Gilsonite Chemical Characterization
Gilsonite Chemical Characterization
Gilsonite is a complex system of different constituents, made of hydrocarbons and heteroatoms. After fractionation of the Gilsonite by specific solvents, four main chemical families are obtained: saturates, aromatics, resins, and asphaltenes. The association of asphaltene sheets (highly polycondensed pseudo monomers of a carbon black-bone, chemical functions, and heteroatoms surrounded by aliphatic chains) leads to the formation of microstructures or “micelles”. They can also form aggregates.
Gilsonite is included in a class of solid bitumens known as asphaltites. Gilsonite deposits are located in eastern Utah in the United States and Kermanshah-Iran. They are different from other asphaltites because of their:
- High asphaltene content
- High solubility in organic solvents
- High purity and consistent properties
- High molecular weight
- High nitrogen content
Gilsonite is available in different grades categorized by softening point. The softening point is used as an approximate guide to melt viscosity and behavior in solution.
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