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Characterization of shale oil by spectroscopic and chromatographic
techniques
Yahya H. Khraisha a, 1
, Jamil J. Asfarb, Ahmad A. Radwan
a
a Department of Chemical Engineering Department, University of Jordan, Amman, 11946, Jordan
b Department of Mechanical Engineering Department, University of Jordan, Amman, 11946, Jordan
Abstract
Spectroscopic and chromatographic techniques were used to investigate the composition and
chemical structure of the extracted shale oils. The shale oils were extracted from two Jordanian oil
shale fields using autoclave devise and fluid solvents at sub- and supercritical conditions. The
analyses show that the variation of sub-and supercritical extraction conditions, particle size, solvent
type and shale field has a slight effect on the composition and chemical structure of the produce oil.
Ultraviolet visible (UV-vis) spectra show two clear signals in the ranges of 210-235 nm and 275-
280 nm. The first could be attributed to benzenic compounds and the other one to naphthenic
compounds. The 1HNMR results indicate that the protons of methyl and methylene represent a high
proportion of the hydrogen (75-85%) in most shale oil samples. GC analysis shows that the oil
samples contain n- alkane (n-C25) with a high predominant proportion. FT-IR results also support
these findings.
Keywords: Shale oil; UV-vis spectroscopy; FT-IR; 1HNMR; GC
1. Introduction
Shale oil is defined as an oil that be derived from the organic matter (kerogen) of the oil shale
sedimentary rocks using different techniques from direct and indirect heating to recently solvent
critical extraction [1-4]. This oil is considered an important prospective energy sources in the
world since it represents about one third greater than the proven resources of conventional crude
oil [5].
Jordan is highly influenced by the world energy situation since it is a non-oil producing country.
It has a future plan or prospect that oil shale utilization will be one of Jordan's future energy
sources. Oil shale resources in Jordan are estimated to be more than 50 billion tons, in which the
oil content is about 4 billion tons [6]. Its large deposits are widely distributed all over the
country, particularly in the central region [7].
1 Correspondence to Y. H. Khraisha, Chemical Engineering Dept., University of Jordan, Amman,
Jordan. Email: [email protected]
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International Journal of Scientific Research and Innovative Technology Vol. 7 No. 2; March 2020
Shale oil is similar to petroleum hydrocarbons with extremely complex molecular structure
containing oxygen, nitrogen, sulfur and metal elements. It is often produced by the thermal
destructive distillations at temperatures 500-600 °C . The chemical and physical properties of
the extracted shale oil were found to change for the investigated oil shales depending on the
origin or nature of kerogen, the type of the extracting technique as well as the operating
conditions. The extracted oil could be highly aromatic, aliphatic, naphthenic or somewhere in
between. In general, shale oil has a low API gravity (18 – 22), low hydrogen to carbon ratio and
high concentration of nitrogen, arsenic, sulfur, and metals. Therefore, it cannot be processed
directly without upgrading [8].
Investigators have used chromatographic methods (capillary GC, HPLC, GC-MS), infrared
spectroscopy (FT-IR) and nuclear magnetic resonance (1H NMR,
13C NMR) to obtain qualitative
and quantitative information on the compositional and structural analysis of heavy
hydrocarbons, bitumen, and petroleum fractions. For example, Khraisha et al. [9] have analyzed
Jordanian shale oil samples derived from an oil shale flash pyrolysis unit using spectroscopic
and GC instruments. The 1H NMR results have shown that the protons of methyl and methylene
represent the bulk of the hydrogen in the most shale oil samples. In addition, the GC analysis
indicates that the oils contain n-alkanes with a predominant proportion of n-C25. Chham et al.
have analyzed Moroccan oil shale samples using FTIR spectroscopy [10]. The results of FT-IR
spectra have indicated that the shale oil contains a substantial proportion of aromatic
hydrocarbon compounds and fewer amounts of paraffins. However, the nature and the type of
kerogen affects significantly the quality and composition of the produced shale oil. Hufnagel et
al. [11] have investigated a Jordanian oil shale deposits and shown that the organic material of
the oil shale consists largely of prebitumen bituminous ground-mass. This was formed during
the early diagenetic process by mainly microbial influence, from initial plant and animal
materials with a lipidic composition. The level of temperature as well as the extraction
technique influence the composition of the produced shale oil. For instant, at high temperature ~
500°C, aliphatic C-C and ether C-O bonds are broken and rearranged to yield aromatic
hydrocarbons [12]. Feng et al. have studied the chemical composition of bitumens in pyrolyzed
Green River oil shale by 13
C NMR spectroscopy [13]. The results have revealed that the bitumen
which formed during the intermediate stage of kerogen decomposition becomes more aromatic
(less aliphatic) with increasing maturity.
