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Graphite is one of the three familiar naturally occurring forms of the chemical element carbon. The two other varieties are amorphous carbon (not to be confused with amorphous graphite) and diamond. Graphite is familiar to most people as the active ingredient in lead pencils. However, its use in writing instruments is far outweighed by a myriad of other industrial applications whose performance depends on the unique chemical and physical properties of this material. Graphite is a major additive to many industrial systems where it provides functionality as a refractory, lubricant, thermal conductor, electrical conductor, UV shield, electromagnetic pulse shield, corrosion shield, pigment, etc.

Graphite is considered an archaic industrial mineral since it has been mined for its useful properties (lubrication, pigmentation, writing, etc.) for thousands of years. The word graphite is derived from the Greek word graphein, which means, to write. A version of the word graphein is still retained by carbon scientists as the word graphene, which is the term used to describe a singe layer of a graphite crystal, the graphene layer. The documented use of graphite as a commercial writing material is traced to the area around Keswick in Cumberland Great Britain where a high quality deposit of writing graphite was discovered in the middle of the 1500s (Petroski).

During the late 1800s, while attempting to manufacture the refractory material silicon carbide, E.G. Acheson discovered that synthetic graphite formed as a result of this ultra high temperature electric process. This discovery was the birth of the synthetic graphite industry. Right around the same time that Mr. Acheson was experimenting with the manufacture of synthetic graphite electrodes, Mr. Riddle (the founder of Asbury Graphite Mills, Inc.) was converting a water-powered mill, formally used to grind flour, into a natural graphite grinding mill.

With the help of the Asbury Graphite Mills, Inc., today's industrial society has the benefit of Asbury's 110+ years of processing both natural and synthetic graphite products to strict size, purity, and performance specifications using the most up to date grinding and size-classification equipment.

Graphite materials fit into two primary classifications: natural graphite and synthetic graphite. Natural graphite can be further divided into three primary types: amorphous, flake, and crystalline vein. Each type has characteristic properties and is formed in a unique geologic setting. Synthetic graphite can be divided into many types whose ultimate properties depend on the precursor carbon used in its manufacture as well as the heat treatment history that the precursor carbon goes through.

Regardless of type, all graphite materials share certain inherent characteristics, which are a reflection of the atomic structure and crystallographic arrangement of carbon atoms in the graphite crystal. Properties such as lubricity, thermal conductivity, electrical conductivity, color, etc., are all constants when applied to a single crystal of graphite. However when single crystals or crystallites combine to form macroscopic particles as in flakes, lumps, powders, or pieces of graphite, these properties see changes that reflect the way microscopic crystals are arranged in macroscopic particles. Crystal or crystallite orientation relative to neighbor domains, grain boundary effects, etc., all contribute to the overall bulk properties of the solid or powder which can be very different from those of the perfect crystal. This arrangement of crystals and crystallites, as well as the purity of a given graphite material, is what gives graphite of different types their respective properties. These differences result in the variation in performance characteristics observed for different graphite materials.

The remainder of this paper can be found at : http://www.asbury.com/Introduction.html