Amorphous graphite is a natural mineral. Contrary to the name, this is not truly amorphous, but is a microcrystalline form of natural graphite. It is granular except in extremely fine grinds, which have a flakey structure.
The term “amorphous” is applied to this form of natural graphite. Material is available in sizes ranging from mixed 1 cm and smaller particles to 10 cm lumps.
|Percent Carbon||60 – 99.9 %|
|Particle Size Range||-3/4 — 5 microns|
|Massive lumps with flat fracture cleavage.|
Amorphous graphite is a seam mineral, not to be confused with a vein mineral. It is formed by the metamorphism of previously existing anthracite coal seams. Proto-coal organic carbon is deposited and converted into anthracite coal followed by low grade metamorphism of the coal. This results in the formation of microcrystalline graphite. Regions where this process occurs may consist of zones where anthracite deposits occur adjacent to graphite deposits. This phenomenon is indicative of localized metamorphism or contact metamorphism.
Contact metamorphism is metamorphism that is the result of localized contact between the agent of metamorphism (magma intrusion, local tectonic stress, etc.) and the body being metamorphosed A good example of this type of graphite formation is the amorphous graphite deposits of Sonora, Mexico. In these deposits the graphite affecting agent has been identified as swarms of dikes that intruded the area.Dikesare intrusions of magma that are tabular in shape, and cut across the structure of the country rocks. The illustration is a schematic of such a contact between a coal seam and its intruded dike. Although the coal bed illustrated is shown “parallel’ to the local bedding, most if not all anthracite seams occur in folded strata, which are indicative of the semi-metamorphic nature of this variety of coal.
Note that the formation of amorphous graphite is not limited to the contact metamorphism agent only. Regional metamorphism may occur as when a large intrusion such a batholith or stock intrudes beneath or adjacent to structures containing the right type of precursor carbon.
Seam graphite is typically higher in ash than other forms of natural graphite. Since the proto-carbon is deposited contemporaneously with other mineral matter that flows into swamps, bogs, deltas, and other “coal producing” environments. Since the ‘system’ is more or less closed to the exchange of mass with the country rock, the mineral matter (ash) that was present in the coal remains in the graphite. This mineral matter may be either “free”, i.e., “mechanically” attached particulates such as quartz, or may consist of clay-like minerals that are intimately associated with the carbon.
Amorphous graphite is the least “graphitic” of the natural graphite types. The macroscopic morphology of this graphite variety is called “massive” which is indicative of its homogeneous non stratified, microcrystalline structure. The long range order common to crystalline substances is minimal in this graphite variety. Crystallinity is poor as is indicated by the fact that none of the common crystal forms (crystal faces) visible in flake and vein graphite are visible in amorphous graphite. Based on “degree of graphitization” as determined by X-ray diffraction studies, amorphous graphite typically shows “graphite content” of 20-40 percent as compared to 90+ percent for other natural graph types.
The development of long range crystallographic order requires that some degree of pre-crystalline order be present in the proto-carbon, and that the energy supplied to this carbon be sufficient to promote graphitization. In the case of amorphous graphite it is apparent that only minimal pre-ordering of proto-crystallographic domains occurred.
Amorphous graphite is extracted using conventional coal-type mining techniques. Most of the current supply of amorphous graphite available in the United States is imported from Mexico and China. Previously other sources included Korea, Italy, and Rhode Island USA. Amorphous graphite is typically lower in purity than other natural graphite. This is due to the intimate contact between the graphite “micro crystals” and the mineral ash with which it is associated. This close graphite/ash association makes floatation and other density and chemical based separation techniques inefficient if not impossible. Commercial grades are available from 75-85% purity in particle sizes from 4-inch lumps to 3-micrometer powder.
Amorphous graphite tends to be much less reflective in both large a small grained sizes. Therefore, it has a darker color, bordering on black, while other natural graphite has a color closer to “silver-gray”. This makes amorphous graphite useful in coatings and other products, which require less reflectance. Also, this graphite variety is typically lower in cost than other types but is still lubricious, conductive, and chemically stable.
Amograph is used in many lubricant products especially greases, forging lubricants, etc. In applications where higher ash contents are acceptable or preferred this type of graphite is a good choice.
Certain applications such as mechanical seals require a certain degree of rubbing abrasion to provide the necessary “lapping” or cleaning of opposing rubbing surfaces. The ash content of amorphous graphite can provide the right balance of gentle abrasion required to perform this function. By selecting a properly sized amorphous graphite powder the user can control the size of the ash.
Asbury Carbons has literally hundreds of grades of amorphous graphite available. Grades are categorized based on particle size and purity and can be customized to fit any requirement. With 100+ years of experience in the grinding and sizing of amorphous graphite we can modestly state that we are experts at providing the right amograph for the job.
If you are unable to locate a Chemical or Mineral you need, our sales department can custom source any needed materials for you directly.