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Kinetics of copper slag oxidation under nonisothermal conditions
Stoyko Gyurov • Diana Rabadjieva •
Daniela Kovacheva • Yoanna Kostova
Received: 12 April 2013 / Accepted: 27 November 2013
� Akademiai Kiado, Budapest, Hungary 2014
Abstract The kinetics of air copper slag oxidation under
nonisothermal conditions is studied using simultaneous TG–
DTA at a varying heating rate of slag and flow rate of the
oxidizing gas flux. The values of the kinetic parameters,
activation energy and pre-exponential factor, have been
determined based on: data from DTA by the methods of
Kissinger and Ozawa; data from TG using an isoconversion
method and the computation procedures of Ozawa–Flynn–
Wall and Kissinger–Akahira–Sunose. No relationship
between the kinetic parameters and the oxidation gas flow rate
has been established. The changes of the phase composition
with temperature are investigated by X-ray powder diffraction
analysis on the basis of data obtained for the products formed
at the different stages of the oxidation process. The mor-
phology of the oxidized slag as well as the elements distri-
bution is studied by electron microscopy and EDS analysis.
Keywords Copper slag � Oxidation � Nonisothermal
kinetics � Simultaneous TG/DTA � Arrhenius parameters
Introduction
The slag being a waste product from the pyrometallurgical
production of copper contains mixed or individual oxides
of iron, silicon, aluminum, calcium, copper, nickel, cobalt,
etc. It has been calculated that about 2.2 tons of slag are
generated per each ton of produced copper and approxi-
mately 24.6 million tons of slag are accumulated every
year [1–3]. Dumping or disposal of this slag causes wast-
age of certain amount of metal available in the raw material
and causes environmental problems [4]. Many efforts have
been focused on developing methods for the recycling of
slag and the reduction of its quantity [5–7]. Various
methods have been proposed for extracting copper and
other precious metals from slag by treating it with solutions
of acids, bases, and salts under atmospheric pressure and
high pressure as well [8–23]. Application of these methods
does not result in a significant reduction of the disposed
slag because the quantity of the extracted copper and pre-
cious metals is negligible in comparison to the amount of
slag [1–3, 5]. A new approach has been proposed in the EU
patent No. 2 331 717 B1 [24], which is based on the
decomposition of the fayalite (2FeO�SiO2) present in the
slag into iron oxide and silicate phases by oxidation and
subsequent hydrometallurgical treatment. As a result, use-
ful products could be obtained in the form of amorphous
silicon dioxide and iron oxide and the slag can be com-
pletely utilized. Therefore, it is important to know thor-
oughly the process of oxidation at the temperatures of
fayalite decomposition.
There are a restricted number of articles addressing
the oxidation of fayalite as a chemical compound. Oxidation
of fayalite (2FeO�SiO2) single crystals involved mainly
its transformation to hematite (Fe2O3), magnetite (Fe3O4),
and amorphous silica [25–27]. The reaction equation is as
follows:
2FeO�SiO2 þ 1=2 O2 ! Fe2O3 þ SiO2 ð1Þ2FeO�SiO2 þ 1=3 O2 ! Fe3O4 þ SiO2 ð2Þ
S. Gyurov (&) � Y. Kostova
Institute of Metal Science, Equipment and Technologies ‘‘Acad.
A. Balevsci’’ with Haydroaerodinamics centre Bulgarian
Academy of Sciences, 67 ‘‘Shipchenski prohod’’ str., 1574 Sofia,
Bulgaria
e-mail: [email protected]
D. Rabadjieva � D. Kovacheva
Institute of General and Inorganic Chemistry, Bulgarian
Academy of Sciences, ‘‘Acad. Georgi Bonchev’’ str. bld.11,
1113 Sofia, Bulgaria
123
J Therm Anal Calorim
DOI 10.1007/s10973-013-3569-2
Sanders and Gallagher [28] reported that the magnetite
is oxidized in a two-stage process; the first stage is the
formation of the metastable spinel c-Fe2O3 (maghemite),
and second stage is the formation of the equilibrium phase
a-Fe2O3 according to the reactions:
4Fe3O4 þ O2 ! 6c-Fe2O3 ð3Þc-Fe2O3 ! a-Fe2O3: ð4Þ
During high temperature annealing in air atmosphere
coarse magnetite powder undergoes oxidation only above
773 K [29]. Magnetite prepared at relatively low
temperatures from freshly precipitated precursors, however,
has a much greater surface area and defects concentration and
therefore oxidizes at much lower temperatures [30]. The
process starts at temperature of about 473 K and ends in the
interval 648–673 K. The beginning of the conversion is at
temperature of about 648 K and the end is at 798–933 K.
