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Speciation of the organic sulfur forms in a recent sediment and type I and II-S kerogens by high-pressure temperature-programmed reduction

机译:高压程序升温还原法在近期沉积物中和I型和II-S型干酪根中形成的有机硫形态

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摘要

Temperature-programmed reduction (TPR) with a well-swept fixed-bed reactor operating at 15 Mpa of hydrogen pressure has facilitated the speciation of the organic sulfur forms in coals and petroleum source rocks through complete hydrodesulfurization with typically 75-80/100 of the sulfur being released as hydrogen sulfide with the remaining 20-25/100 occurring as primarily thiophenic compounds in the oils obtained in high yield. In his study, the technique has been applied to kerogens isolated from a series of unconsolidated Peru margin sediments, and for comparison, to type I and II-S kerogens (Goynuk oil shale and Monterey Fm, respectively) from immature organic-rich rocks.
机译:程序设计良好的固定床反应器在氢气压力为15 Mpa的条件下进行程序升温还原(TPR),通过完全加氢脱硫,通常以75-80 / 100的氢进行脱硫,从而促进了煤和石油烃源岩中有机硫形式的形成。硫以硫化氢的形式释放出来,剩余的20-25 / 100主要以噻吩化合物形式出现在高收率的油中。在他的研究中,该技术已应用于从一系列未固结的秘鲁边缘沉积物中分离出的干酪根,并且为了进行比较,还应用于来自未成熟有机质岩石的I型和II-S型干酪根(分别为Goynuk油页岩和Monterey Fm)。

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  • 来源
    《Energy & Fuels》 |1997年第3期|p.532-538|共7页
  • 作者单位
  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 TK-;
  • 关键词

  • 入库时间 2022-08-18 00:26:53

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