organic pharmaceutical products containing boron are used or are being studied. natural boron comprises two stable isotopes, one of which (born-10) has different uses as a neutron capture agent.

Cobalt powder (Co) is a chemical element with the symbol Co and atomic number 27. Like nickel, cobalt is found in the earths crust only in a combined chemical form, except for the small deposits that are found in alloys of iron natural methods. The free element, produced by reductive fusion, is a hard, shiny, silver-gray metal.

The blue pigments based on cobalt (cobalt blue) have been used since ancient times to make jewels and paintings and to give a blue note to the glass, but the alchemists thought that the color was due to the well-known metallic bismuth. Miners have long used the name of mineral kobold (German for goblin ore) for some of the minerals that produce the blue pigment; they were called because they were poor in known metals and emitted toxic fumes that contained arsenic when they melted. In 1735, it was discovered that such minerals were reducible to a new metal (the first discovered since antiquity), and this was eventually called by the kobold.

Copper is a chemical element with the symbol Cu (Latin: cuprum) and atomic number 29. It is a soft, malleable and ductile metal with high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish orange color. Copper is used as a conductor of heat and electricity, as a building material and as a component of various metal alloys such as Sterling silver used in jewelry, cupronickel used to make hardware and marine coins, and is constantly used in large gauges and thermocouples. For temperature measurement.

Copper is one of the few metals that can occur naturally in a metal that can be used directly (native metals). This led to very early human use in different regions, from c. 8000 BC Thousands of years later, it was the first fusion of sulfide, c metal ore. 5000 a. C., the first metal to be molded into a mold, c. 4000 BC and the first metal to be bound with another metal for purpose, tin, to create bronze, c. 3500 BC

Spherical Ferromagnetic iron powder / Fe spherical powder is composed of particles of high purity iron microspheres with unique electromagnetic properties for use in electronics, energy injection molding, sensors, and radiation protection. Ferromagnetic spherical powder in iron / spherical powder Fe used as probes for fundamental magnetic interactions; Iron spherical ferromagnetic powder / Fe spherical powder used. Data storage and magnetic media; Spherical ferromagnetic powder / spherical powder Fe used Iron liquids for vacuum rotating seals; Spherical ferromagnetic iron powder / spheric powder Fe used for biomedical applications such as magnetic separation and contrast agents for magnetic resonance; The iron ferromagnetic spherical powder / Fe spherical powder is also used in the environmental field; Ferromagnetic spherical iron powder / Fe Spherical powder used in the degradation of chlorinated hydrocarbons and hard metals in contaminated soils; Ferromagnetic spherical powder in iron / spherical powder Fe used for single electron transistors, absorption of electromagnetic waves, catalyst, medical applications

Iron is a chemical element with symbol Fe (from Latin: ferrum) and atomic number 26. It is a metal in the first transition series. It is by mass the most common element on Earth, forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. Its abundance in rocky planets like Earth is due to its abundant production by fusion in high-mass stars, where it is the last element to be produced with the release of energy before the violent collapse of a supernova, which scatters the iron into space.

Magnesium is a chemical element with symbol Mg and atomic number 12. It is a shiny gray solid which bears a close physical resemblance to the other five elements in the second column (group 2, or alkaline earth metals) of the periodic table: all group 2 elements have the same electron configuration in the outer electron shell and a similar crystal structure.

Magnesium is the ninth most abundant element in the universe. It is produced in large, aging stars from the sequential addition of three helium nuclei to a carbon nucleus. When such stars explode as supernovas, much of the magnesium is expelled into the interstellar medium where it may recycle into new star systems. Magnesium is the eighth most abundant element in the Earth's crust and the fourth most common element in the Earth (after iron, oxygen, and silicon), making up 13% of the planet's mass and a large fraction of the planet's mantle. It is the third most abundant element dissolved in seawater, after sodium and chlorine.

