A set of eight tar sand samples with identical source, from sedimentary facies of the Pirambóia Formation, Paraná Basin, provides an interesting opportunity to assess the biodegradation extent of bitumens using high-resolution mass spectrometry with Orbitrap mass analyzer. The results suggest that acidic compounds have been degraded by microorganisms, since the O 2 and O 3 classes were lower to bitumens from dry interdune facies, the most biodegraded. It was also proposed a new parameter to evaluate biodegradation, DBE ratio (ratio between acidic species with the same number of double bond equivalent), that was used together with the already proposed A/C ratio (acyclic to cyclic naphthenic acids), both obtained from O 2 class distribution. The bitumens from dry interdune facies presented the highest DBE ratios and lowest A/C ratios, which suggested that these parameters can be used to assess the extent of bitumen biodegradation in which the DBE ratios increase and the A/C ratios decrease with increasing biodegradation.
Keywords: heavy oil, biodegradation, heteroatom class, sedimentary facies, Paraná Basin
IntroductionIt is expected that the production of heavy, biodegraded oil will increase worldwide as lighter conventional oil reserves are depleted.1 This shortage of light oil makes these less attended energy resources more attractive, especially considering that heavy oils are currently 10 times more abundant than conventional oils.2 Even with the fluctuation of crude oil prices, unconventional oil probably will gain a considerable market share in the short term, although conventional oil remains as a major source of global oil market in the long term.3 Therefore, these unconventional oils are potential resources that could be used to fulfill current and future energy requirements. Among these unconventional oils, bitumens from tar sand reservoirs have great potential to assist in meeting the world's rising energy demand. 4,5 The occurrence of tar sand bitumens is common in many basins worldwide, but they are mainly found in shallow reservoirs on the flanks of foreland basins in North and South America. The largest accumulations are the supergiant deposits of tar sands in the Alberta (Canada) and Eastern Venezuelan (Venezuela) basins. 6,7 In Brazil, there are tar sand bitumen accumulations in the Paraná Basin, mostly occurring in sandstones of the Triassic Pirambóia Formation. These tar sands are restricted to the eastern margin, with approximately 25 known localities spread over two areas in the state of São Paulo. The Anhembi Exudation area is one of the major heavy oil exudations in this area. The oil reservoir was estimated at 5,712,000 barrels based on a mean content of 5.5% weight oil. These bitumen deposits have a high viscosity and medium-to-high sulfur content (2-3% by weight).
8The Paraná Basin is a very large intracratonic basin in which the tar sand accumulations are attributed to the Irati-Pirambóia petroleum system. 8,9 In the Pirambóia Formation, there are four different sedimentary eolic facies...