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graphite

 
Dictionary: graph·ite   (grăf'īt') pronunciation
 
n.

A soft, steel-gray to black, hexagonally crystallized allotrope of carbon with a metallic luster and a greasy feel, used in lead pencils, lubricants, paints, and coatings, that is fabricated into a variety of forms such as molds, bricks, electrodes, crucibles, and rocket nozzles. Also called black lead, plumbago.

[Greek graphein, to write + –ITE1.]

graphitic gra·phit'ic (gră-fĭt'ĭk) adj.
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A low-pressure polymorph of carbon (the common high-pressure polymorph being diamond). Graphite is metallic in appearance and very soft. Crystals of graphite are infrequently encountered since the mineral usually occurs as earthy, foliated, or columnar aggregates often mixed with iron oxide, quartz, and other minerals. See also Carbon.

The sheetlike character of the graphite atomic arrangement results in distinctive physical properties. The mineral is very soft, with hardness 1½; it soils the fingers and leaves a black streak on paper, hence its use in pencils. The specific gravity is 2.23, often less because of the presence of pore spaces and impurities. The color is black in earthy material to steel-gray in plates, and thin flakes are deep blue in transmitted light. Graphite is a conductor of electricity.

The major sources of graphite are in gneisses and schists, where the mineral occurs in foliated masses mixed with quartz, mica, and so on. Noteworthy localities include the Adirondack region of New York, Korea, and Ceylon. In Sonora, Mexico, graphite occurs as a product of metamorphosed coal beds. Graphite is also observed in meteorites.

Synthetic graphite

Commercially produced synthetic graphite is a mixture of crystalline graphite and cross-linking intercrystalline carbon. Its physical properties are the result of contributions from both sources. Thus, among engineering materials, synthetic graphite is unusual because a wide variation in measurable properties can occur without significant change in chemical composition.

At room temperature the thermal conductivity of synthetic graphite is comparable to that of aluminum or brass. An unusual property of graphite is its increased strength at high temperature. Graphite is resistant to thermal shock because of its high thermal conductivity and low elastic modulus. It is one of the most inert materials with respect to chemical reaction with other elements and compounds. It is subject to oxidation, and reaction with and solution in some metals.

Graphite has many uses in the electrical, chemical, metallurgical, nuclear, and rocket fields: electrodes in electric furnaces producing carbon steel, alloy steel, and ferroalloys; anodes for the electrolytic production of chlorine, chlorates, magnesium, and sodium; motor and generator brushes; sleeve-type bearings and seal rings; rocket motor nozzles; missile nose cones; metallurgical molds and crucibles; linings for chemical reaction vessels; and, in a resin-impregnated impervious form, for heat exchangers, pumps, pipings, valves, and other process equipment.

Graphite (carbon) fibers

Carbon fibers are filamentary forms of carbon, with a fiber diameter normally in the 6–10-micrometer range. The product is offered in the form of yarns or tows containing from 1000 to 500,000 filaments per strand. The fibers offer a unique combination of properties. They are flexible, lightweight, thermally and to a large extent chemically inert, and are good thermal and electrical conductors. In their high-performance varieties, carbon fibers are very strong and can be extremely stiff.

The principal use of high-performance carbon fibers is as the reinforcing component in structural epoxy matrix composites. Due to initially high cost, the original applications were almost exclusively for lightweight, high-stiffness, and high-strength composites for the aerospace industry. The second major usage of high-performance carbon fibers is in sporting goods, such as golf club shafts, tennis rackets, fishing rods, and sailboat structures. The major matrix material for both applications is epoxy.


 
Dental Dictionary: graphite
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n

A soft carbon substance with a metallic black or gray sheen and a greasy feel. It is used in pencils, as a constituent of lubricants, and for making refractories such as crucibles in which to melt gold and other metals.

