Formation of H2S and sulfur-rich bitumen from a reservoired heavy oil in the presence of elemental sulfur

被引:20
|
作者
Kowalewski, Isabelle [1 ]
Schaeffer, Philippe [2 ]
Adam, Pierre [2 ]
Dessort, Daniel [3 ]
Fafet, Anne [1 ]
Carpentier, Bernard [1 ]
机构
[1] IFP Energies Nouvelles, Geol Geochem Div, F-92506 Rueil Malmaison, France
[2] Univ Strasbourg, Lab Biogeochim Mol, ECPM, UMR 7177, F-67200 Strasbourg, France
[3] CSTJF, Total, F-64000 Pau, France
关键词
THERMOCHEMICAL SULFATE REDUCTION; GEOCHEMICAL SIGNIFICANCE; HYDROGEN-SULFIDE; SOLID BITUMENS; ABU-DHABI; BASIN; PRECIPITATION; GENERATION; ORIGIN; OMAN;
D O I
10.1016/j.orggeochem.2010.05.002
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The hypothesis of a low temperature natural "vulcanization" process as a potential mechanism for the formation of insoluble bitumen and H2S in reservoirs which have not undergone biodegradation, high thermal stress, or thermochemical sulfate reduction (TSR) has been investigated using laboratory simulation experiments. The experiments, involving elemental sulfur (S-32 and S-34), a low maturity oil and water at 200 degrees C in sealed gold tubes, clearly showed that elemental sulfur is able to Induce the formation of H2S, polar compounds (resins and asphaltenes) and insoluble bitumen most likely by way of sulfur cross-linking processes Specific organic sulfur compounds (thiophenes, dithiophenes and thienothiophenes) formed by the reaction of sulfur and hydrocarbons may be potential markers of such a process, but remain to be detected in natural samples. (C) 2010 Elsevier Ltd. All rights reserved
引用
收藏
页码:951 / 958
页数:8
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