Silicon is a chemical element with symbol Si and atomic number 14. It is a hard and brittle crystalline solid with a blue-grey metallic luster, and it is a tetravalent metalloid and semiconductor. It is a member of group 14 in the periodic table: carbon is above it; and germanium, tin, and lead are below it. It is relatively unreactive. Because of its high chemical affinity for oxygen, it was not until 1823 that Jns Jakob Berzelius was first able to prepare it and characterize it in pure form. Its melting and boiling points of 1414 C and 3265 C respectively are the second-highest among all the metalloids and nonmetals, being only surpassed by boron. Silicon is the eighth most common element in the universe by mass, but very rarely occurs as the pure element in the Earth's crust. It is most widely distributed in dust, sands, planetoids, and planets as various forms of silicon dioxide (silica) or silicates. More than 90% of the Earth's crust is composed of silicate minerals, making silicon the second most abundant element in the Earth's crust (about 28% by mass) after oxygen.

Titanium is a chemical element with symbol Ti and atomic number 22. It is a lustrous transition metal with a silver color, low density, and high strength. Titanium is resistant to corrosion in sea water, aqua regia, and chlorine.

Titanium was discovered in Cornwall, Great Britain, by William Gregor in 1791, and was named by Martin Heinrich Klaproth after the Titans of Greek mythology. The element occurs within a number of mineral deposits, principally rutile and ilmenite, which are widely distributed in the Earth's crust and lithosphere, and it is found in almost all living things, water bodies, rocks, and soils. The metal is extracted from its principal mineral ores by the Kroll and Hunter processes. The most common compound, titanium dioxide, is a popular photocatalyst and is used in the manufacture of white pigments. Other compounds include titanium tetrachloride (TiCl4), a component of smoke screens and catalysts; and titanium trichloride (TiCl3), which is used as a catalyst in the production of polypropylene.

Vanadium is a chemical element with symbol V and atomic number 23. It is a hard, silvery-grey, ductile, malleable transition metal. The elemental metal is rarely found in nature, but once isolated artificially, the formation of an oxide layer (passivation) somewhat stabilizes the free metal against further oxidation.

Andrs Manuel del Ro discovered compounds of vanadium in 1801 in Mexico by analyzing a new lead-bearing mineral he called "brown lead", and presumed its qualities were due to the presence of a new element, which he named erythronium (derived from Greek for "red") since, upon heating, most of the salts turned red. Four years later, however, he was (erroneously) convinced by other scientists that erythronium was identical to chromium. Chlorides of vanadium were generated in 1830 by Nils Gabriel Sefstrm who thereby proved that a new element was involved, which he named "vanadium" after the Scandinavian goddess of beauty and fertility, Vanads (Freyja). Both names were attributed to the wide range of colors found in vanadium compounds. Del Rio's lead mineral was later renamed vanadinite for its vanadium content. In 1867 Henry Enfield Roscoe obtained the pure element.

Chromium is a chemical element with symbol Cr and atomic number 24. It is the first element in group 6. It is a steely-grey, lustrous, hard and brittle transition metal. Chromium boasts a high usage rate as a metal that is able to be highly polished while resisting tarnishing. Chromium is also the main additive in stainless steel, a popular steel alloy due to its uncommonly high specular reflection. Simply polished chromium reflects almost 70% of the visible spectrum, with almost 90% of infrared light waves being reflected. The name of the element is derived from the Greek word , chrma, meaning color, [6] because many chromium compounds are intensely colored.

Manganese is a chemical element with symbol Mn and atomic number 25. It is not found as a free element in nature; it is often found in minerals in combination with iron. Manganese is a metal with important industrial metal alloy uses, particularly in stainless steels.

Historically, manganese is named for pyrolusite and other black minerals from the region of Magnesia in Greece, which also gave its name to magnesium and the iron ore magnetite. By the mid-18th century, Swedish-German chemist Carl Wilhelm Scheele had used pyrolusite to produce chlorine. Scheele and others were aware that pyrolusite (now known to be manganese dioxide) contained a new element, but they were unable to isolate it. Johan Gottlieb Gahn was the first to isolate an impure sample of manganese metal in 1774, which he did by reducing the dioxide with carbon.

Nickel is a chemical element with symbol Ni and atomic number 28. It is a silvery-white lustrous metal with a slight golden tinge. Nickel belongs to the transition metals and is hard and ductile. Pure nickel, powdered to maximize the reactive surface area, shows a significant chemical activity, but larger pieces are slow to react with air under standard conditions because an oxide layer forms on the surface and prevents further corrosion (passivation). Even so, pure native nickel is found in Earth's crust only in tiny amounts, usually in ultramafic rocks, and in the interiors of larger nickel-iron meteorites that were not exposed to oxygen when outside Earth's atmosphere.