 

Mineral allotrope of carbon. It is dark gray to black, opaque, and very soft. Its layered structure, with rings of six atoms arranged in widely spaced parallel sheets, gives it its slippery quality. It occurs in nature and is used (mixed with clay) as the "lead" in pencils. It is also used in lubricants, crucibles, polishes, arc lamps, batteries, brushes for electric motors, and nuclear reactor cores.

For more information on graphite, visit Britannica.com.

 
Columbia Encyclopedia: graphite
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graphite (grăf'īt) , an allotropic form of carbon, known also as plumbago and black lead. It is dark gray or black, crystalline (often in the form of slippery scales), greasy, and soft, with a metallic luster. It is a good conductor of electricity and does not fuse at very high temperatures or burn easily. It occurs in nature in grayish-black masses, massive or crystalline, and is obtained in various parts of the world—in the United States (massive) in Nevada, Michigan, and Rhode Island and (crystalline) in Alabama and North Carolina; in Brazil; in the British Isles and on the Continent; and in Sri Lanka, Madagascar, and Siberia. It is also prepared artificially by treating hard coal in the electric furnace, a process discovered by E. G. Acheson. The uses of graphite are wide and diverse. The so-called lead of pencils is in reality a mixture of graphite with clay. Crucibles required to withstand high temperatures and also electrodes are commonly made of graphite. It is used also in stove polish, in some paints, and as a lubricant.


 
Rock & Mineral Guide: graphite
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C
Hexagonal -- Dihexagonal bipyramidal

Environment

Mainly in metamorphic rocks, possibly in pegmatites.

Crystal description

Isolated crystals are thin plates, usually in marbles, with rhombohedral faces on the edges. Commercial deposits are strange veinlike masses of solid material, or abundant plates disseminated through rock.

Physical properties

Black. Luster submetallic; hardness 1-2; specific gravity 2.3; streak black; cleavage perfect basal. Flexible inelastic flakes; greasy feel; stains the fingers; completely opaque.

Composition

Carbon.

Tests

Infusible, insoluble.

Distinguishing characteristics

Can only be confused with molybdenite, which shares its softness and greasy feel but is soluble in nitric acid and gives off fumes under the blowpipe flame.

Occurrence

Most frequently found in isolated, well-formed but tiny black crystals in an impure marble, associated with other minerals such as spinel, chondrodite, and pyroxene; apparently one product of the metamorphism of the organic contaminants of limestone. Around Ticonderoga, New York--where it was once mined for use in lead pencils--it also occurs in thin veins. Madagascar and Sri Lanka (Ceylon), where it forms large pure masses in thick veins, are the most important (and unusual) occurrences. European localities have included Bohemia, Bavaria, and Styria (Austria); but the most important were those in Siberia. There is no U.S. occurrence of this type.

Remarks

Its Old World name, plumbago (black lead) comes from its use in lead pencils. It is also used as a lubricant and as a refractory in crucibles. It is an outstanding example of the effect of the internal atomic arrangement on a mineral's physical properties. Carbon, with an open and sheeted spacing that gives it a specific gravity of 2.3, is opaque and one of the softest minerals. The diamond, the same element in a tighter spacing with a consequent specific gravity of 3.5, is transparent and the hardest substance known.



 
Wikipedia: Graphite
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Graphite

Graphite specimen
General
Category Native mineral
Chemical formula C
Identification
Color Steel black, to gray
Crystal habit Tabular, six-sided foliated masses, granular to compacted masses
Crystal system Hexagonal (6/m 2/m 2/m)
Cleavage Perfect in one direction
Fracture Flaky, otherwise rough when not on cleavage
Mohs Scale hardness 1–2
Luster metallic, earthy
Streak Black
Density 2.09–2.23 g/cm³
Refractive index Opaque
Pleochroism None
Solubility Molten Ni

The mineral graphite is one of the allotropes of carbon. It was named by Abraham Gottlob Werner in 1789 from the Greek γραφειν (graphein): "to draw/write", for its use in pencils, where it is commonly called lead, as distinguished from the actual metallic element lead. Unlike diamond (another carbon allotrope), graphite is an electrical conductor, a semimetal, and can be used, for instance, in the electrodes of an arc lamp. Graphite holds the distinction of being the most stable form of carbon under standard conditions. Therefore, it is used in thermochemistry as the standard state for defining the heat of formation of carbon compounds. Graphite may be considered the highest grade of coal, just above anthracite and alternatively called meta-anthracite, although it is not normally used as fuel because it is hard to ignite.

