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名   称 Influence of carbonate minerals on the pyrolysis and phase behavior of oil
科技资源标识 CSTR:11738.14.NCDC.XDA14.PP4457.2024
DOI 10.1016/j.marpetgeo.2021.105374
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摘   要 The concept that reservoir minerals can affect oil cracking behavior is widely accepted by geochemists. However,
the role of carbonate minerals on the thermal evolution of oil is still not well understood. This is especially true
for dolomite, which is one of the most important carbonate cements. To investigate its influence, a series of
laboratory simulation experiments of a crude oil with various carbonate minerals, including calcite, magnesite,
and dolomite was conducted. The simulation experiments were carried out using a closed system of flexible gold
capsules at temperatures of 250–600◦С at a heating rate of 20 ◦C/h and a constant pressure of 50 MPa. The
results indicate that dolomite/magnesite might promote the generation of sulfate radical ion (SO4
2− ). Subse_x0002_quently, the presence of SO4
2− can initiate thermochemical sulfate reduction reaction with the help of minor
water and H2S, resulting in the destruction of gaseous hydrocarbons. Meanwhile, the influence of dolomite on the
composition of oil can further affect its phase behavior, especially in the gas window (Easy Ro range of
1.19–1.47% in the experiments). For the investigated oil, at Easy Ro of 1.47%, the presence of dolomite will
increase the cricondentherm (ca. 35 ◦C) and decrease the cricondenbar (ca. 1.3 MPa) compared to those of pure
oil
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作者 Liangliang Wu
数据量 19.5 MiB
论文类型: journal
论文网址: https://doi.org/10.1016/j.marpetgeo.2021.105374
期刊名称: Marine and Petroleum Geology
出版时间: 2021-12-01
引用和标注
数据引用
Liangliang Wu. Influence of carbonate minerals on the pyrolysis and phase behavior of oil. 国家冰川冻土沙漠科学数据中心(http://www.ncdc.ac.cn), 2024. https://cstr.cn/CSTR:11738.14.NCDC.XDA14.PP4457.2024.
Liangliang Wu. Influence of carbonate minerals on the pyrolysis and phase behavior of oil. 国家冰川冻土沙漠科学数据中心(http://www.ncdc.ac.cn), 2024. https://www.doi.org/10.1016/j.marpetgeo.2021.105374.
许可协议
知识共享许可协议   本作品采用 知识共享署名 4.0 国际许可协议进行许可。

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