J. of Supercritical Fluids 47 (2008) 195–199
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The Journal of Supercritical Fluids
journal homepage: www.elsevier.com/locate/supflu
New pitches with very significant maturation degree obtained by supercritical
extraction of Moroccan oil shales
A. Abourriche
a,∗
, A. Adil
b
, M. Oumam
b
, H. Hannache
b
,
R. Pailler
c
, R. Naslain
c
, M. Birot
d
, J.-P. Pillot
d
a
École Nationale des Sciences Appliquées, B.P. 63, 46000 Safi, Morocco
b
Laboratoire des Matériaux Thermostructuraux, Faculté des Sciences Ben M’sik, B.P. 7955 Casablanca, Morocco
c
Université Bordeaux 1/CNRS/CEA/SAFRAN, Laboratoire des Composites Thermostructuraux (LCTS), 3 allée de la Boétie, F-33600 Pessac, France
d
Université de Bordeaux, Institut des Sciences Moléculaires, CNRS-UMR 5255, 351 cours de la Libération, F-33405 Talence, France
article info
Article history:
Received 16 February 2008
Received in revised form 1 July 2008
Accepted 18 July 2008
Keywords:
Oil shale
Pitch
Supercritical extraction
Maturation
abstract
In the present work, new pitches were obtained by supercritical extraction of Moroccan oil shales with
water–shale oil as solvent. The aim of the research was to obtain pitches with very significant maturation
degree of the organic matter. The evolution of the pitch structure was studied through indexes calculated
from quantitative infrared spectroscopy. The classification of the pitches enabled us to assess their degree
of maturation. This allowed us to establish the water–shale oil mixture composition likely to give the best
maturation of the oil shale
′
s organic matter.
© 2008 Elsevier B.V. All rights reserved.
1. Introduction
Currently, the conventional energy resources (natural gas, oil,
... ) of the world are being largely used, so they will not last indef-
initely. Therefore, it is necessary to seek for alternatives. A lot of
efforts and studies have been carried out in the direction of the
oil shales [1–4] whose world reserves are 500 times more signif-
icant than those of oil are [5], although the presence of mineral
matter makes difficult their use as a source of energy. However,
their organic matter, rich in aromatic compounds, could have other
applications [6,7]. The present work is part of a more general pro-
gram for the exploitation of the Moroccan oil shale deposit of
Tarfaya. More specifically, the aim was to try to show that the
organic fraction of the oil shales could be used, after appropri-
ate chemical treatments resulting in a “maturation” of this organic
phase, as precursors of low cost carbon fibres (e.g. activated car-
bon fibres) [8]. During this study, we tried to define, from infrared
spectroscopy data, the optimal operating conditions likely to give
the higher maturation degree of the organic matter of the oil
shale.
∗
Corresponding author. Tel.: +212 64456721; fax: +212 24668012.
E-mail address: krimabou@hotmail.com (A. Abourriche).
2. Materials and methods
2.1. Materials
The oil shale used in this work was from the Tarfaya deposit
located in the South of Morocco. This deposit consists of several
layers that are in turn subdivided in sub-layers, each having a dif-
ferent amount of organic matter. The samples were obtained from
the R
3
sub-layer, characterized by its high content of organic mat-
ter [9]. The chemical composition of the R
3
sub-layer is given in
Table 1.
The carbonate-free oil shale (RH) was obtained by dissolution
of carbonates with HCl [10,11]. The powdered R
3
shale (20 g, grain
size 0.063–0.08 mm) and 80 mL of concentrated HCl (7 M) were
introduced in an Erlenmeyer. The mixture was then subjected to
magnetic stirring for 4 h. The formed CO
2
was trapped by bubbling
in a solution of barium hydroxide. After filtration, the solid residue
(referred to as RH) was washed carefully with distilled water, dried
at 100
◦
C and stocked in a sealed plastic bag.
2.2. Apparatus
2.2.1. Preparation of the pitch
Supercritical extraction of the sample RH (10g) with a mixture
of water [12–14] and shale oil [15] as solvent was conducted in a
120 mL stainless steel autoclave equipped with a stirrer and heated
0896-8446/$ – see front matter © 2008 Elsevier B.V. All rights reserved.
doi:10.1016/j.supflu.2008.07.016