There are three principal types of natural graphite, each occurring in different types of ore deposit: (1) Crystalline flake graphite (or flake graphite for short) occurs as isolated, flat, plate-like particles with hexagonal edges if unbroken and when broken the edges can be irregular or angular; (2) Amorphous graphite occurs as fine particles and is the result of thermal metamorphism of coal, the last stage of coalification, and is sometimes called meta-anthracite. Very fine flake graphite is sometimes called amorphous in the trade; (3) Lump graphite (also called vein graphite) occurs in fissure veins or fractures and appears as massive platy intergrowths of fibrous or acicular crystalline aggregates, and is probably hydrothermal in origin.

Highly Ordered Pyrolytic Graphite or Highly Oriented Pyrolytic Graphite (HOPG) refers to graphite with an angular spread of the between the graphite sheets of less than 1°. This highest-quality synthetic form is used in scientific research.[1] The name "graphite fiber" is also sometimes used to refer to carbon fibre or carbon fibre reinforced plastic.

Contents

Occurrence

Graphite ore
Graphite output in 2005

Minerals associated with graphite include quartz, calcite, micas, iron meteorites, and tourmalines. China is usually the top producer of graphite, followed by India and Brazil.

Graphite has various other characteristics. Thin flakes are flexible but inelastic, the mineral can leave black marks on hands and paper, it conducts electricity, and displays superlubricity. Its best field indicators are softness, luster, density and streak.

According to the USGS, world production of natural graphite in 2006 was 1.03 million tonnes and in 2005 was 1.04 million tonnes (revised), of which the following major exporters produced: China produced 720,000 tonnes in both 2006 and 2005, Brazil 75,600 tonnes in 2006 and 75,515 tonnes in 2005 (revised), Canada 28,000 tonnes in both years, and Mexico (amorphous) 12,500 tonnes in 2006 and 12,357 tonnes in 2005 (revised). In addition, there are two specialist producers: Sri Lanka produced 3,200 tonnes in 2006 and 3,000 tonnes in 2005 of lump or vein graphite, and Madagascar produced 15,000 tonnes in both years, a large portion of it "crucible grade" or very large flake graphite. Some other producers produce very small amounts of "crucible grade".

According to the USGS, U.S. (synthetic) graphite electrode production in 2006 was 132,000 tonnes valued at $495 million and in 2005 was 146,000 tonnes valued at $391 million, and high-modulus graphite (carbon) fiber production in 2006 was 8,160 tonnes valued at $172 million and in 2005 was 7,020 tonnes valued at $134 million.

Detailed properties

Graphite is a layered compound. In each layer, the carbon atoms are arranged in a hexagonal lattice with separation of 0.142 nm, and the distance between planes is 0.335 nm.[2] The two known forms of graphite, alpha (hexagonal) and beta (rhombohedral), have very similar physical properties (except that the graphene layers stack slightly differently).[3] The hexagonal graphite may be either flat or buckled.[4] Graphites that naturally occur have been found to contain up to 30% of the beta form, when synthetically-produced graphite only contains the alpha form.[citation needed] The alpha form can be converted to the beta form through mechanical treatment and the beta form reverts to the alpha form when it is heated above 1300 °C.[5] The layering contributes to its lower density.

The acoustic and thermal properties of graphite are highly anisotropic, since phonons propagate very quickly along the tightly-bound planes, but are slower to travel from one plane to another.

Graphite can conduct electricity due to the vast electron delocalization within the carbon layers. These valence electrons are free to move, so are able to conduct electricity. However, the electricity is only conducted within the plane of the layers.

