Formation and identification of unresolved complex mixtures in lacustrine biodegraded oil from Nanxiang Basin, China.

ScientificWorldJournal

Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China.

Published: May 2015

AI Article Synopsis

  • A new method using two-dimensional gas chromatography/time-of-flight mass spectrometry (GC × GC/TOFMS) has been created to analyze complex mixtures in biodegraded oils from the Nanxiang Basin in China, revealing how different types of oil degrade.
  • The study found that as oil degradation progresses from B330 to G574, there's a gradual loss of diverse compounds, leading to similar relative contents and minor polarity differences among remaining ones, causing them to coelute and form unresolved complex mixtures (UCMs).
  • UCMs consist mainly of cyclic alkanes, classified into six groups, with the first two classes originating from degradation-resistant hydrocarbons, while the latter classes appear to form from microbial transformations during oil degradation.

Article Abstract

A comprehensive two-dimensional gas chromatography/time-of-flight mass spectrometry (GC × GC/TOFMS) method has been developed for the formation and identification of unresolved complex mixtures (UCMs) in lacustrine biodegraded oils that with the same source rock, similar maturity, and increasing degradation rank from Nanxiang Basin, China. Normal alkanes, light hydrocarbons, isoprenoids, steranes, and terpanes are degraded gradually from oil B330 to oil G574. The compounds in biodegraded oil (oil G574) have fewer types, the polarity difference of compounds in different types is minor, and the relative content of individual compounds is similar. All the features make the compounds in biodegraded oil coelute in GC analysis and form the raised "baseline hump" named UCMs. By injecting standard materials and analyzing mass spectrums of target compounds, it is shown that cyclic alkanes with one to five rings are the major components of UCMs. Furthermore, UCMs were divided into six classes. Classes I and II, composed of alkyl-cyclohexanes, alkyl-naphthanes, and their isomers, are originated from the enrichment of hydrocarbons resistant to degradation in normal oils. Classes III ~ VI, composed of sesquiterpenoids, tricyclic terpanes, low molecular steranes, diasteranes, norhopanes, and their isomers, are probably from some newly formed compounds during the microbial transformation of oil.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4142316PMC
http://dx.doi.org/10.1155/2014/102576DOI Listing

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