Hydrocarbon gas generation from pyrolysis of extracts and residues of low maturity solid bitumens from the Sichuan Basin, China. (January 2017)

• Record Type: Journal Article
• Authors: Wang, Zixiang; Wang, Yongli; Wu, Baoxiang; Wang, Gen; Sun, Zepeng; Xu, Liang; Zhu, Shenzheng; Sun, Lina; Wei, Zhifu
• Is Part Of: Organic geochemistry. Volume 103(2017:Feb.)
• Page Start: 51
• Page End: 62
• Publication Date: 2017-01
• Subjects: Hydrocarbon gas generation -- Sinian-Cambrian -- Bitumen "A" -- Insoluble residual -- Stable carbon isotope -- Kinetics; Organic geochemistry -- Periodicals; Biogeochemistry -- Periodicals; Géochimie organique -- Périodiques; 553.205
• DOI: 10.1016/j.orggeochem.2016.10.011
• Languages: English
• ISSNs: 0146-6380

Abstract

Highlights: Two sets of pyrolysis experiments were performed at different heating rates. Bitumen "A" and extracted residues have similar gas evolution profiles. Three key plots classify the evolution of hydrocarbon gas generation. Hydrocarbon generation history of both sample types have been reconstructed. Abstract: Two sets of pyrolysis experiments were performed on bitumen "A" (BA) and extracted organic matter (ER) from low-maturity solid bitumen at heating rates of 2 °C/h and 20 °C/h in confined systems (gold capsules). The main observations can be listed as follows: (1) BA and ER have high generation potential of hydrocarbons and were a significant secondary hydrocarbon source. (2) Both have similar evolutionary characteristics of hydrocarbon gas generation, and have high C1 /C1–5 values than those from an Ordovician normal oil. Ea distributions of the methane generated from pyrolysis of BA and ER is far lower than that of Ordovician normal oil. (3) The evolution of stable carbon isotope values of individual hydrocarbon gases can be divided into three stages. Plots of ln C1 /C2 versus ln C2 /C3, δ 13 C1 –δ 13 C2 versus ln(C1 /C2 ) and δ 13 C2 –δ 13 C3 versus ln(C2 /C3 ) clearly illustrate the characteristics of hydrocarbon gases generated from BA and ER at different thermal maturity stages. (4) Basin modelling reconstructions of the hydrocarbon generation history of BA and ER in Sinian and Cambrian strata respectively indicate: Hydrocarbon gases generation from ER started in the Middle Jurassic, and ended in the Early Cretaceous with a maturity equivalent to Easy%Ro ≈ 2.2%. The final conversion rate of C1–5 and C1 are 0.71 and 0.48, respectively. Hydrocarbon gas generation from BA started in the Early Jurassic, and ended in the Early Cretaceous with an Easy%Ro ≈ 3.0%. The final conversion rate of C1–5 and C1 are 0.90 and 0.81, respectively.