Experimental analysis of the combustion characteristics of Estonian oil
shale in air and oxy-fuel atmospheres
Lauri Loo
a,
⁎, Birgit Maaten
a
, Andres Siirde
a
, Tõnu Pihu
a
, Alar Konist
a,b
a
Department of Thermal Engineering, Tallinn University of Technology, Ehitajate tee 5, Tallinn 19086, Estonia
b
School of Engineering, Brown University, 182 Hope St., Providence, RI 02912, USA
abstract article info
Article history:
Received 19 August 2014
Received in revised form 10 December 2014
Accepted 11 December 2014
Available online 27 February 2015
Keywords:
Oil shale
Oxy-fuel combustion
Carbonate mineral decomposition
DSC
TGA
O
2
/CO
2
combustion
A non-isothermal experimental study using thermogravimetric analysis and differential scanning calorimetry
coupled with a quadrupole mass spectrometer was conducted to investigate Estonian oil shale combustion
characteristics. The analyses were performed in air (N
2
/O
2
) and oxy-fuel (CO
2
/O
2
) atmospheres with various
oxygen ratios (10, 20 and 30 vol.%). Our experimental results in TGA show that combustion in the CO
2
/O
2
atmosphere is delayed compared to that in the N
2
/O
2
atmosphere. Carbonate minerals in oil shale decompose
in air in one step and in the oxy-fuel atmosphere in two separate steps: the decomposition of dolomite
(CaMg(CO
3
)
2
) and the subsequent decomposition of calcite (CaCO
3
). An increased oxygen ratio in combustion
in the oxy-fuel atmosphere increases the overall combustion rate, whereas the CO
2
emission volumes decrease
because of the lower decomposition extent of carbonates. The quadrupole mass spectrometer measurements
indicate several combustion products. A higher CO reading is registered in the CO
2
/O
2
atmosphere, but there is
no other significant difference. Based on the measurement results, a combustion model for Estonian oil shale is
proposed. Combustion in the oxy-fuel atmosphere is similar to combustion in air, which eases the design of
oxy-fuel combustors.
© 2015 Elsevier B.V. All rights reserved.
1. Introduction
The world's growing demand for energy enforces the usage of low-
grade fuels. In Estonia, oil shale (OS) power and oil production sectors
are the largest CO
2
emitters. Estonia depends on OS because over 90%
of its electricity is produced from OS [1,2]. Therefore, improving the
OS combustion process has large environmental and economic benefits.
OS is a low-grade fossil fuel that consists of kerogen (organic) and
mineral components. The organic matter contains a relatively large
amount of hydrogen, and the H/C atomic ratio is 1:4–1:5 [3]. Estonian
OS has a high content of mineral matter, which consists of carbona-
ceous, sandy-clay-carbonaceous and sandy-clay parts [4]. A higher CO
2
concentration can alter the decomposition of carbonates and decrease
CO
2
emission [5]. Therefore, implementation of oxy-fuel technology
offers many benefits.
The most energy- and cost-effective CCS technology is considered to
be the oxy-fuel technology [6]. Implementing the carbon capture and
storage (CCS) systems on oxy-fuel combustion technology significantly
reduces CO
2
emission. The concept of the oxy-fuel technology is the
removal of nitrogen from the combustion process, that is, combustion
occurs in an oxygen and carbon dioxide atmosphere. As a result, the
formed flue gas mainly consists of carbon dioxide and water vapor,
and the volume of flue gas considerably decreases [7,8].
Previous studies [5,9–14] concluded that a higher carbon
dioxide concentration in the combustion atmosphere decreases
the decomposition of carbonate minerals in the OS, but to our best
knowledge, there is no data about higher CO
2
atmosphere effects on
the combustion of OS kerogen. Thermogravimetric analysis (TGA) of
coal oxy-fuel combustion has proven that the oxy-fuel atmosphere
considerably changes the combustion process [15–18]. Nevertheless,
Niu and co-workers considered that the investigation of the reaction
mechanism and kinetic parameters of the oxy-fuel combustion of coal
are not sufficiently reviewed [15]. The same applies to OS oxy-fuel
combustion.
Simultaneous use of TGA, DSC and QMS allow one to obtain more
data with higher precision from different processes that occur in the
OS during the thermal treatment. TGA is a common technique to rapidly
investigate and compare thermal events and kinetics during the
combustion and pyrolysis of a material [19]. TGA measures the mass
loss of the sample as a function of time and temperature. A quadrupole
mass spectrometer (QMS) improves the analyses of the processes by
adding information about the evolving gases. The temperatures at
which the mass changes occur can be viewed using TGA, and quantita-
tive methods can be applied to the data to obtain the kinetic parameters.
DSC adds thermal information about the processes that occur during the
measurement, and QMS detects the evaporating ions.
Fuel Processing Technology 134 (2015) 317–324
⁎ Corresponding author.
http://dx.doi.org/10.1016/j.fuproc.2014.12.051
0378-3820/© 2015 Elsevier B.V. All rights reserved.
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