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Characterization of Crude Oil, Asphaltenes Based on Bismuth (Bi), Thorium (Th) and Uranium (U) Levels: Potential Environmental Impact

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DOI: 10.4236/jep.2016.72017    2,627 Downloads   2,899 Views   Citations

ABSTRACT

The actinides (Th, U) and bismuth exist at ultra-trace levels in petroleum and have rarely been reported to characterize combustible fuels. However, high-performance mass spectrometry coupled with plasma technology has succeeded in reaching detectable limits in the ng/L range, and has thus made such characterization possible. Crude oil is used as sludge for certain agricultural purposes; and asphaltenes are converted to by-products for constructing car parks, pavements, roofing material and thoroughfares. Our study uncovers an area that has not been previously explored and we examine the potential ecotoxicology of bismuth, thorium and uranium in this context. Asphaltene derivatives were separated from crude oil samples via multiple-stage soxhlet extraction. The virgin crude oil and isolated asphaltenes were investigated for Bi, Th and U content using a high-powered hyphenated facility. A Perkin Elmer SCIEX DRC-e ICP coupled to a quadrupole mass spectrometer was employed to detect the elements of interest. The levels of these elements occurred in the mg/L (ppm) and μg/L (ppb) ranges and were compared for crude oil and asphaltenes. The data showed higher levels of the detected elements in the asphaltene phase. The feasibility of applying the experimental results as a fingerprinting tool for provenancing crude oil and asphaltenes was examined. The results are discussed from the perspective of bismuth and actinide pollution and its long-term impact on sustainable development.

Received 19 January 2016; accepted 19 February 2016; published 22 February 2016

1. Introduction

Bismuth, thorium and uranium occur naturally at ultra-trace levels in soils, rocks and geochemical formations [1] [2] . Their presence in crude oil is as a result of leaching from subterranean rock formations and reservoirs [3] . The environmental impact of these elements is relatively underexplored due to the lack of suitably sensitive instrumentation to detect them. The advent of ICP-MS technology, however, has facilitated measurement of these heavy metals. Of significance is that all three of them possess relatively long-lived radioisotopes that are embedded in the earth’s crust. The health effects relating to these metals of interest depend on how widely humans are exposed to them. In the case of soils, they are usually confined to agricultural areas so human exposure is limited. However, crude oil in the form of sludge is used as a soil-conditioner on land farms [4] [5] and asphaltenes are converted into material for constructing roads, paving for malls, roofing and car parks [6] [7] . Human exposure to the converted forms of crude oil and asphaltenes is, therefore, much wider than expected. Low-level chronic pollution could result, necessitating investigation of the potential environmental effects [4] .

The most critical threat that bismuth and these particular actinides can present is pollution of aquatic resources and underground water supplies. Most oil producing countries are arid and there is a chronic water shortage in many of these regions [8] [9] . Contamination of water supplies by toxins of this nature would be highly deleterious to the environment and would seriously affect sustainability. Sustainable development refers to growth of our planet in all forms so that humans and other organisms can survive and possess a high quality of life [10] [11] . Any trace of such pollution could pose a threat to sustainability [12] . The main objective of this study was to investigate the levels of bismuth, thorium and uranium in crude oil and asphaltenes and explore their potential impact on the environment. Possible use of our results as a “fingerprinting” tool and the feasibility of “mining” crudes and asphaltenes for these metals are novel aspects that have emerged from this work.

2. Material and Methods

2.1. Soxhlet Extraction/ICP

2.2. Quadrupole Mass Filter

The quadrupole mass filter isolates ions and consists of four rods made of molybdenum (Figure 1). The opposite pairs of rods are supplied with AC and DC voltages and the voltages are rapidly switched in combination with an RF field [7] . This results in a sequentially changing electrostatic field which allows only ions of a single mass-to-charge ratio (m/e) to pass through the filter at a given instant in time. Even though the switching and the mass selection process is sequential, this happens at a very rapid rate so that the quadrupole mass filter can separate up to 2400 amu (atomic mass units) per second, making it an ultra-sensitive instrument for multi elemental analysis. The ICP-MS was standardized with certified solutions (Fluka 70007; 10.00 ppb per element). Repeatability produced relative standard deviations <5% indicating that the system’s performance was satisfactory (Table 1). An internal standard was used to adjust any minor perturbations due to instrumental drift. Samples and standards were prepared in mild acidic aqueous solutions. The software played a major role in background correction and eliminating matrix effects. The technique is highly sensitive compared to other analytical techniques [15] -[20] .

3. Results and Discussion

3.1. Elemental Profiles

Bismuth, thorium and uranium have some relatively long-lived radioactive isotopes that occur naturally in the earth’s crust [1] . In the case of bismuth, Bi-209 was considered to be stable until 2003, when it was found to

Figure 1. Quadrupole mass filter in the ICP-MS.

