Effects of high temperatures on biomarker ratios during oil-to-gas cracking experiments at two pressures. (November 2016)

• Record Type: Journal Article
• Authors: Chen, Zhonghong; Simoneit, Bernd R.T.; Wang, T.-G.; Huang, Wei; Yan, Detian; Ni, Zhiyong; Liu, Keyu
• Is Part Of: Organic geochemistry. Volume 101(2016:Dec.)
• Page Start: 108
• Page End: 131
• Publication Date: 2016-11
• Subjects: Biomarkers -- Sterane -- Tricyclic terpanes -- Pentacyclic triterpanes -- Thermal maturity -- Oil cracking -- Pressure -- High temperature; Organic geochemistry -- Periodicals; Biogeochemistry -- Periodicals; Géochimie organique -- Périodiques; 553.205
• DOI: 10.1016/j.orggeochem.2016.08.011
• Languages: English
• ISSNs: 0146-6380

Abstract

Highlights: Biomarker ratios show non-linear trends during oil-to-gas cracking. High temperatures dominantly control biomarker ratios compared to pressure. Most tricyclic terpane ratios show maximum concentrations at 500 °C. Change of most biomarker ratios with rising temperature are retarded at 20 MPa. Biomarkers may be more affected by pressure in deep basins than currently thought. Abstract: Variations in biomarker concentrations, including tricyclic terpanes, tetracyclic terpanes, pentacyclic triterpanes, steranes, methylphenanthrenes and triaromatic steranes, were investigated at two different pressures (0.1 and 20 MPa) in multiple laboratory simulation experiments of oil-to-gas cracking. The low-maturity non-marine oil samples used in the study are from the Paleogene Shahejie Formation in the Dongying Depression, Bohai Bay Basin, eastern China. The oils were pyrolyzed to gas at elevated temperatures (300–650 °C) in an autoclave. The oil residue was sampled and analyzed at 50 °C temperature intervals. The results show that changes in biomarker concentrations are controlled mainly by temperature, while high pressures exert non-linear suppression effects on these variations. There appear to be different evolution regimes based on biomarker cracking and generation rates in the primary (400–500 °C for 0.1 MPa and 450–550 °C for 20 MPa) and secondary (500–650 °C for 0.1 MPa and 550–650 °C for 20 MPa) oil-to-gas cracking stages. Generally, the biomarker ratio differences are considerable in the early primary oil-to-gas cracking stage but decrease substantially in the later primary oil-to-gas cracking stage. The differences remain stable at high temperatures in the secondary oil-to-gas cracking stage. These oil-to-gas pyrolysis experiments reveal the characteristics of biomarker ratios, which are quite different from their distribution within the conventional "liquid window" at moderate maturity level. They provide new insights on oil biomarker maturity parameters under high temperatures and the change of oil and gas in deep buried basins.