Graphite and graphite powder are valued in industrial applications for its self-lubricating and dry lubricating properties. There is a common belief that graphite's lubricating properties are solely due to the loose interlamellar coupling between sheets in the structure. However, it has been shown that in a vacuum environment (such as in technologies for use in space), graphite is a very poor lubricant. This observation led to the discovery that the lubrication is due to the presence of fluids between the layers, such as air and water, which are naturally adsorbed from the environment. This molecular property is unlike other layered, dry lubricants such as molybdenum disulfide. Recent studies suggest that an effect called superlubricity can also account for graphite's lubricating properties. The use of graphite is limited by its tendency to facilitate pitting corrosion in some stainless steel[6][7], and to promote galvanic corrosion between dissimilar metals (due to its electrical conductivity). It is also corrosive to aluminium in presence of moisture. For this reason, the US Air Force banned its use as a lubricant in aluminium aircraft [8], and discouraged its use in aluminium-containing automatic weapons [9]. Even graphite pencil marks on aluminium parts may facilitate corrosion [10]. Another high-temperature lubricant, hexagonal boron nitride, has the same molecular structure as graphite. It is sometimes called white graphite, due to its similar properties.

When a large number of crystallographic defects binds these planes together, graphite loses its lubrication properties and becomes what is known as pyrolytic carbon. This material is useful for blood-contacting implants such as artificial heart valves. It is also highly diamagnetic, thus it will float in mid-air above a strong magnet.

Natural and crystalline graphites are not often used in pure form as structural materials, due to their shear-planes, brittleness and inconsistent mechanical properties.

History

Some time before 1565 (some sources say as early as 1500), an enormous deposit of graphite was discovered on the approach to Grey Knotts from the hamlet of Seathwaite near Borrowdale parish, Cumbria, England, which the locals found very useful for marking sheep.[11][12] This particular deposit of graphite was extremely pure and solid, and could easily be sawn into sticks. This remains the only deposit of graphite found in this solid form.[13]

Uses of natural graphite

According to the USGS, U.S. consumption of natural graphite in 2005-06 averaged 41,850 tonnes in end uses such as refractories, steelmaking, expanded graphite, brake linings, and foundry facings-lubricants. GAN (Graphite Advocate News) import-export statistics for 2006 and 2007 indicate the consumption will continue at that level unless steelmaking carbon raiser takes a drastic drop.

Graphene, which occurs naturally in graphite, might be one of the strongest substance known; however, the process of separating it from graphite will require some technological development before it is economical enough to be used in industrial processes.

Refractories

This end-use begins before 1900 with the graphite crucible used to hold molten metal; this is now a minor part of refractories. In the mid 1980s, the carbon-magnesite brick became important, and a bit later the alumina-graphite shape. Currently the order of importance is alumina-graphite shapes, carbon-magnesite brick, monolithics (gunning and ramming mixes), and then crucibles. Crucibles began using very large flake graphite, and carbon-magnesite brick requiring not quite so large flake graphite; for these and others there is now much more flexibility in size of flake required, and amorphous graphite is no longer restricted to low-end refractories. Alumina-graphite shapes are used as continuous casting ware, such as nozzles and troughs, to convey the molten steel from ladle to mould, and carbon magnesite bricks line steel converters and electric arc furnaces to withstand extreme temperatures. Graphite Blocks are also used in parts of blast furnace linings where the high thermal conductivity of the graphite is critical. High-purity monolithics are often used as a continuous furnace lining instead of the carbon-magnesite bricks. The U.S. and European refractories industry had a crisis in 2000-2003, with an indifferent market for steel and a declining refractory consumption per tonne of steel underlying firm buyouts and many plant closings. Many of the plant closings resulted from the RHI acquisition of Harbison-Walker Refractories; some plants had their equipment auctioned off. Since much of the lost capacity was for carbon-magnesite brick, graphite consumption within refractories area moved towards alumina-graphite shapes and monolithics, and away from the brick. The major source of carbon-magnesite brick is now imports from China. Almost all of the above refractories are used to make steel and account for 75% of refractory consumption; the rest is used by a variety of industries, such as cement. According to the USGS, 2006 U.S. natural graphite consumption in refractories was 11,000 tonnes and in 2005 11,800 tonnes.