In short, shale oil is a complex mixture of hydrocarbon compounds in which the analysis using
different instrumental techniques provides important information that impacts on the handling,
transportation, upgrading and refining. In this study, spectroscopic (FT-IR, UV-Vis, 1HNMR)
and chromatographic (temperature programmed-GC) analyses have been done on oil samples
derived from Jordanian oil shale under sub and supercritical critical conditions of fluid
solvents.
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2. Experimental
2.1 Oil samples
The oil samples were derived from two Jordanian deposits; El-Lajjun and Sultani. The fluid
supercritical extraction was conducted in an autoclave devise under a high pressure of inert
atmosphere. The apparatus and procedure of oil extraction have been given in detail
elsewhere [14]. Table 1 shows the conditions, variables and the analytical techniques for the
different shale oil samples.
Table 1. Conditions and analytical methods for different shale oil samples derived from
extraction unit. Sample T, °C P, bar T, min dp. µm Solvent GC UV 1HNMR IR Field
ST1 100 42 60 850-1400 Toluene X El-Lajjun
ST2 150 42 60 850-1400 Toluene X X X X El-Lajjun
ST3 200 42 60 850-1400 Toluene X X X X El-Lajjun
ST4 318 42 60 850-1400 Toluene X X X X El-Lajjun
SD1 318 42 60 850-1400 Toluene X X Sultani
SD2 318 42 60 500-850 Toluene X X El-Lajjun
SD3 318 42 60 255-355 Toluene X X X X El-Lajjun
SD4 318 42 60 355-500 Toluene X X El-Lajjun
SD5 318 42 60 175-255 Toluene X X El-Lajjun
St1 318 42 20 850-1400 Toluene X X Sultani
St2 318 42 40 850-1400 Toluene X X X X Sultani
St3 318 42 80 850-1400 Toluene X X Sultani
SP1 318 10 60 850-1400 Toluene X X El-Lajjun
SP2 318 20 60 850-1400 Toluene X X El-Lajjun
SP3 318 30 60 850-1400 Toluene X X X X El-Lajjun
SSo1 273 60 60 850-1400 Trichloroethylene X X Sultani
SSo2 240 80 60 850-1400 Methanol X X Sultani
SSo3 240 50 60 850-1400 Benzene X X Sultani
2.2 Analytical methods
2.2.1 Fourier Transform Infrared Spectroscopy (FTIR) Analysis
The infrared analysis was performed using an FTIR Nicolet, Impact 400 infrared
spectrometer for detecting functional groups and characterizing covalent bonding
information in shale oil samples.
2.2.2 Ultraviolet spectroscopy (UV-Vis)
A Milton Roy, Spectronic instrument 1201 UV was used to measure the electronic
spectra of shale oil samples. The samples were dissolved in n-hexane.
2.2.3 Proton nuclear magnetic resonance spectroscopy (1H NMR)
A Bruker Avance DPX300 MHz Solution State 1H NMR spectroscopy was used to
analyze the oil samples. The samples were dissolved in dichloromethane.
2.2.4 Gas chromatography (GC)
Shale oil samples were analyzed using a Vraian gas chromatograph, Model 3300. The
sample concentration was 0.5g in 5ml hexane. In order to specify the peak's identity,
pure n-paraffins (C12, C14, C16, C18 and C20) were firstly injected, and hence, the
retention time for each paraffin peak was determined. However, to specify the other n-
alkanes carbon atom, gas oil was injected and its peaks were compared with pure n-
paraffins, and the others extrapolated. To certain this calibration procedure, the gas oil
spectrum was compared with other published gas oil spectra, analyzed at the same
operating and packing conditions [15].