Table 1. Repeatability test of the ICP-MS for various elements (μg/L) in an aqueous standard showing the mean, standard deviation (SD) and relative standard deviation (SD%).

have a half-life of about 2 × 1019 years [1] . Thorium has one partially stable isotope, Th-232, with a half-life of about 2 × 106 years. And uranium has two relatively stable isotopes U-238 (half-life, 5 × 109 years) and U-235 (half-life, 7 × 108 years), of which U-238 predominates in nature [1] . The elemental profiles of each of these elements in crude oil and asphaltene samples are discussed below.

Bismuth (Z = 83): Investigating bismuth levels in petroleum has not been previously documented. The profile in Figure 2 shows that bismuth is highly concentrated in the asphaltene fractions. This pattern is consistent with crude oil samples displaying much lower levels. Comparison between the levels in crude oil and asphaltene samples reveals that concentrations differ by about a factor of fifty in some cases. Bi levels in soil are roughly 1 - 10 µg/kg (1 - 10 ppb), and, in surface ocean waters, about 0.5 µg/L (0.5 ppb). The levels in potable water are not known, and could possibly be surmised to be below 0.1 ppb. The maximum concentration in our asphaltenes is about 65 mg/L (65 ppm), which is extremely elevated. These abnormal levels could have a significant impact on the environment and create an unwanted threat, especially to water supplies. The bismuth itself originates from source rock and underground formations in contact with the crude. It is usually present in the sulphide and

Figure 2. Bismuth levels in crude oil and asphaltene samples.

oxide forms. The data in our previous papers [6] [7] suggest that metals tend to concentrate in the asphaltene phase, perhaps at the point of separation. According to Figure 2, the maximum level in crude oil is roughly 5 mg/L, which is also above expected levels. It is interesting to note that the levels in the asphaltene samples vary widely in the range 20 - 70 mg/L, and the range in crude oil is roughly 2 - 6 mg/L. The reason for this wide variation is not clear and could be due to uneven leaching of source rock. These elevated levels could be useful in diagenetic studies to provide important clues in geochemical mechanisms [3] .

Thorium (Z = 90): The environmental impact of thorium in petroleum products has not been widely reported and is one of the essential features of this study. The general profile of thorium (Figure 3) differs from that of bismuth, in that some crude oil samples display higher levels than the asphaltene samples. This particular “anomaly” is present only in the profile of this element―and is conspicuously absent in those for Bi and U. Thorium is present in the earth’s mantle mainly in the form of phosphates (monazite), and the metal has pronounced allotropic forms, some of which could have a stronger affinity for crude oil than the asphaltene phase [7] . This allotropic feature, therefore, could possibly be attributed to greater retention in crude oil (in some cases) when the asphaltenes are separated. Thorium occurs in soil at levels between 1 - 10 mg/kg. The levels presented in Figure 3 are within the expected range, except for a single asphaltene sample, which reflects a level slightly above 20 mg/L. According to Figure 3, the maximum level in crude oil is roughly 10 mg/L, which is at the limit of expected levels. Of interest, is that the levels in the asphaltene samples vary roughly in the range 2 - 20 mg/L, and the range in crude oil is roughly 1 - 10 mg/L. Such variations are appreciable and cannot be used to either characterize or identify asphaltenes or crude based on thorium concentrations. However, this fluctuation in levels signifies irregular leaching of the earth’s crust (as in the case of bismuth) [3] .

Uranium (Z = 92): U-238 and U-234 are “primordial” isotopes of uranium and predominate in nature [1] . A comparison between the levels in crude oil and asphaltene samples (Figure 4) indicates that uranium concentrations in the asphaltene fractions are relatively higher, with depletion to levels below 0.50 mg/L in crude. This trend is similar to the one encountered in Figure 2 for Bi. However, the experimentally determined levels of uranium are much lower in comparison with the Bi levels. Uranium concentration in soils is about 2 mg/kg, which is in the region of the detected levels in asphaltenes. There is no evidence of elevated concentrations in the asphaltene samples, and the range is comparatively narrow, varying between 1 - 3 mg/L. The levels in the crude oil samples are not wide either, and vary between 0.2 - 0.5 mg/L. Seawater contains about 3.3 µg/L of uranium and is considered to be a useful source of uranium. Of the three elements studied here the most diminished range for asphaltenes is encountered in uranium. This suggests that asphaltene samples could possibly be identified on the basis of their uranium concentration. Clearly in Figure 4, most of the asphaltene concentrations fall between 1.0 - 1.5 mg/L, and this range could be used for purposes of characterization. Of course, outliers will occur, as seen in Figure 4, but the data suggest that in the majority of cases it may be possible to distinguish asphaltene samples on the basis of their uranium levels.