Steelmaking

Natural graphite in this end use mostly goes into carbon raising in molten steel, although it can be used to lubricate the dies used to extrude hot steel. Supplying carbon raiser is very competitive, therefore subject to cut-throat pricing from alternatives such as synthetic graphite powder, petroleum coke, and other forms of carbon. A carbon raiser is added to increase the carbon content of the steel to the specified level. A GAN consumption estimate based on USGS U.S. graphite consumption statistics indicates that 10,500 tonnes were used in this fashion in 2005.

Expanded graphite

Expanded graphite is made by immersing natural flake graphite in a bath of chromic acid, then concentrated sulfuric acid, which forces the crystal lattice planes apart, thus expanding the graphite. The expanded graphite can be used to make graphite foil or used directly as "hot top" compound to insulate molten metal in a ladle or red-hot steel ingots and decrease heat loss, or as firestops fitted around a fire door or in sheet metal collars surrounding plastic pipe, (During a fire, the graphite expands and chars to resist fire penetration and spread.), or to make high-performance gasket material for high-temperature use. After being made into graphite foil, the foil is machined and assembled into the bipolar plates in fuel cells. The foil is made into heat sinks for laptop computers which keeps them cool while saving weight, and is made into a foil laminate that can be used in valve packings or made into gaskets. Old-style packings are now a minor member of this grouping: fine flake graphite in oils or greases for uses requiring heat resistance. A GAN estimate of current U.S. natural graphite consumption in this end use is 7,500 tonnes.

Intercalated graphite

Structure of CaC6

Graphite forms intercalation compounds with some metals and small molecules. In these compounds, the host molecule or atom gets "sandwiched" between the graphite layers, resulting in compounds with variable stoichiometry. A prominent example of an intercalation compound is potassium graphite, denoted by the formula KC8. Graphite intercalation compounds are superconductors. The highest transition temperature (by June 2009) Tc = 11.5 K is achieved in CaC6 and it further increases under applied pressure (15.1 K at 8 GPa).[14]

Brake linings

Natural amorphous and fine flake graphite are used in brake linings or brake shoes for heavier (nonautomotive) vehicles, and became important with the need to substitute for asbestos. This use has been important for quite some time, but nonasbestos organic (NAO) compositions are beginning to cost graphite market share. A brake-lining industry shake-out with some plant closings has not helped either, nor has an indifferent automotive market. According to the USGS, U.S. natural graphite consumption in brake linings was 6,510 tonnes in 2005.

Foundry facings and lubricants

A foundry facing or mold wash is a water-based paint of amorphous or fine flake graphite. Painting the inside of a mold with it and letting it dry leaves a fine graphite coat that will ease separation of the object cast after the hot metal has cooled. Graphite lubricants are specialty items for use at very high or very low temperatures, as a wire die extrusion lubricant, an antiseize agent, a gear lubricant for mining machinery, and to lubricate locks. Having low-grit graphite, or even better no-grit graphite (ultra high purity), is highly desirable. It can be used as a dry powder, in water or oil, or as colloidal graphite (a permanent suspension in a liquid). An estimate based on USGS graphite consumption statistics indicates that 2,200 tonnes was used in this fashion in 2005.

Other uses

Natural graphite has found uses as the marking material ("lead") in common pencils, in zinc-carbon batteries, in electric motor brushes, and various specialized applications.

Uses of synthetic graphite

Electrodes

These electrodes carry the electricity that heats electric arc furnaces, the vast majority steel furnaces. They are made from petroleum coke after it is mixed with petroleum pitch, extruded and shaped, then baked to sinter it, and then graphitized by heating it above the temperature that converts carbon to graphite. They can vary in size up to 11 ft. long and 30 in. in diameter. An increasing proportion of global steel is made using electric arc furnaces, and the electric arc furnace itself is getting more efficient and making more steel per tonne of electrode. An estimate based on USGS data indicates that graphite electrode consumption was 197,000 tonnes in 2005.