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3. Results and Discussion
3.1. Fourier Transform Infrared Spec
The FTIR is a useful tool to underst
and the functional groups present in i
shale oil samples, ST2, ST4, SD3, SP
general, the figure indicates a comple
the tested samples have shown a si
spectra were based on the informatio
intensity band at 3050 cm-1
represent
at 2924 cm-1
and 2853 cm-1
are du
stretching, respectively. The bands fa
C=O group. The samples also show
(1375 cm-1
) and aromatic oxygenate
wavelength bands at 873, 774, 772 cm
3.2.UV-visible spectroscopy analysis
Figure 2 shows a typical examp
ST2, SD3, SP3, St2 and SSo2 at
plots represent the wavelength ve
In general, most of the samples s
to 1.4. The shale oil sample w
absorbance value compared to the
the absorbance value, the lower
Therefore, it can be concluded
(toluene); ST2, ST4, SD3, SP3
sample extracted by polar solvent
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Spectroscopy (FTIR) Analysis
nderstand the chemical composition of a liquid heavy
nt in it. Figure 1 shows a typical example of the FTIR
D3, SP3, St2 and SSo3 at different extracting conditio
omplex composition of the oil with a high number of
n a similar spectrum with slight differences. Interpr
rmation acquired from the literature [16,17]. For ex
resents aromatic C-H stretching. The strong absorptio
due to methyl C-H stretching compounds and m
ands falling between 1708 and 1724 cm -1
are attribu
show C-H bending (1454-1459 cm-1
), C-H bending in
genated compounds such as aromatic ether at 1073
772 cm-1
are considered aromatic C-H bending out-of
alysis (UV-vis spectra)
xample of ultraviolet – visible spectra for shale oil
So2 at different extracting conditions as mentioned
gth versus the absorbance over a range of 200 – 600 n
ples show similar spectra with maximum absorbanc
ple which was extracted by methanol (SSo2) sho
to the others extracted by toluene. It has been shown
lower the aromatic content in the heavy oil hydr
luded that the shale oil samples extracted by no
, SP3 and st2 have a higher content of aromatics t
olvent (methanol).
7 No. 2; March 2020
heavy hydrocarbons
e FTIR spectra of the
nditions (table 1). In
ber of peaks. Most of
nterpretations of the
or example, the low
orption bands falling
and methylene C-H
ttributed to carbonyl
ing in methyl groups
1073 cm-1
. The long
of-plan.
le oil samples; ST4,
ioned in table 1. The
00 nm wavelength.
orbance (λmax) of 0.5
) shows the lowest
shown that the lower
l hydrocarbons [18].
nonpolar solvent
atics than that SSo2
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Figure 1(A). FT
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FT-IR spectra of shale oil samples; ST4, ST2, SP3
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, SP3
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Most of the tested samples show
The first signal range could be
naphthenic compounds [9, 19, 20
Figure 1 (B) FT
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show clear signals in the ranges of 210-235 nm an
uld be attributed to benzenic compounds and the
19, 20].
) FT-IR spectra of shale oil samples; SD3, St2, SSo3
7 No. 2; March 2020
nm and 275-280 nm.
the second one to
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Figure 2. UV-Vis spectra of shale oil
3.3. Proton Nuclear Magnetic Resona
Figure 3 illustrates the 1H NMR
samples. Figure 4, for example,
shale oil sample. The absorption
saturated carbons in terms of
aromatic protons can be observe
indicates the detailed assignmen
distribution of the shale oil samp
hydrogen, Har, represents 15-25 %
high proportion of Har (90 %).
SP3) which were extracted by to
about of 40 %, 10-14% of the t
protons represent about 75% of t
by toluene.
88
ale oil samples; ST4, ST2, SD3, SP3, St2, SSo2.
esonance Spectroscopy (1H NMR Spectra)
NMR Spectra for ST4, ST2, ST3, St2, SD3, SP3 and
mple, shows the detailed shape of the 1H NMR spe
rptions in region 0.5 to 2 ppm indicate the presence
s of methyl and methylene groups. Moreover, th
bserved in regions 4 to 5 and 7 to 8 ppm, respect
gnments of the bands of the 1H NMR spectra and
l samples [9]. From the results (table 2), it is clear th
25 % of the total protons except the sample SSo3
%). By contrast, the oil shale samples (ST4, ST2, S
by toluene indicate a hydrogen of types Hβ and Hγ
the total hydrogen, respectively. In short, methyl
% of the hydrogen for most shale oil samples particu
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3 and SSo3 shale oil
R spectrum of SD3
esence of protons on
er, the olefinic and
espectively. Table 2
ra and the hydrogen
lear that the aromatic
SSo3 which shows a
ST2, ST3, St2, SD3,
γ (see table 2) of
ethyl and methylene
particularly extracted
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Figure 3. 1HNMR spectra of ST4, ST2, ST3, St2, SD3, SP3 and SSo3 shale oil.
Table 2: Assignments of the bands in the 1HNMR spectra (Khraisha et al.,2003) of
the shale oil sample
Hydrogen Type Symbol 104 x chemical
shift
Hydrogen distribution, %
ST2 ST3 ST4 SP3 SD3 St2 SSo3
Aromatic Har 6.0 – 9.0 24.01 22.59 25.19 13.29 24.34 21.46 92.28
Ring-joining
methylene Hα, 2 3.5 – 5.0 1.75 1.71 1.94 3.73 4.47 4.19 0.00
CH3, CH2 and CH-α
to an aromatic ring Hα 2.0 – 3.4 24.32 24.72 25.19 20.24 20.37 27.23 1.17
β-CH3, CH2 and CH-β
or further from an
aromatic + paraffinic CH2 and CH
Hβ 1.0 – 2.0 37.52 39.91 36.50 48.94 38.96 34.95 5.35
CH3-γ or further from
an aromatic ring +
paraffinic CH2
Hγ 0.5 – 1.0 12.40 11.08 11.18 13.80 11.86 12.17 1.20
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Figure 4. 1H N
90
H NMR spectra of SD3 shale oil.