Meteoric nickel is found in combination with iron, a reflection of the origin of those elements as major end products of supernova nucleosynthesis. An iron-nickel mixture is thought to compose Earth's inner core.

Zinc is a chemical element with symbol Zn and atomic number 30. It is the first element in group 12 of the periodic table. In some respects zinc is chemically similar to magnesium: both elements exhibit only one normal oxidation state (+2), and the Zn2+ and Mg2+ ions are of similar size. Zinc is the 24th most abundant element in Earth's crust and has five stable isotopes. The most common zinc ore is sphalerite (zinc blende), a zinc sulfide mineral. The largest workable lodes are in Australia, Asia, and the United States. Zinc is refined by froth flotation of the ore, roasting, and final extraction using electricity (electrowinning).

Gallium is a chemical element with symbol Ga and atomic number 31. It is in group 13 of the periodic table and thus has similarities to the other metals of the group, aluminum, indium, and thallium. Gallium does not occur as a free element in nature, but as gallium(III) compounds in trace amounts in zinc ores and in bauxite. Elemental gallium is a soft, silvery blue metal at standard temperature and pressure, a brittle solid at low temperatures, and a liquid at temperatures greater than 29.76 C (85.57 F) (above room temperature, but below the normal human body temperature of 98.6 F (37.0 C), hence, the metal will melt in a person's hands).

Germanium is a chemical element with symbol Ge and atomic number 32. It is a lustrous, hard, grayish-white metalloid in the carbon group, chemically similar to its group neighbors silicon and tin. Pure germanium is a semiconductor with an appearance similar to elemental silicon. Like silicon, germanium naturally reacts and forms complexes with oxygen in nature.

Because it seldom appears in high concentration, germanium was discovered comparatively late in the history of chemistry. Germanium ranks near fiftieth in the relative abundance of the elements in the Earth's crust. In 1869, Dmitri Mendeleev predicted its existence and some of its properties from its position on his periodic table and called the element ekasilicon. Nearly two decades later, in 1886, Clemens Winkler found the new element along with silver and sulfur, in a rare mineral called argyrodite. Although the new element somewhat resembled arsenic and antimony in appearance, the combining ratios in compounds agreed with Mendeleev's predictions for a relative of silicon.

Selenium is a chemical element with symbol Se and atomic number 34. It is a nonmetal (more rarely considered a metalloid) with properties that are intermediate between the elements above and below in the periodic table, sulfur, and tellurium, and also has similarities to arsenic. It rarely occurs in its elemental state or as pure ore compounds in the Earth's crust. Selenium (from Ancient Greek (seln) "Moon") was discovered in 1817 by Jns Jacob Berzelius, who noted the similarity of the new element to the previously discovered tellurium (named for the Earth).

Yttrium is a chemical element with symbol Y and atomic number 39. It is a silvery-metallic transition metal chemically similar to the lanthanides and has often been classified as a "rare-earth element". Yttrium is almost always found in combination with lanthanide elements in rare-earth minerals and is never found in nature as a free element. 89Y is the only stable isotope, and the only isotope found in the Earth's crust.

In 1787, Carl Axel Arrhenius found a new mineral near Ytterby in Sweden and named it ytterbite, after the village. Johan Gadolin discovered yttrium's oxide in Arrhenius' sample in 1789, and Anders Gustaf Ekeberg named the new oxide yttria. Elemental yttrium was first isolated in 1828 by Friedrich Whler.

Zirconium is a chemical element with symbol Zr and atomic number 40. The name zirconium is taken from the name of the mineral zircon (the word is related to Persian zargun (zircon;zar-gun, "god-like" or "as gold")), the most important source of zirconium. It is a lustrous, grey-white, strong transition metal that closely resembles hafnium and, to a lesser extent, titanium. Zirconium is mainly used as a refractory and opacifier, although small amounts are used as an alloying agent for its strong resistance to corrosion. Zirconium forms a variety of inorganic and organometallic compounds such as zirconium dioxide and zirconocene dichloride, respectively. Five isotopes occur naturally, three of which are stable. Zirconium compounds have no known biological role.