Powder and scrap

The powder is made by heating powdered petroleum coke above the temperature of graphitization, sometimes with minor modifications. The graphite scrap comes from pieces of unusable electrode material (in the manufacturing stage or after use) and lathe turnings, usually after crushing and sizing. Most synthetic graphite powder goes to carbon raising in steel (competing with natural graphite), with some used in batteries and brake linings. According to the USGS, U.S. synthetic graphite powder and scrap production was 95,000 tonnes in 2001 (latest data).

Other uses

Graphite (carbon) fiber and carbon nanotubes are also used in carbon fiber reinforced plastics, and in heat-resistant composites such as reinforced carbon-carbon (RCC). Products made from carbon fiber graphite composites include fishing rods, golf clubs,bicycle frames,and pool sticks and have been successfully employed in reinforced concrete. The mechanical properties of carbon fiber graphite-reinforced plastic composites and grey cast iron are strongly influenced by the role of graphite in these materials. In this context, the term "(100%) graphite" is often loosely used to refer to a pure mixture of carbon reinforcement and resin, while the term "composite" is used for composite materials with additional ingredients.

Synthetic graphite also finds use as a matrix and neutron moderator within nuclear reactors. Its low neutron cross section also recommends it for use in proposed fusion reactors. Care must be taken that reactor-grade graphite is free of neutron absorbing materials such as boron, widely used as the seed electrode in commercial graphite deposition systems—this caused the failure of the Germans' World War II graphite-based nuclear reactors. Since they could not isolate the difficulty they were forced to use far more expensive heavy water moderators. Graphite used for nuclear reactors is often referred to as nuclear graphite.

Graphite has been used in at least three radar absorbent materials. It was mixed with rubber in Sumpf and Schornsteinfeger, which were used on U-boat snorkels to reduce their radar cross section. It was also used in tiles on early F-117 Nighthawks. Modern gunpowder is coated in graphite to prevent the buildup of static charge.

Graphite also has the interesting property that, under certain conditions, it can serve as a form of armor against nuclear weapons. While there is no practical military application for this, graphite is a common material proposed for the pusher plate of a nuclear pulse rocket; a space vehicle that propels itself by ejecting nuclear explosives through the rear and detonating them.[citation needed]

Graphite mining, beneficiation, and milling

Graphite is mined around the world by both open pit and underground methods. While flake graphite and amorphous graphite are both mined open pit and underground, lump (vein) graphite is only mined underground in Sri Lanka. The open pit mines usually employ equipment (i.e. bulldozers) to scoop up the ore, which is usually put in trucks and moved to the plant. Since the original rock is usually lateritized or weathered, this amounts to moving dirt with flecks or pieces of graphite in it from the pit (blasting is seldom required). The underground graphite mines employ drilling and blasting to break up the hard rock (ore), which is then moved by mine cars pulled by a locomotive, or moved by automotive vehicles, to the surface and then to the plant. In less-developed areas of the world, the ore can be mined by pick and shovel and transported by mine cars pushed by a laborer or by women carrying baskets of ore on their heads.

Graphite usually needs beneficiation, although thick-bedded amorphous graphite and vein graphite is almost always beneficiated, if beneficiated at all, by laborers hand-picking out the pieces of gangue (rock) and hand-screening the product. The great majority of world flake graphite production is crushed and ground if necessary and beneficiated by flotation. Treating graphite by flotation encounters one big difficulty: graphite is very soft and "marks" (coats) the particles of gangue. This makes the "marked" gangue particles float off with the graphite to yield a very impure concentrate. There are two ways of obtaining a saleable concentrate or product: regrinding and floating it again and again (up to seven times) to obtain a purer and purer concentrate, or by leaching (dissolving) the gangue with hydrofluoric acid (for a silicate gangue) or hydrochloric acid (for a carbonate gangue).

