Reservoir Characterization. Группа авторов

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Total organic carbon content (TOC) and hydrocarbon generating potential of the carbonate samples were analyzed by Leco carbon analyzer and Rock-Eval pyrolysis, respectively. Solvent extraction was used to remove bitumen from the source rocks, while liquid chromatography (LC), FID- gas chromatography (FID-GC), and gas chromatograph-mass spectrometry (GC-MS) analyses were performed on both the oils and selected bitumen. Selected results from these analyses are discussed in the following chapter.

4.3 Results and Discussions

All 6 source rocks investigated are organically very rich (Table 4.1), showing TOC content in the 3.35% to 11.31% range. Results of Rock-Eval pyrolysis, such as hydrogen index (HI) and Tmax values indicates that all carbonaceous source rocks analyzed are highly enriched in sapropelic (Type II) kerogen (Figure 4.1) which based on Tmax-values appear to be thermally within the oil window (Figure 4.2). The pyrolysis results also indicate that the kerogen present in these source rocks show relatively high pyrolysis S2-peak values ranging from 7.74 to 15.13 mg HC/g rock, indicating that the kerogen present has a large remaining potential capable to generate hydrocarbons at higher maturity stages [5, 6].

The LC-results presented in Figure 4.3 indicate that the majority of the oils investigated are rich in aromatic hydrocarbons, with their polar compounds (resins and asphaltenes) present in relatively high proportions, characteristic of the aromatic-intermediate class. This class of oils includes most crude oils from Jurassic and Cretaceous sources of the Middle East [1].

Typical gas chromatograms (GC-fingerprints) of carbonate and shale-derived oils are presented in Figures 4.4 and 4.5, respectively. Carbonate-derived oil shows a pristane/phytane ratio below (i.e. a predominance of phytane over pristane), indicative of a reducing environment, while that of oil from shale facies shows a pristane/phytane above 1 [7–9].

As mentioned above almost all Tertiary oils studied (Figure 4.6 as an example) are relatively heavy and severely biodegraded. This can be seen from the absence of all normal alkanes, while Cretaceous oils analyzed are relatively light and non-biodegraded (Figure 4.7 as an example), with all normal and branced (iso-) alkanes being present.

Saturated and aromatic fractions of the oils and source rock bitumens were further analyzed by GC-MS to investigate their aliphatic (saturated) and aromatic biomarkers. Table 4.2 shows biomarker parameters of carbonate facies oils compared to those of shale-derived hydrocarbons.

Table 4.1 Results of TOC and Rock-Evaol Pyrolysis for the rock samples analyzed.

Well name	Depth (ft)	% TOC⋆	RE-SI⋆	RE-S2⋆	RE-S3⋆	Tmax⋆	HI⋆	OI⋆	SI/TOC⋆100	PI
Well A	14144	11.31	3.76	15.13	1.09	454	134	10	33	0.20
Well A	14171	9.34	3.44	9.98	1.43	451	107	15	37	0.26
Well A	14193	6.25	2.92	7.9	1.37	454	126	22	47	0.27
WellB	13709	3.35	9.19	3.57	1.00	448	107	30	274	0.72
WellB	13718	9.82	15.67	12.9	1.00	454	131	10	160	0.55
WellB	13726	5.88	5.11	7.74	0.64	455	132	11	87	0.40

      ^⋆TOC = Total organic Carbon (wt%); SI = mg HCs/g rock; S2 = mg HCs/g rock; S3 = C0₂/g rockmg; Tmax = deg C; HI = Hydrogen index (mg HCs/g TOC); OI = oxygen index (mg/C0₂/g TOC).

Figure 4.1 Type of Kerogen present in source rocks.

      The following are the significant observations that could be obtained from Table 4.2 and GC-MS biomarker results:

       Carbonate oils show Pristane/phytane ratios below one, whereas pristane/phytane ratios of shale facies oils are around or above one.

       Carbonate oils are more enriched in αβ-hopanes than steranes, showing lower steranes/αβ-hopanes ratios, whereas in shale-derived oils steranes are more abundant than hopanes, showing high steranes/αβ- hopanes ratios [2].

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