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3.4. Gas Chromatography (GC)
Figure 5 (A, B, C) shows GC peak
oil samples, ST1, ST3, SD1, St1, SP
samples.
Figure 5 (A): Packed column gas chro
paraffins, gas oil and shale oil (ST1).
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Gas oil
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C peaks of normal alkanes (C12, C14, C16, C18 and C
t1, SP1, SSo1, and SSo2, compared with gas oil and
as chromatography n- alkanes identified by carbon number
ST1).
Pure Paraffins
7 No. 2; March 2020
nd C20) for the shale
il and pure paraffins
umber for pure
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Figure 5 (B). Packed column gas ch
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gas chromatography for ST3, St1 and SD1 shale oil sample
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samples.
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Figure 5 (C). Packed column gas c
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n gas chromatography for SP1, SSo1 and SSo2 shale o
SSo1
7 No. 2; March 2020
shale oil.
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The distributions of n-alkanes relative to n-C5 (area to area peak’s ratio) for the different analyzed
shale oil samples are given in table 3. Clearly seen, the normal alkanes obtained are n-C15 to n-C32.
Moreover, the n-C25 represents the greatest quantity of the n-alkanes in most shale oil samples. In
general, most of the tested samples indicate close trends except samples SSo1 and SSo2 who show
only one peak (n-C25). On the other hand, the variation of operating conditions as well as the
shale’s field (see table 1) have no significant effect on the chemical structure of the shale oil
produced.
Table 3. Normal alkanes obtained from shale oils analysis by GC
a relative to the area of n-C25
Peak
No.
n-
alkanes
Relative quantitya
ST1 ST2 ST3 ST4 SD1 SD2 SD3 SD4 St1 St2 St3 SP1 SP2 SP3 SSo1 SSo2
C12 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
C13 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
C14 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
1 C15 0 0 0 0 0.060 0 0 0 0 0.064 0 0 0 0.071 0 0
C16 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
C17 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
2 C18 0 0 0 0 0 0 0 0 0.043 0.040 0 0 0 0.019 0 0
3 C19 0 0 0 0 0.094 0 0 0 0 0.016 0 0 0 0 0 0
4 C20 0 0 0.104 0.074 0.113 0 0 0 0 0.017 0 0.160 0.130 .016 0 0
5 C21 0.106 0 0 0 0 0 0 0 0.032 0 0 0 0 0 0 0
C23 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
6 C24 0 0 0 0 0 0 0 0 0.049 0.027 0 0 0 0 0 0
7 C25 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000 1.000
8 C26 0 0 0 0 0.039 0 0 0 0 0 0 0.75 0 0.054 0 0
9 C27 0 0 0 0.032 0.041 0 0 0 0 0.034 0 0 0 0.072 0 0
10 C28 0.059 0.064 0.114 0.103 0.038 0 0 0 0.172 0.025 0 0.276 0 0.161 0 0
11 C29 0.035 0.018 0.047 0.055 0.039 0.068 0.052 0.141 0.030 0.037 0.019 0.032 0.116 0.066 0 0
12 C30 0.100 0.043 0.089 0.099 0.095 0.091 0.059 0.099 0.071 0.101 0 0.077 0.05 0.106 0 0
13 C32 0.041 0.038 0.036 0.032 0.042 0.039 0.20 0.038 0.064 0.029 0.035 0.078 0.048 0.033 0 0
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4. Conclusions
Shale oil obtained at supercritical conditions has been analyzed using different spectroscopic
techniques (UV-Vis, FT-IR, 1HNMR) and Gas Chromatography in order to elucidate its
composition and chemical structure. From the results and analyses, the following conclusions
can be drawn.
1. The spectroscopic and chromatographic investigations inform that the variations in
supercritical conditions has no significant effect on the composition of the produced
shale oil.
2. UV-Vis shows two clear signals in the ranges of 210-235 nm and 275-280 nm. The first
could be attributed to benzenic compounds and the other one to naphthenic compounds.
3. Most of the shale oil samples (extracted by toluene) consist of a high proportion of
aliphatic hydrocarbons with a small amount of aromatic and olefinic compounds. 1HNMR supports this finding since the oil contains about 75% of methyl and methylene
protons. Moreover, FT-IR spectra enhance this finding.
4. GC analysis reveals that the oil samples contain n- alkanes with a predominant
proportion of n-C25.
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