Distribution of Phenanthrene and Methylphenanthrene in Some Nigerian Oils
The distribution of Phenanthrene and the methyl analogues in Niger Delta oils was studied. Samples were obtained from various oil fields in the Niger Delta basin. The analytical method of choice used is the GC–MS. Mass chromatograms for identification of phenanthrene and methyl phenanthrene were extracted from the data file using Enhanced MSD ChemStation 2011 software by Agilent Technologies. The objectives of this study includes identifying phenanthrene and methyl phenanthrene in the oils, delineating their abundances as parametric ratios and their application in correlation study. Most of the parametric ratios used for the study showed fairly similar range values between the oils. The Pr/nC17 and Ph/nC18 plot inferred that the oils were generated from mixed organic matter, while the DBT/P and Pr/Ph plot indicated that the oils were generated from organic matter in fluvial–deltaic settings with subtle variations, Umutu oil indicated shallow marine settings. Maturity of the oils as indicated by phenanthrene and methyl phenanthrene varies from early mature stage to late mature stage. Principal Component Analysis (PCA) score plot discriminated Umutu and Utorugu oils from others and the hierarchical cluster analysis (HCA) dendrogram also indicated significant difference of Umutu oil from others.
Introduction
Phenanthrenes and the methyl analogues are aromatic compounds with three benzene rings. Phenanthrenes found in fossil material had been postulated to originate from steroids and triterpenoids. Phenanthrene and the methyl analogues can be found in both natural and anthropogenic sources. Natural sources of includes oil seeps from crude oil deposits, forest fires, volcanoes and erosion of ancient sediments [1].
The partial dealkylation of the steranes and hopanoids molecules give rise to 1– and 2– methylphenanthrene. The presence of the 3– and 9– methylphenanthrenes in ancient sediments and crude oils has been attributed to methylation of phenanthrene and rearrangement of mono–methylphenanthrene [2]. Studies have shown that
1–and 9-methylphenanthrenes are less stable than the 3– and 2–methyl phenanthrene, hence the mechanistic postulate that are rearrangement of 1–and 9- methylphenanthrene at higher temperature regimes and are used for maturation studies of compounds in crude oils [2].
Studies have shown that 1–and 9- methylphenanthrenes are abundant in younger sediments and less older formations relative to 3– and 2–methyl phenanthrenes [3]. Different analogues of methylphenanthrene have been observed to show discriminative tendencies with respect to dominant organic matter type in the matrix of the source rock. Zakir Hossain HM, Sampei Y, Roser BP showed that in a study, high abundance of 1–methylphenanthrene corresponded to the abundance of higher plant organic matter [3]. 1– and 9-methylphenanthrenes have also been observed to be enriched in immature sediments, and also with increasing enrichment of oleanane and Pristane.
In a study BudzinskiH, Garrigues P, Bernard G, Bellocq J, Hinrichs K [4], 1–methylphenanthrene has been related to terrestrial organic matter while 9– methylphenanthrene has been associated with marine organic matter.
Actually the source of phenanthrenes and the methyl analogues can be attributed to the organic matter that constitute the source rock, the Niger Delta oils are generated from source rocks that were deposited in mega sequences constituting depobelts [5], each of the depbobelts have been deposited in slightly varying environments, the combined effect of sediment deposition, sedimentary faulting, sealevel fluctuations resulted in continuous stacking of proximal fluvio–marine sediment to distal marine sediment as cyclic events with the depobelts at different age [6]. This results in organic matter with various degree of combination of various sorts of organic inputs ranging from vascular land plants, algal and bacterial mats and planktons. The resulting petroleum generated from these organic matter will bear various compositional heterogeneity, depending on the shale and the depobelt. The objectives of this study include: 1. To identify phenanthrenes and the mono methyl analogues in some Nigeria oils as listed in the samples subsection. 2. To delineate their abundance of the mono methyl analogues i.e. 3– and 2–methyl phenanthrenes, 1–and 9-methylphenanthrenes as parametric ratios.
3. Discriminate the Niger Delta oils, by relating phenanthrenes and the mono methyl analogues to environment of deposition.
Materials and Method
Samples and Sampling
The samples used from this study were petroleum crude oils, obtained from various well heads in various oil fields during flow test and well maintenance. The oil fields are Nembe Creek, Umutu, Afam, Enang, Usang, Rumuekpe, Abo, Clough Creek, Utorugo, Tebedaba and Azuzuama oil fields (Figure 1). Eleven samples were obtained in glass sample vials with Teflon caps. Samples were preserved in refrigerator before analysis.
Pre Sample Analysis
Samples were prepared for analysis by dissolving 10mg of oils in 10mls of hexane, to achieve the concentration of sample allowable to be injected into the GC–MS (Gas chromatography–mass spectrometry), which is 1mg/ml, the method of analysis adopted is whole oil analysis full scan. This means that the oil is not fractionated and all available compounds in the oil is scanned.
GC–MS Analysis
All the oils from different oil fields were subjected to GC–MS analysis using a HP5890 II GC with a split/spiltless injector linked to a HP 5972 MSD (Mass Selective Detector). The GC was temperature programmed for 40ºC–300ºC at 4ºC per minute and held at final temperature for 20 min. The carrier gas was Helium (flow rate 1ml/min., pressure of 50kPa, slit at 30ml/min). The ionization and identification was carried out in the HP 5972 MSD, which was equipped with electron voltage of 70 eV, filament current of 220µA, source temperature of 160ºC, a multiplier voltage of 1600V and interface temperature of 300ºC. The acquisition was monitored by HP Vectra 48 PC chemstation computer in both full scan mode (30ions 0.7 cps 35m dwell). HP is currently known as Agilent, UK. Phenanthrene and Methylphenanthrene were detected and identified by extracting m/z=178 and m/z=192 chromatograms respectively and from literature references. Peak integration was done using the RTE integrator [7]. Data was obtained from the percentage report from the Enhanced MSD ChemStation 2011 software by Agilent Technologies.
Copyright© Abrakasa S and Nwankwoala HO.
Abrakasa S and Nwankwoala HO. Distribution of Phenanthrene and Methylphenanthrene in Some Nigerian Oils. Pet Petro Chem Eng J 2019, 3(1): 000184.