In the milling process, the incoming graphite products and concentrates can be ground before being classified (sized or screened), with the coarser flake size fractions (above 8 mesh, 8 mesh to 20 mesh, 20 mesh to 50 mesh) carefully preserved, and then the carbon contents are determined. Then some standard blends can be prepared from the different fractions, each with a certain flake size distribution and carbon content. Custom blends can also be made for individual customers who want a certain flake size distribution and carbon content. If flake size is unimportant, the concentrate can be ground more freely. Typical final products include a fine powder for use as a slurry in oil drilling; in zirconium silicate, sodium silicate and isopropyl alcohol coatings for foundry molds; and a carbon raiser in the steel industry ( Synthetic graphite powder and powdered petroleum coke can also be used as carbon raiser)(Earth Metrics, 1989). Rough graphite is typically classified, ground, and packaged at a graphite mill; often the more complex formulations are also mixed and packaged at the mill facility. Environmental impacts from graphite mills consist of air pollution including fine particulate exposure of workers and also soil contamination from powder spillages leading to heavy metals contaminations of soil. Dust masks are normally worn by workers during the production process to avoid worker exposure to the fine airborne graphite and zircon silicate.

Graphite recycling

The most common way graphite is recycled occurs when synthetic graphite electrodes (or anodes or cathodes) are either manufactured and pieces are cut off or lathe turnings are discarded, or the electrode (or other) are used all the way down to the electrode holder. A new electrode replaces the old one , but a sizeable piece of the old electrode remains. This is crushed and sized, and the resulting graphite powder is mostly used to raise the carbon content of molten steel. Graphite-containing refractories are sometimes also recycled , but often not because of their graphite: the largest-volume items, such as carbon-magnesite bricks that contain only 15%-25% graphite, usually contain too little graphite. However, some recycled carbon-magnesite brick is used as the basis for furnace repair materials, and also crushed carbon-magnesite brick is used in slag conditioners. While crucibles have a high graphite content, the volume of crucibles used and then recycled is very small.

A high-quality flake graphite product that closely resembles natural flake graphite can be made from steelmaking kish. Kish is a large-volume near-molten waste skimmed from the molten iron feed to a basic oxygen furnace, and is a mix of graphite (precipitated out of the supersaturated iron), lime-rich slag, and some iron. The iron is recycled on site, so what is left is a mixture of graphite and slag. The best recovery process uses hydraulic classification (Which utilizes a flow of water to separate minerals by specific gravity: graphite is light and settles nearly last.) to get a 70% graphite rough concentrate. Leaching this concentrate with hydrochloric acid gives a 95% graphite product with a flake size ranging from 10 mesh down.