Figure 3. Thorium levels in crude oil and asphaltene samples.

Figure 4. Uranium levels in crude oil and asphaltene samples.

3.2. Fingerprinting Tool

The novelty that emerges from this work is the possibility of using the foregoing data as a “fingerprinting” tool to identify crudes and asphaltenes. It is well known that Ni/V ratios are used to characterize asphaltenes and are employed in “fingerprinting” studies [7] . Of significance, is that “fingerprinting” is linked to provenancing [21] , so the primary purpose of employing such ratios is to identify the source and location of the asphaltenes. It is acknowledged that Ni/V ratios could be used to identify the oil field linked to the asphaltene specimen [7] . However, the problem is that if there is nickel contamination from the pipeline these ratios are not reliable. It is therefore, necessary to seek more reliable parameters devoid of contamination. Figure 5 depicts plots of Bi/Th, Bi/U and Th/U concentration ratios, for each sample, to determine whether some trend or pattern exists to identify or “fingerprint” asphaltenes or crude oil on the basis of elemental content. It is clear from Figure 5 that the Bi/U ratios are widely scattered, which makes this particular ratio ineffective for use as a fingerprinting tool. However, careful inspection of Figure 5 reveals that Bi/Th ratios for crude oil samples are more or less consistent (encircled) and based on these data it is feasible that Bi/Th ratios in the range 0.5 - 1 could be used to “fingerprint” crude oil. On the other hand, in the case of asphaltenes, the experimental results associated with Th/U ratios in Figure 5 (encircled) are equally consistent and suggest that it is equally feasible to employ these ratios

Figure 5. Plots showing Bi/Th, Bi/U and Th/U ratios for “fingerprinting”.

to “fingerprint” asphaltenes. Th/U ratios could be used as a possible alternative to Ni/V ratios and are widely impervious to contamination from general sources such as pipelines and chemical treatment. Th/U ratios in the range 3 - 5 could characterize the asphaltene samples of interest. A point to stress is that previously these ratios were not available because measuring devices for detection were not adequately sensitive. However, as aforementioned, ICP-MS performs at ultra-sensitive levels and makes “fingerprinting” of this nature possible.

3.3. Environmental Impact

The environmental effects of bismuth, thorium and uranium in crudes and asphaltenes are obscure largely because little or no work has been done in this area, mainly due to the lack of sensitive instrumentation (as aforementioned) [2] . The data in Figures 2-4 show without doubt that the levels of Bi are highly elevated. Collectively, the physiological effects and bio-distribution of Bi are the subject of continued research [22] . However, it is known that Bi at elevated levels could affect the liver and kidneys. Abnormal levels of toxins in crude oil and asphaltenes could reach water resources through constant leaching and run-off. Water pollution is a major global concern and clean drinking water is in short supply in many oil producing countries. Although thorium and uranium levels in Figure 3 and Figure 4 are comparable with those in soil, asphaltenes and crude oil in converted forms (such as sludge and road materials) tend to be associated with wider human exposure, and contamination of water supplies poses the most serious hazard. Like bismuth, thorium poisoning is under considerable investigation [22] , but it has come to light that ingested thorium at raised levels could bind to protein responsible for transporting iron in blood, and thus affect the liver, kidneys and bones. The main health effect with elevated uranium is kidney toxicity. These metals are naturally occurring and have long-lived radioisotopes; therefore, radiological effects from all three elements could present a potential long-term hazard [22] . Constant ingestion of low-level radiation (especially alpha particles) from water pollution could result in chronic physiological and dermal disorders. Depletion of these metals in crudes and asphaltenes is therefore, essential and could have mutually beneficial effects, as discussed below.

3.4. “Mining” Asphaltenes and Crude Oil

4. Conclusion

The development of our research produced two novel features: i) the use of bismuth and actinide ratios as potential fingerprinting tools; and ii) the prospect of “mining” enriched asphaltenes and crudes for Bi, Th and U. The latter could lead to reduced environmental effects, which could be potentially significant, especially if the asphaltenes in converted forms are exposed to the environment. The most critical threat is that of water contamination, which can be avoided by chemical treatment and demetallisation of these combustible fuels prior to deploying them for construction and other purposes.

Acknowledgements

The authors wish to thank the Petroleum Institute for financial support.

NOTES

*Corresponding authors.

Conflicts of Interest

The authors declare no conflicts of interest.

Cite this paper

Elhameed, A. , Pillay, A. , Nunn, R. and Stephen, S. (2016) Characterization of Crude Oil, Asphaltenes Based on Bismuth (Bi), Thorium (Th) and Uranium (U) Levels: Potential Environmental Impact. Journal of Environmental Protection, 7, 190-197. doi: 10.4236/jep.2016.72017.

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