Properties of thermally metamorphosed coal from Tanjung Enim Area, South Sumatra Basin, Indonesia with special reference to the coalification path of macerals

Abstract

Abstract Thermally metamorphosed Tertiary age coals from Tanjung Enim in South Sumatra Basin have been investigated by means of petrographic, mineralogical and chemical analyses. These coals were influenced by heat from an andesitic igneous intrusion. The original coal outside the metamorphosed zone is characterized by high moisture content (4.13–11.25 wt.%) and volatile matter content (> 40 wt.%, daf), as well as less than 80 wt.% (daf) carbon and low vitrinite reflectance (VR max = 0.52–0.76%). Those coals are of subbituminous and high volatile bituminous rank. In contrast the thermally metamorphosed coals are of medium-volatile bituminous to meta-anthracite rank and characterized by low moisture content (only 80 wt.%, daf) and vitrinite reflectance (VR max = 1.87–6.20%). All the studied coals have a low mineral matter content, except for those which are highly metamorphosed, due to the formation of new minerals. The coalification path of each maceral shows that vitrinite, liptinite and inertinite reflectance converge in a transition zone at VR max of around 1.5%. Significant decrease of volatile matter occurs in the zone between 0.5% and 2.0% VR max . A sharp bend occurs at VR max between 2.0% and 2.5%. Above 2.5%, the volatile matter decreases only very slightly. Between VR r = 0.5% and 2.0%, the carbon content of the coals is ascending drastically. Above 2.5% VR r , the carbon content becomes relatively stable (around 95 wt.%, daf). Vitrinite is the most abundant maceral in low rank coal (69.6–86.2 vol.%). Liptinite and inertinite are minor constituents. In the high rank coal, the thermally altered vitrinite composes 82.4–93.8 vol.%. Mosaic structures can be recognized as groundmasss and crack fillings. The most common minerals found are carbonates, pyrite or marcasite and clay minerals. The latter consist of kaolinite in low rank coal and illite and rectorite in high rank coal. Change of functional groups with rank increase is reflected most of all by the increase of the ratio of aromatic C–H to aliphatic C–H absorbances based on FTIR analysis. The Oxygen Index values of all studied coals are low (OI 2 /g TOC) and the high rank coals have a lower Hydrogen Index ( T max increases with maturity (420–440 °C for low rank coals and 475–551 °C for high rank coals). Based on the above data, it was calculated that the temperature of contact metamorphism reached 700–750 °C in the most metamorphosed coal.