Media

Rotating graphite stereogram

See also

References

  1. ^ IUPAC Gold Book
  2. ^ P. Delhaes (2001). Graphite and Precursors. CRC Press. 
  3. ^ C. S. G. Cousins (2003). "Elasticity of carbon allotropes. I. Optimization, and subsequent modification, of an anharmonic Keating model for cubic diamond". Physical Review B 67: 024107. http://prola.aps.org/pdf/PRB/v67/i2/e024107. 
  4. ^ W.G. Wyckoff (1963). Crystal Structures. New York, London: John Wiley & Sons. 
  5. ^ "Rhombohedral graphite". IUPAC. http://www.iupac.org/goldbook/R05385.pdf. 
  6. ^ "Galvanic Corrosion". http://steel.keytometals.com/Articles/Art160.htm. 
  7. ^ "ASM Tech Notes - TN7-0506 - Galvanic Corrosion". http://metals.lincdigital.com.au/files/ASM_Tech_Notes/TN7-0506-Galvanic%20Corrosion.pdf. 
  8. ^ "Better Lubricants than Graphite". http://www.graflex.org/speed-graphic/lubricants.html. 
  9. ^ "Weapons Lubricant in the Desert". http://gojackarmy.blogspot.com/2005/09/weapons-lubricant-in-desert.html. Retrieved on 2009-06-06. 
  10. ^ "Good Engineering Practice/Corrosion". http://7faq.com/owbase/ow.asp?GoodEngineeringPractice%2FCorrosion. Retrieved on 2009-06-06. 
  11. ^ Martin and Jean Norgate, Geography Department, Portsmouth University (2008). "Old Cumbria Gazetteer, black lead mine, Seathwaite". http://www.geog.port.ac.uk/webmap/thelakes/html/lgaz/lk00976.htm. Retrieved on 2008-05-19. 
  12. ^ Alfred Wainwright (2005). A Pictorial Guide to the Lakeland Fells, Western Fells. London: Frances Lincoln. ISBN 0-7112-2460-9. 
  13. ^ "Pencil". 2007-08-07. http://en.wikipedia.org/wiki/Pencil. Retrieved on 2007-08-07. 
  14. ^ N. Emery et al. (2008). "Synthesis and superconducting properties of CaC6". Sci. Technol. Adv. Mater. 9: 044102. doi:10.1088/1468-6996/9/4/044102. http://www.iop.org/EJ/article/1468-6996/9/4/044102/stam8_4_044102.pdf. 
  • C.Michael Hogan, Marc Papineau et al., Phase I Environmental Site Assessment, Asbury Graphite Mill, 2426-2500 Kirkham Street, Oakland, California, Earth Metrics report 10292.001, December 18, 1989
  • Klein, Cornelis and Cornelius S. Hurlbut, Jr. (1985) Manual of Mineralogy: after Dana 20th ed. ISBN 0-471-80580-7
  • Taylor, Harold A., "Graphite", Financial Times Executive Commodity Reports (London: Mining Journal Books ltd.) 2000 ISBN 1-84083-332-7
  • Taylor, Harold A., "Graphite", Industrial Minerals and Rocks, 7th ed. (Littleton, CO AIME-Society of Mining Engineers) 2005 ISBN 0-87335-233-5

External links


 
Translations: Graphite
Top

Dansk (Danish)
n. - grafit

Nederlands (Dutch)
grafiet

Français (French)
n. - graphite

Deutsch (German)
n. - Graphit

Ελληνική (Greek)
n. - (χημ.) γραφίτης

Italiano (Italian)
grafite

Português (Portuguese)
n. - grafite (f) (Quím.)

Русский (Russian)
графит, графитовый

Español (Spanish)
n. - grafito

Svenska (Swedish)
n. - blyerts

中文(简体)(Chinese (Simplified))
黑铅, 石墨

中文(繁體)(Chinese (Traditional))
n. - 黑鉛, 石墨

한국어 (Korean)
n. - 흑연

日本語 (Japanese)
n. - 石墨, 黒鉛

العربيه (Arabic)
‏(الاسم) الغرافيت : نوع من الكربون الاسود تصنع منه اقلام الرصاص‏

עברית (Hebrew)
n. - ‮גרפיט, חומר הכתיבה של העיפרון‬


 
 

 

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Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved.  Read more
Sci-Tech Encyclopedia. McGraw-Hill Encyclopedia of Science and Technology. Copyright © 2005 by The McGraw-Hill Companies, Inc. All rights reserved.  Read more
Dental Dictionary. Mosby's Dental Dictionary. Copyright © 2004 by Elsevier, Inc. All rights reserved.  Read more
Britannica Concise Encyclopedia. Britannica Concise Encyclopedia. © 2006 Encyclopædia Britannica, Inc. All rights reserved.  Read more
Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/  Read more
Rock & Mineral Guide. Peterson Field Guide to Rocks and Minerals, by Frederick H. Pough. Copyright © 1998 by Houghton Mifflin Company. Published by Houghton Mifflin Company. All rights reserved.  Read more
Wikipedia. This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Graphite" Read more
Translations. Copyright © 2007, WizCom Technologies Ltd. All rights reserved.  Read more