Sub-bituminous coals are the second division of low-rank coals. They are transitional between lignite and bituminous coal. In the U.S. rank classification, sub-bituminous coals and their subdivisions (A, B, C) are based on calorific value. Sub-bituminous coals have calorific (heating) values of 8,300 to 11,500 Btu/lb (ASTM, 2014). Vitrinite reflectance (%Ro) in subbituminous coals is generally Ro between 0.4 to 0.5%Ro, although there is overlap between reflectance values for subbituminous A and bituminous C coals.

Sub-bituminous C (lower rank sub-bituminous) coals in the U.S. rank system are brown and earthy like lignites, whereas, sub-bituminous A (higher rank sub-bituminous) coals are gray to black and shiny like bituminous coals. Sub-bituminous coals are sometimes referred to as black lignite (Jackson, 1997).

Sub-bituminous rank and defining characteristics.


Physical and Chemical Changes (Sub-bituminous Rank)

Stages of coalification cited in different reports relative to their approximate U.S. coal rank. The term diagenesis was used by Tissot and Welte (1984) for the initial stages of coalification but it has also been used for the entire coalification process. %Ro= Vitrinite reflectance in oil. %Ro data from Teichm├╝ller and Teichmüller (1982). In the U.S. rank system, vitrinite reflectance values overlap between subbituminous A and high volatile bituminous C ranks, which is shown here as a dashed line.

During coalification of sub-bituminous coals, moisture loss continues, but biochemical gelification is replaced by geochemical gelification, also termed vitrinization. Vitrinization is the process by which low-rank components of coals called huminite macerals are transformed into vitreous (shiny) vitrinite macerals, which are characteristic of higher rank coals. Vitrinization is followed by bituminization, in which biogenic breakdown of the coal matrix is replaced by thermal breakdown (Mukhopadhya and Hatcher, 1993; Levine, 1993; Teichmüller, 1989; Stach et al., 1982). Above the rank of sub-bituminous B coals, most of the changes to coal chemistry and structure are driven by increased thermal (heating) rather than biogenic processess. The phase of increased thermally-driven changes is termed catagenesis in maturation studies (e.g., Tissot and Welte, 1984).


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Last Modified on 2017-08-18
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