Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis
Abstract
Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis were studied. The maturity ratios based on biomarkers and alkylaromatics which showed the best applicability were determined. Intensity of observed changes of maturity ratios decreases in the following order: mineral-rich coal > matrix coal > xylite-rich coal, indicating that mineral matter, which is dominated by clays in all lithotypes, plays an important role in the isomerisation of polycyclic biomarkers and aromatic compounds. Carbon isotopic signatures of n-C25 and n-C27 alkanes, as well as δ13C values of phenathrene and cadalene are very close in studied range of maturity, confirming that isotopic signatures are useful tracers for alteration products of biological molecules. Long-chain homologues of n-alkanes exhibit slight enrichment in 12C with increasing maturity, whereas almost no change is detected in δ13C of short-chain n-alkanes. Negligible enrichment in... 13C of aromatic compounds is observed during maturation.
Keywords:
Lignite lithotypes / Maturity / Biomarkers / Aromatic hydrocarbons / Carbon isotopic compositionSource:
Conference Proceedings, 29th International Meeting on Organic Geochemistry, 2019, 2019Publisher:
- European Association of Geoscientists & Engineers
Funding / projects:
- Geochemical investigations of sedimentary rocks - fossil fuels and environmental pollutants (RS-176006)
Collections
Institution/Community
Hemijski fakultet / Faculty of ChemistryTY - CONF AU - Kojić, I. AU - Bechtel, A. AU - Sachsenhofer, R.F. AU - Životić, D. AU - Stojanović, Ksenija A. PY - 2019 UR - http://cherry.chem.bg.ac.rs/handle/123456789/5173 AB - Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis were studied. The maturity ratios based on biomarkers and alkylaromatics which showed the best applicability were determined. Intensity of observed changes of maturity ratios decreases in the following order: mineral-rich coal > matrix coal > xylite-rich coal, indicating that mineral matter, which is dominated by clays in all lithotypes, plays an important role in the isomerisation of polycyclic biomarkers and aromatic compounds. Carbon isotopic signatures of n-C25 and n-C27 alkanes, as well as δ13C values of phenathrene and cadalene are very close in studied range of maturity, confirming that isotopic signatures are useful tracers for alteration products of biological molecules. Long-chain homologues of n-alkanes exhibit slight enrichment in 12C with increasing maturity, whereas almost no change is detected in δ13C of short-chain n-alkanes. Negligible enrichment in 13C of aromatic compounds is observed during maturation. PB - European Association of Geoscientists & Engineers C3 - Conference Proceedings, 29th International Meeting on Organic Geochemistry T1 - Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis VL - 2019 DO - 10.3997/2214-4609.201903023 ER -
@conference{ author = "Kojić, I. and Bechtel, A. and Sachsenhofer, R.F. and Životić, D. and Stojanović, Ksenija A.", year = "2019", abstract = "Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis were studied. The maturity ratios based on biomarkers and alkylaromatics which showed the best applicability were determined. Intensity of observed changes of maturity ratios decreases in the following order: mineral-rich coal > matrix coal > xylite-rich coal, indicating that mineral matter, which is dominated by clays in all lithotypes, plays an important role in the isomerisation of polycyclic biomarkers and aromatic compounds. Carbon isotopic signatures of n-C25 and n-C27 alkanes, as well as δ13C values of phenathrene and cadalene are very close in studied range of maturity, confirming that isotopic signatures are useful tracers for alteration products of biological molecules. Long-chain homologues of n-alkanes exhibit slight enrichment in 12C with increasing maturity, whereas almost no change is detected in δ13C of short-chain n-alkanes. Negligible enrichment in 13C of aromatic compounds is observed during maturation.", publisher = "European Association of Geoscientists & Engineers", journal = "Conference Proceedings, 29th International Meeting on Organic Geochemistry", title = "Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis", volume = "2019", doi = "10.3997/2214-4609.201903023" }
Kojić, I., Bechtel, A., Sachsenhofer, R.F., Životić, D.,& Stojanović, K. A.. (2019). Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis. in Conference Proceedings, 29th International Meeting on Organic Geochemistry European Association of Geoscientists & Engineers., 2019. https://doi.org/10.3997/2214-4609.201903023
Kojić I, Bechtel A, Sachsenhofer R, Životić D, Stojanović KA. Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis. in Conference Proceedings, 29th International Meeting on Organic Geochemistry. 2019;2019. doi:10.3997/2214-4609.201903023 .
Kojić, I., Bechtel, A., Sachsenhofer, R.F., Životić, D., Stojanović, Ksenija A., "Maturation and isotopic changes of individual hydrocarbons in lignite lithotypes through diagenesis and early catagenesis" in Conference Proceedings, 29th International Meeting on Organic Geochemistry, 2019 (2019), https://doi.org/10.3997/2214-4609.201903023 . .