Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter

Abstract In order to investigate the impact of U-ore on organic matter maturation and isotopic fractionation, we designed hydrous pyrolysis experiments on Type-II kerogen samples, supposing that the water and water–mineral interaction play a role. U-ore was set as the variable for comparison. Meanwh...

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Autores principales: Yu-Wen Cai, Shui-Chang Zhang, Kun He, Jing-Kui Mi, Wen-Long Zhang, Xiao-Mei Wang, Hua-Jian Wang, Chao-Dong Wu
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Publicado: KeAi Communications Co., Ltd. 2017
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Acceso en línea:https://doaj.org/article/f640c10e394a4f428f307721a8d74046
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spelling oai:doaj.org-article:f640c10e394a4f428f307721a8d740462021-12-02T00:52:51ZEffects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter10.1007/s12182-017-0161-61672-51071995-8226https://doaj.org/article/f640c10e394a4f428f307721a8d740462017-05-01T00:00:00Zhttp://link.springer.com/article/10.1007/s12182-017-0161-6https://doaj.org/toc/1672-5107https://doaj.org/toc/1995-8226Abstract In order to investigate the impact of U-ore on organic matter maturation and isotopic fractionation, we designed hydrous pyrolysis experiments on Type-II kerogen samples, supposing that the water and water–mineral interaction play a role. U-ore was set as the variable for comparison. Meanwhile, anhydrous pyrolysis under the same conditions was carried out as the control experiments. The determination of liquid products indicates that the presence of water and minerals obviously enhanced the yields of C15+ and the amounts of hydrocarbon and non-hydrocarbon gases. Such results may be attributed to water-organic matter reaction in the high-temperature system, which can provide additional hydrogen and oxygen for the generation of gas and liquid products from organic matter. It is found that δD values of hydrocarbon gases generated in both hydrous pyrolysis experiments are much lower than those in anhydrous pyrolysis. What is more, δD values are lower in the hydrous pyrolysis with uranium ore. Therefore, we can infer that water-derived hydrogen played a significant role during the kerogen thermal evolution and the hydrocarbon generation in our experiments. Isotopic exchange was facilitated by the reversible equilibration between reaction intermediaries with hydrogen under hydrothermal conditions with uranium ore. Carbon isotopic fractionations of hydrocarbon gases were somehow affected by the presence of water and the uranium ore. The increased level of i-C4/n-C4 ratios for gas products in hydrous pyrolysis implied the carbocation mechanism for water-kerogen reactions.Yu-Wen CaiShui-Chang ZhangKun HeJing-Kui MiWen-Long ZhangXiao-Mei WangHua-Jian WangChao-Dong WuKeAi Communications Co., Ltd.articleOrganic–inorganic interactionHydrous pyrolysisStable isotopesU-oreCarbocation mechanismScienceQPetrologyQE420-499ENPetroleum Science, Vol 14, Iss 2, Pp 315-329 (2017)
institution DOAJ
collection DOAJ
language EN
topic Organic–inorganic interaction
Hydrous pyrolysis
Stable isotopes
U-ore
Carbocation mechanism
Science
Q
Petrology
QE420-499
spellingShingle Organic–inorganic interaction
Hydrous pyrolysis
Stable isotopes
U-ore
Carbocation mechanism
Science
Q
Petrology
QE420-499
Yu-Wen Cai
Shui-Chang Zhang
Kun He
Jing-Kui Mi
Wen-Long Zhang
Xiao-Mei Wang
Hua-Jian Wang
Chao-Dong Wu
Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
description Abstract In order to investigate the impact of U-ore on organic matter maturation and isotopic fractionation, we designed hydrous pyrolysis experiments on Type-II kerogen samples, supposing that the water and water–mineral interaction play a role. U-ore was set as the variable for comparison. Meanwhile, anhydrous pyrolysis under the same conditions was carried out as the control experiments. The determination of liquid products indicates that the presence of water and minerals obviously enhanced the yields of C15+ and the amounts of hydrocarbon and non-hydrocarbon gases. Such results may be attributed to water-organic matter reaction in the high-temperature system, which can provide additional hydrogen and oxygen for the generation of gas and liquid products from organic matter. It is found that δD values of hydrocarbon gases generated in both hydrous pyrolysis experiments are much lower than those in anhydrous pyrolysis. What is more, δD values are lower in the hydrous pyrolysis with uranium ore. Therefore, we can infer that water-derived hydrogen played a significant role during the kerogen thermal evolution and the hydrocarbon generation in our experiments. Isotopic exchange was facilitated by the reversible equilibration between reaction intermediaries with hydrogen under hydrothermal conditions with uranium ore. Carbon isotopic fractionations of hydrocarbon gases were somehow affected by the presence of water and the uranium ore. The increased level of i-C4/n-C4 ratios for gas products in hydrous pyrolysis implied the carbocation mechanism for water-kerogen reactions.
format article
author Yu-Wen Cai
Shui-Chang Zhang
Kun He
Jing-Kui Mi
Wen-Long Zhang
Xiao-Mei Wang
Hua-Jian Wang
Chao-Dong Wu
author_facet Yu-Wen Cai
Shui-Chang Zhang
Kun He
Jing-Kui Mi
Wen-Long Zhang
Xiao-Mei Wang
Hua-Jian Wang
Chao-Dong Wu
author_sort Yu-Wen Cai
title Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
title_short Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
title_full Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
title_fullStr Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
title_full_unstemmed Effects of U-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
title_sort effects of u-ore on the chemical and isotopic composition of products of hydrous pyrolysis of organic matter
publisher KeAi Communications Co., Ltd.
publishDate 2017
url https://doaj.org/article/f640c10e394a4f428f307721a8d74046
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