Thermal behavior of copper slag obtained from rever-
beratory furnace was investigated using simultaneous
thermal analysis (STA), dilatometry, and X-ray diffraction
(XRD) techniques [31]. The authors reported two exo-
thermic peaks in DTA curve, which could be related to the
magnetite–maghemite and maghemite–hematite transfor-
mations, respectively. The isothermal decomposition of
copper slag in synthetic air was investigated by Gyurov
et al. [32]. However, the process has not been sufficiently
studied. In order to develop an appropriate technology for
industrial utilization of copper slag, additional investiga-
tions are needed, especially with respect to the heating rate
and the parameters of the oxidizing gas flux.
The aim of the present work is to study the processes of
nonisothermal oxidation of copper slag by using the simul-
taneous TG–DTA, XRD, and SEM. The obtained data from
TG–DTA were used to calculate the kinetic parameters
(activation energy and pre-exponential factor), while the
data obtained from the XRD and SEM were used to deter-
mine the phase composition and morphological character-
istics of the formed solid phases at the stages of oxidation.
Experimental
The copper slag used in the experiments is a waste product
from the pyrometallurgical production of copper in Aurubis
Bulgaria AD. The slag was sifted through a 100 mesh sieve
and the fraction with particle sizes under 100 meshes was
used in the experiment.
XRD analysis
The XRD analysis was carried out using an automatic
Bruker D8 Advance powder X-ray diffractometer with
CuKa radiation (Ni filter) and registration of LynxEye
solid-state position-sensitive detector. The X-ray spectra
were recorded in the range from 5.3� to 80� 2h with a step
of 0.02� 2h. The qualitative phase analysis was made using
the PDF-2(2009) database of the International Center for
Diffraction Data (ICDD) by means of the DiffracPlusEVA
software package. Refinement of the unit cell parameters
was made with Topas4.2.
SEM analysis
The slag compositions as well as the distribution of the
chemical elements were determined using a JEOL JSM 35
CF scanning electron microscope with a TRACOR
NORTHERN TN-2000 X-ray microanalyzer applying
JEOL standards.
Simultaneous TG–DTA
The nonisothermal oxidation of copper slag was carried out
using the computerized combined thermal analysis appa-
ratus LABSYSEvo, SETARAM Company, France, at
atmospheric pressure in a flow of synthetic air (MESSER
CHIMCO GAS-OOH 1056, ADR 2, 1A) in the temperature
range 298–1,273 K. Synthetic air was used as an oxidant in
order to maintain a constant oxygen partial pressure in all
experiments. Corundum crucibles with a volume of 100 ll
were used. The sample mass in all tests was 80 ± 1 mg.
The experiments were carried out under dynamic condi-
tions, with heating rates of 4, 8, 12, 16, and 20 K min-1
and oxidizing gas flow rates of 20, 35, and 50 mL min-1.
Additional experiments for identification of the interme-
diate solid phases were carried out under the following
conditions: heating up to 523, 573, 623, 673, 723, 773, 873,
973, 1,073, 1,173, and 1,273 K with heating rate of
12 K min-1 and maintaining the desired temperature for
2 h. The flow rate of the oxidizing gas was 20 mL min-1.
These oxidized samples were used in XRD analysis.
