Diagenetic relationships between sulphur species and formation of pyrite in coals and sediments
Samo za registrovane korisnike
2007
Članak u časopisu (Objavljena verzija)
Metapodaci
Prikaz svih podataka o dokumentuApstrakt
Based on the abundant minerals in a Miocene freshwater sequence of mixed sediments (pieces of coal in clays, sand-stones and shales) alternating with coal layers, the following main sedimentation environments were distinguished: illite-montmorillonitic (I-M), calcitic (Ct) and coal-forming environment. Applying factor analyses to 16 geochemical parameters, an environmentally- specific early diagenetic connection between the sulphur transformation processes, amount of Corg and precursor material species (C27-C29-steranes) was determined. It was found that the effects of limiting factors on Spyr formation depended on the hydrogeochemical conditions of individual sedimentation environments. Pyrite formation in coals depended directly on participation of higher plant precursor materials and/or on the total sulphur content in the system. In the MS, pyrite formation directly depended on total sulphur content, hydrogeological conditions and the amount of Corg.
Ključne reči:
Coal / Early diagenesis / MS (calcitic and illite-mont-morillonitic environment) / Pyrite formation / Sulphur speciesIzvor:
Energy Sources, Part A: Recovery, Utilization and Environmental Effects, 2007, 29, 16, 1487-1498Izdavač:
- Taylor & Francis Inc, Philadelphia
DOI: 10.1080/00908310600626531
ISSN: 1556-7036
WoS: 000250369600005
Scopus: 2-s2.0-35648956261
Institucija/grupa
IHTMTY - JOUR AU - Dević, Gordana AU - Pfendt, Petar A. PY - 2007 UR - https://cer.ihtm.bg.ac.rs/handle/123456789/371 AB - Based on the abundant minerals in a Miocene freshwater sequence of mixed sediments (pieces of coal in clays, sand-stones and shales) alternating with coal layers, the following main sedimentation environments were distinguished: illite-montmorillonitic (I-M), calcitic (Ct) and coal-forming environment. Applying factor analyses to 16 geochemical parameters, an environmentally- specific early diagenetic connection between the sulphur transformation processes, amount of Corg and precursor material species (C27-C29-steranes) was determined. It was found that the effects of limiting factors on Spyr formation depended on the hydrogeochemical conditions of individual sedimentation environments. Pyrite formation in coals depended directly on participation of higher plant precursor materials and/or on the total sulphur content in the system. In the MS, pyrite formation directly depended on total sulphur content, hydrogeological conditions and the amount of Corg. PB - Taylor & Francis Inc, Philadelphia T2 - Energy Sources, Part A: Recovery, Utilization and Environmental Effects T1 - Diagenetic relationships between sulphur species and formation of pyrite in coals and sediments VL - 29 IS - 16 SP - 1487 EP - 1498 DO - 10.1080/00908310600626531 ER -
@article{ author = "Dević, Gordana and Pfendt, Petar A.", year = "2007", abstract = "Based on the abundant minerals in a Miocene freshwater sequence of mixed sediments (pieces of coal in clays, sand-stones and shales) alternating with coal layers, the following main sedimentation environments were distinguished: illite-montmorillonitic (I-M), calcitic (Ct) and coal-forming environment. Applying factor analyses to 16 geochemical parameters, an environmentally- specific early diagenetic connection between the sulphur transformation processes, amount of Corg and precursor material species (C27-C29-steranes) was determined. It was found that the effects of limiting factors on Spyr formation depended on the hydrogeochemical conditions of individual sedimentation environments. Pyrite formation in coals depended directly on participation of higher plant precursor materials and/or on the total sulphur content in the system. In the MS, pyrite formation directly depended on total sulphur content, hydrogeological conditions and the amount of Corg.", publisher = "Taylor & Francis Inc, Philadelphia", journal = "Energy Sources, Part A: Recovery, Utilization and Environmental Effects", title = "Diagenetic relationships between sulphur species and formation of pyrite in coals and sediments", volume = "29", number = "16", pages = "1487-1498", doi = "10.1080/00908310600626531" }
Dević, G.,& Pfendt, P. A.. (2007). Diagenetic relationships between sulphur species and formation of pyrite in coals and sediments. in Energy Sources, Part A: Recovery, Utilization and Environmental Effects Taylor & Francis Inc, Philadelphia., 29(16), 1487-1498. https://doi.org/10.1080/00908310600626531
Dević G, Pfendt PA. Diagenetic relationships between sulphur species and formation of pyrite in coals and sediments. in Energy Sources, Part A: Recovery, Utilization and Environmental Effects. 2007;29(16):1487-1498. doi:10.1080/00908310600626531 .
Dević, Gordana, Pfendt, Petar A., "Diagenetic relationships between sulphur species and formation of pyrite in coals and sediments" in Energy Sources, Part A: Recovery, Utilization and Environmental Effects, 29, no. 16 (2007):1487-1498, https://doi.org/10.1080/00908310600626531 . .