Abstract

For a petroleum company, the oil biodegradation is an important aspect to appraisal both exploration/production and economic perspective. Black to volatile oils require different materials and techniques in comparison to those used for heavy oils. Economically, biodegradable oils has a lower market value than the non-biodegradable oil. Following the presence and absence of a set of biomarkers observed in the chromatograms and fragmentograms, it is possible an interpretation and an indentification of different levels of biodegradation . This methodology comprises the main objective of this work. The oil studied lacks “n” and iso-alkanes, the major proportion of tricyclic on the pentacyclic, the presence of demethylated compounds, plus the major proportion of diasteranes on steranes, suggesting an advanced degree of biodegradation. According to this investigation, the degree 8 of biodegradation (Peter & Moldowan, 1993), records a huge process of bacterial attack happened into the reservoir in a range of temperature from 35°C up to 50°C, from the oil/water contact.

Highlights

  • The study of oil biodegradation process has been investigated by oil industry for a long time

  • This work aims the identification and characterization of the biodegradation that happens in the oil collected in the 1-BSS-0069BS well, a siliciclastic reservoir of Paleogene age from Santos Basin

  • The Santos Basin is located in the southeast portion of Brazilian continental margin, it is limited to the north by Cabo Frio Arch, to the south by Florianópolis Arch, to the east by bathymetry of 3000 m and to the west by Cretaceous hinge line

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Summary

Introduction

The study of oil biodegradation process has been investigated by oil industry for a long time. Its importance lies in the fact that the biodegradation level defines what kind of explotation and refine techniques will be used. It will need the appropriated industry installations to diferent levels of biodegradation. The Santos Basin is located in the southeast portion of Brazilian continental margin, it is limited to the north by Cabo Frio Arch, to the south by Florianópolis Arch, to the east by bathymetry of 3000 m and to the west by Cretaceous hinge line. It has an overall area of 350.000 km of extention (Mohriak, 2003)

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