Niobium, formerly known as columbium, is a chemical element with symbol Nb (formerly Cb) and atomic number 41. It is a soft, grey, crystalline, ductile transition metal, often found in the minerals pyrochlore and columbite, hence the former name "columbium". Its name comes from Greek mythology, specifically Niobe, who was the daughter of Tantalus, the namesake of tantalum. The name reflects the great similarity between the two elements in their physical and chemical properties, making them difficult to distinguish.

Molybdenum is a chemical element with symbol Mo and atomic number 42. The name is from Neo-Latin molybdaenum, from Ancient Greek molybdos, meaning lead, since its ores were confused with lead ores. Molybdenum minerals have been known throughout history, but the element was discovered (in the sense of differentiating it as a new entity from the mineral salts of other metals) in 1778 by Carl Wilhelm Scheele. The metal was first isolated in 1781 by Peter Jacob Hjelm.

Molybdenum does not occur naturally as a free metal on Earth; it is found only in various oxidation states in minerals. The free element, silvery metal with a gray cast, has the sixth-highest melting point of any element. It readily forms hard, stable carbides in alloys, and for this reason, most of the world production of the element (about 80%) is used in steel alloys, including high-strength alloys and superalloys.

Silver is a chemical element with symbol Ag (from the Latin Argentum, derived from the Proto-Indo-European her: "shiny" or "white") and atomic number 47. A soft, white, lustrous transition metal, it exhibits the highest electrical conductivity, thermal conductivity, and reflectivity of any metal. The metal is found in the Earth's crust in the pure, free elemental form ("native silver"), as an alloy with gold and other metals, and in minerals such as argentite and chlorargyrite. Most silver is produced as a byproduct of copper, gold, lead, and zinc refining.

Cadmium is a chemical element with symbol Cd and atomic number 48. This soft, bluish-white metal is chemically similar to the two other stable metals in group 12, zinc and mercury. Like zinc, it demonstrates oxidation state +2 in most of its compounds, and like mercury, it has a lower melting point than the transition metals in groups 3 through 11. Cadmium and its congeners in group 12 are often not considered transition metals, in that they do not have partly filled d or f electron shells in the elemental or common oxidation states. The average concentration of cadmium in Earth's crust is between 0.1 and 0.5 parts per million (ppm). It was discovered in 1817 simultaneously by Stromeyer and Hermann, both in Germany, as an impurity in zinc carbonate.

Indium is a chemical element with symbol In and atomic number 49. It is a post-transition metal that makes up 0.21 parts per million of the Earth's crust. Very soft and malleable, indium has a melting point higher than sodium and gallium, but lower than lithium and tin. Chemically, indium is similar to gallium and thallium, and it is largely intermediate between the two in terms of its properties. Indium was discovered in 1863 by Ferdinand Reich and Hieronymous Theodor Richter by spectroscopic methods. They named it for the indigo blue line in its spectrum. Indium was isolated the next year.

Tin is a chemical element with the symbol Sn (from Latin: stannum) and atomic number 50. It is a post-transition metal in group 14 of the periodic table of elements. It is obtained chiefly from the mineral cassiterite, which contains a stannic oxide, SnO2. Tin shows chemical similarity to both of its neighbors in group 14, germanium and lead, and has two main oxidation states, +2 and the slightly more stable +4. Tin is the 49th most abundant element and has, with 10 stable isotopes, the largest number of stable isotopes in the periodic table, thanks to its magic number of protons. It has two main allotropes: at room temperature, the stable allotrope is -tin, a silvery-white, malleable metal, but at low temperatures, it transforms into the less dense grey -tin, which has the diamond cubic structure. Metallic tin does not easily oxidize in air.