Result and Discussion
Identification of Phenanthrene and Methylphenanthrene
Phenanthrene peak always appear as a single peak on the m/z = 178 chromatogram (Figure 1), while the methylphenanthrene peaks appears as two doublet on the m/z = 192 chromatogram (Figure 2) [7, 8]. Their abundances can be extracted by integrating with RTE integrator for the correct retention time, based on the retention time the peak area can be extracted from the percent report generated by the Enhanced MSD ChemStation 2011 software by Agilent Technologies. The extracted values were used to calculate the various parametric ratios used in the study.
Table 1 shows the various parametric ratios derived from the percent report from the chemstation software. It is observed that the DPT/P ratio is very high for the Umutu oil. The Pr/Ph ratio are all higher than 1.0. The Utorugu oil show very high Pr/nC17 ratio, relative to oils from other oil fields. As observed in Table 1, the phenanthrene and methylphenanthrene are variable in abundance. All methylphenanthrene based ratios did not show any significant difference but subtle variations which reflects minute or negligible differences.
Oil Correlation Studies
The ratios obtained can be used in oil correlation studies. They can be used to also discriminate oils [7]. Oil correlation studies entails the use of biomarkers in establishing genetic relationships of oil based on the premise that oils generated from a source rock bearing the same organic matter should have similar characteristics and should behave in similar manner when subject to robust analytical statistical processes [9].
Depositional Environment
Depositional environment entails the palaeoenvironment where the source rock that generated the oils were deposited. The Pr/nC17 and Ph/nC18 plot of had been used to preliminarily determine palaeoenvironment of deposition and potentially the organic matter type embedded in the source rock [10]. In this study, the Pr/nC17 and Ph/nC18 plot in Figure 3, infers that the organic matter embedded in the source rock generating the oils were deposited in a suboxic Copyright© Abrakasa S and Nwankwoala HO.
Abrakasa S and Nwankwoala HO. Distribution of Phenanthrene and Methylphenanthrene in Some Nigerian Oils. Pet Petro Chem Eng J 2019, 3(1): 000184.
environment. Suboxic environment contains about 0.2– 0.0 mL L-1 of dissolved oxygen in the waters during deposition of the organic matter [11].
- In this study, the plot of DBT/P and Pr/Ph (Figure 3) was employed to delineate the environment of deposition
Table 1: Ratio of Biomarker Parameters obtained from the percentage report.

