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Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases

Isotopic rollover refers to that δ(13)C value of a gas component decreases with maturity. Its occurrence is closely related to high productivity of shale gas. Isothermal confined pyrolysis experiments (gold capsules) were performed to simulate this phenomenon on whole rock Lucaogou and kerogens Saer...

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Autores principales: Xu, Hao, Pan, Changchun, Zeng, Lifei, Huang, Wenkui, Zhou, Chenxi, Yu, Shuang, Liu, Jinzhong, Zou, Yanrong, Peng, Ping’an
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7109094/
https://www.ncbi.nlm.nih.gov/pubmed/32235858
http://dx.doi.org/10.1038/s41598-020-62790-6
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author Xu, Hao
Pan, Changchun
Zeng, Lifei
Huang, Wenkui
Zhou, Chenxi
Yu, Shuang
Liu, Jinzhong
Zou, Yanrong
Peng, Ping’an
author_facet Xu, Hao
Pan, Changchun
Zeng, Lifei
Huang, Wenkui
Zhou, Chenxi
Yu, Shuang
Liu, Jinzhong
Zou, Yanrong
Peng, Ping’an
author_sort Xu, Hao
collection PubMed
description Isotopic rollover refers to that δ(13)C value of a gas component decreases with maturity. Its occurrence is closely related to high productivity of shale gas. Isothermal confined pyrolysis experiments (gold capsules) were performed to simulate this phenomenon on whole rock Lucaogou and kerogens Saergan, Wuerhe and Fengcheng in the absence (anhydrous) and presence of added water (hydrous) at 50 MPa, 372 °C and heating duration 0–672 h, corresponding to 0.96–1.85 EASY%Ro. For kerogen Saergan isolated from source rock with hydrogen index (HI) 159 mg/g TOC and 1.10–1.30% Ro equivalent, none of δ(13)C(1), δ(13)C(2) and δ(13)C(3) showed any rollover in both anhydrous and hydrous experiments. For Lucaogou whole rock with HI 856 mg/g TOC and 0.50–0.60%Ro, both δ(13)C(2) and δ(13)C(3) showed rollover in anhydrous experiments while all δ(13)C(1), δ(13)C(2) and δ(13)C(3) showed rollover with greater magnitude in hydrous experiments starting at 1.49–1.64 EASY%Ro. For kerogens Wuerhe and Fengcheng isolated from source rocks with HI of 550 and 741 mg/g TOC, and 1.18 and 0.96%Ro respectively, both δ(13)C(2) and δ(13)C(3) demonstrated rollover in anhydrous experiments while only δ(13)C(2) showed rollover with minor magnitude in hydrous experiments starting at 1.47–1.53 EASY%Ro. The different effects of water on isotopic rollover among samples Lucaogou, Wuerhe and Fengcheng can be ascribed to rate related isotopic fractionation. Higher generation rate leads to minor isotopic fractionation and rollover magnitude. It was suggested that isotopic rollover likely occurs in a source rock having higher amount of initial retained oil prior to bulk oil cracking and currently within the major stage of oil-cracking to gas (1.50–2.00%Ro).
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spelling pubmed-71090942020-04-06 Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases Xu, Hao Pan, Changchun Zeng, Lifei Huang, Wenkui Zhou, Chenxi Yu, Shuang Liu, Jinzhong Zou, Yanrong Peng, Ping’an Sci Rep Article Isotopic rollover refers to that δ(13)C value of a gas component decreases with maturity. Its occurrence is closely related to high productivity of shale gas. Isothermal confined pyrolysis experiments (gold capsules) were performed to simulate this phenomenon on whole rock Lucaogou and kerogens Saergan, Wuerhe and Fengcheng in the absence (anhydrous) and presence of added water (hydrous) at 50 MPa, 372 °C and heating duration 0–672 h, corresponding to 0.96–1.85 EASY%Ro. For kerogen Saergan isolated from source rock with hydrogen index (HI) 159 mg/g TOC and 1.10–1.30% Ro equivalent, none of δ(13)C(1), δ(13)C(2) and δ(13)C(3) showed any rollover in both anhydrous and hydrous experiments. For Lucaogou whole rock with HI 856 mg/g TOC and 0.50–0.60%Ro, both δ(13)C(2) and δ(13)C(3) showed rollover in anhydrous experiments while all δ(13)C(1), δ(13)C(2) and δ(13)C(3) showed rollover with greater magnitude in hydrous experiments starting at 1.49–1.64 EASY%Ro. For kerogens Wuerhe and Fengcheng isolated from source rocks with HI of 550 and 741 mg/g TOC, and 1.18 and 0.96%Ro respectively, both δ(13)C(2) and δ(13)C(3) demonstrated rollover in anhydrous experiments while only δ(13)C(2) showed rollover with minor magnitude in hydrous experiments starting at 1.47–1.53 EASY%Ro. The different effects of water on isotopic rollover among samples Lucaogou, Wuerhe and Fengcheng can be ascribed to rate related isotopic fractionation. Higher generation rate leads to minor isotopic fractionation and rollover magnitude. It was suggested that isotopic rollover likely occurs in a source rock having higher amount of initial retained oil prior to bulk oil cracking and currently within the major stage of oil-cracking to gas (1.50–2.00%Ro). Nature Publishing Group UK 2020-03-31 /pmc/articles/PMC7109094/ /pubmed/32235858 http://dx.doi.org/10.1038/s41598-020-62790-6 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Article
Xu, Hao
Pan, Changchun
Zeng, Lifei
Huang, Wenkui
Zhou, Chenxi
Yu, Shuang
Liu, Jinzhong
Zou, Yanrong
Peng, Ping’an
Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases
title Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases
title_full Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases
title_fullStr Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases
title_full_unstemmed Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases
title_short Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases
title_sort isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: implication in isotopic rollover in shale gases
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7109094/
https://www.ncbi.nlm.nih.gov/pubmed/32235858
http://dx.doi.org/10.1038/s41598-020-62790-6
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