Antimony is a chemical element with symbol Sb (from Latin: stibium) and atomic number 51. A lustrous gray metalloid, it is found in nature mainly as the sulfide mineral stibnite (Sb2S3). Antimony compounds have been known since ancient times and were powdered for use as medicine and cosmetics, often known by the Arabic name, kohl.[4] Metallic antimony was also known, but it was erroneously identified as lead upon its discovery. The earliest known description of the metal in the West was written in 1540 by Vannoccio Biringuccio.

tantalum is a chemical element with symbol ta and atomic number 73. Previously known as tantalum, its name comes from tantalus, a villain from greek mythology. Tantalum is a rare, hard, blue-gray, lustrous transition metal that is highly corrosion-resistant. It is part of the refractory metals group, which are widely used as minor components in alloys. The chemical inertness of tantalum makes it a valuable substance for laboratory equipment and a substitute for platinum. Its main use today is in tantalum capacitors in electronic equipment such as mobile phones, dvd players, video game systems and computers. Tantalum, always together with the chemically similar niobium, occurs in the mineral groups tantalite, columbite, and coltan (a mix of columbite and tantalite, though not recognized as a separate mineral species). Tantalum is considered a technology-critical element.

Tungsten, or wolfram, is a chemical element with symbol W and atomic number 74. The name tungsten comes from the former Swedish name for the tungstate mineral scheelite, tungsten or "heavy stone". Tungsten is a rare metal found naturally on Earth almost exclusively combined with other elements in chemical compounds rather than alone. It was identified as a new element in 1781 and first isolated as a metal in 1783. Its important ores include wolframite and scheelite.

are a chemical element with symbol Au (from Latin: aurum) and atomic number 79, making it one of the higher atomic number elements that occur naturally. In its purest form, it is a bright, slightly reddish yellow, dense, soft, malleable, and ductile metal. Chemically, gold is a transition metal and a group 11 element. It is one of the least reactive chemical elements and is solid under standard conditions. Gold often occurs in free elemental (native) form, as nuggets or grains, in rocks, in veins, and in alluvial deposits. It occurs in a solid solution series with the native element silver (as electrum) and also naturally alloyed with copper and palladium. Less commonly, it occurs in minerals as gold compounds, often with tellurium (gold tellurides).

Lead is a chemical element with symbol Pb (from the Latin plumbum) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cut, lead is silvery with a hint of blue; it tarnishes to a dull gray color when exposed to air. Lead has the highest atomic number of any stable element and three of its isotopes each include a major decay chain of heavier elements.

Lead is a relatively unreactive post-transition metal. Its weak metallic character is illustrated by its amphoteric nature; lead and lead oxides react with acids and bases, and it tends to form covalent bonds. Compounds of lead are usually found in the +2 oxidation state rather than the +4 state common with lighter members of the carbon group. Exceptions are mostly limited to organolead compounds. Like the lighter members of the group, lead tends to bond with itself; it can form chains and polyhedral structures.

Bismuth is a chemical element with symbol Bi and atomic number 83. It is a pentavalent post-transition metal and one of the pnictogens with chemical properties resembling its lighter homologs arsenic and antimony. Elemental bismuth may occur naturally, although its sulfide and oxide form important commercial ores. The free element is 86% as dense as lead. It is a brittle metal with a silvery white color when freshly produced, but surface oxidation can give it a pink tinge. Bismuth is marginally radioactive, and the most naturally diamagnetic element, and has one of the lowest values of thermal conductivity among metals.

Titanium Boride Micropowder (TiB2) Applications:

Electrical conductivity composite materials- Electrical conduction boron nitride named dissipation watercraft made by titanium diboride and boron nitride is the essential part for vacuum aluminizing hardware; Ceramic cutting instruments and their segments Titanium diboride fired is utilized for metal worthless, expulsion kicks the bucket, sandblasting spouts, pruned segments and cutting devices; Composite clay materials- It could be utilized as multi-component composite materials critical constituent component. It can be made up cutting devices composite materials with TIC, TIN or SIC. Furthermore, it is as a part to make reinforcement assurance materials. It is the best materials for thermo soundness parts and capacity gadgets; Aluminum electrolysis cathode materials- Because of the great wet capacity of TIB2 and metal aluminum fluid. It influences the electrolytic aluminums to control utilization turn out to be low, at that point the electrolytic showers life will be long. It might likewise make up PIC exothermic materials and adaptability PIC materials, and it is the strengthen reagent of the metal materials, for example, AL, FE, and CU.

Titanium Boride Micropowder (TiB2) Storage Conditions:The damp reunion will affect its dispersion performance and using effects, therefore, this product should be sealed in vacuum and stored in a cool and dry room and it should not be exposed to air. In addition, the product should be avoided under stress.