Copyright© Abrakasa S and Nwankwoala HO.
Abrakasa S and Nwankwoala HO. Distribution of Phenanthrene and Methylphenanthrene in Some Nigerian Oils. Pet Petro Chem Eng J 2019, 3(1): 000184.

most matured oil being Utorugu and the less matured being Tebidaba. The plot also show an excellence inverse relationship between MPI-1 and (9+1)/(Total MP), by the MPI-1 values, the oils studied varies in maturity from early mature stage, where there is transition from kerogen to wet gas and soluble bitumen to late mature stage, which consist light oils and indicates transition to condensate and wet gas. The subtle variations in maturity indicates that generation did not commence at the same time and deposition of the source rock could have been at different times, this corroborates the depobelt concept, which postulates the deposition of the basins in mega sequences at particular time frame [5, 6].
Maturity
The maturity of oil reflects the extent to which the source rock generating the oil has transformed into the oil window, which is the burial depth at which oil generation commences. The MPI (methylphenanthrene index) has been used as one of the aromatic biomarker ratios for expressing maturity oils [14]. The MPI is expressed as MPI-1=1.5*[3-MP+2-MP]/[P+9-MP+1-MP]. The conversion to calculated vitrinite reflectance (%Rc) is achieved with the expression %Rc (MPI-1) = 0.6*MPI- 1+0.4. The plot of MPI-1 and (9+1)/(Total MP) in Figure 4 show that the maturity of the oils studied varies with the
Copyright© Abrakasa S and Nwankwoala HO.
Abrakasa S and Nwankwoala HO. Distribution of Phenanthrene and Methylphenanthrene in Some Nigerian Oils. Pet Petro Chem Eng J 2019, 3(1): 000184.

Abrakasa S and Nwankwoala HO. Distribution of Phenanthrene and Methylphenanthrene in Some Nigerian Oils. Pet Petro Chem Eng J 2019, 3(1): 000184.

The relationship between (9+1) MP/(Total MP) and (9+1)MP/(3+2)MP were observed to be a linear relationship with a correlation coefficient of 0.968, which implies about 96.8% of similarity between the two parameters in the plot. This invariably implies that (9+1)MP/(3+2)MP could be used to infer maturity statues.
A robust multivariate analysis was carried out for the parametric ratio used in this study. The PCA (principal component analysis) was done for two factors, the first explain about 44% of the difference, while the second factor explains 26% of the variations. The two factors explain 70% of the variations. The score plot (Figure 6) obtained from the principal component analysis show that Umutu and Utorugu oils are significantly discriminated from the other oils. The HCA (hierarchical cluster analysis) as shown by the dendrogram in Figure 8, infers Umutu oil is very dissimilar with other oils, however Utorugu oil is similar to other oils by 89.84% while the rest are similar to each other by 99.44%. The HCA was performed on conditions of linkage method as complete and distance measured as Square Euclidean distance.
Conclusions
The study was carried on Niger delta oils and for the purpose of identifying phenanthrene and methylphenanthrene in Niger Delta oils. GC–MS is the analytical method of choice, m/z = 178 and 192 chromatograms were extracted for phenanthrene and methylphenanthrene from the result data file using an Enhanced MSD ChemStation 2011 software by Agilent Technologies. Abundance for each compound was obtained from the percent report and the parametric ratios were calculated. The DBT/P and Pr/Ph plot showed that most of the oils were generated by organic matter deposited in fluvial–deltaic environment except the Umutu oil. MPI values used for evaluating the maturity of the oils showed that the maturity varies from early mature to late mature. The PCA score plot show that the Umutu and Utorugu oils are discriminated from others. But the HCA dendrogram show that Umutu oil significantly different from other oils by quantitative compositional variations not by classical genetic classification.
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