Experimental results
XRD analysis
XRD powder diffraction patterns are shown in Fig. 1. The
initial slag is composed of fayalite Fe2SiO4; a cubic phase
with a spinel type structure and an unit cell parameter of
8.37 A; quartz–SiO2; calcite (Ca, Mg)CO3; and calcium
mono-carboaluminate Ca4Al2O6CO3�11H2O. The phases
presented are typical for copper slag but the amount of
different components may vary depending on the manu-
facturers. In any case, fayalite is dominant phase in this
type of slags [6, 33]. The value of unit cell parameter at
S. Gyurov et al.
123
room temperature of the spinel iron oxide (8.37 A) is lower
than the reported values for pure magnetite: 8.3958 A [34],
8.3965 A [35], and 8.3970 A [36] showing that magnetite
phase is slightly oxidized. The change of the unit cell
parameter of the spinel iron oxide with the temperature is
presented in Fig. 2.
SEM analysis
Chemical composition of the slag is (in mass%): FeO
50.93, MgO 1.43, CaO 1.39, MnO \0.01, SiO2 31.26,
Al2O3 6.93, Na2O 3.02, K2O 1.74, TiO2 0.22, and CuO 0.6,
respectively. The SEM image of the cross-section of slag
oxidized to 1,173 K and the distribution of Fe, Si, and O2 is
shown in Fig. 3. Three types of microstructure are
observed in the SEM image of the cross-section of slag
oxidized to 1,173 K: particles with dendrites, particles with
lamellar structure, and particles with eutectic-like structure,
which is probably a grain section, perpendicular to the
lamellae, Fig. 3. The particles contain three phases: iron
oxide, silicon oxide and iron silicate (residual fayalite).
TG–DTA
The obtained TG–DTA curves are similar in shape to the
one shown in Fig. 4. It shows an endothermic effect within
the temperature range 298 to about 400 K and a broad
exothermal effect in the temperature interval 400–1,273 K,
where four peaks could be distinguished. The general view
of the exothermic effect revealed the simultaneous run of
several (oxidation or phase transition) processes. The endo-
effect is characterized by a minimum decrease of mass and
is due to the released residual moisture in the slag. The
exo-effect is characterized by gradual increase of mass and
is due to the oxidation processes in the slag. The peak
temperatures Tp from the DTA curves are summarized in
Table 1. They follow, with some exceptions, the general
trend of shifting toward higher temperature values with the
increase of the heating rates. It can be observed that the
sample mass increases continuously between 693 and
1,273 K and is associated with the oxidation processes of
the slag.
Discussion
The XRD data presented in Fig. 1 show that in the temper-
ature range 293–673 K no changes of the slag’s phase
composition are observed. From 673 to 773 K, changes of
the unit cell parameter of magnetite are observed due to its
partial oxidation to maghemite, Fig. 2. The first diffraction
peaks of hematite phase are observed at temperatures
between 673 and 723 K. It is difficult to identify the process
leading to hematite formation: transformation of maghemite
or decomposition of fayalite. Actually, the oxidation and
transformation of the slag magnetite into hematite take place
in parallel with the oxidation and decomposition of the slag
fayalite into magnetite, hematite, and amorphous silicate
phase. At temperatures in the interval 673–1,273 K, the
processes of oxidation and decomposition of the fayalite and
transformation of magnetite phase become more intensive.
In the temperature range 1,073–1,273 K, a gradual increase
of the unit cell parameter of the spinel phase is observed as a
result of reduction of part of the iron ions. The size of the
crystallites of magnetite in the slag, oxidized at temperatures
below 873 K is greater than that of the samples oxidized at
temperatures in the interval 973–1,273 K. The smaller
grains (the broader peaks) of magnetite phase observed at
higher temperatures indicate that magnetite phase here is an
intermediate product from decomposition of fayalite.
1273K
1173K
1073K
873K
973K
773K
723K
623K
673K
573K
HS
S
SS H
HHHH
H
H
FF SSS
S
FFF
F
FFFF
F
F
F
Inte
nsity
/a.u
.
FS
H
298K
523K
H-hematite
F-fayalite
S-spinel
20 25 30 35 40 45 50 55 60 65
2θ /°
Fig. 1 X-ray powder diffraction patterns of the copper slag at
different stages of the oxidation process
8.34
8.35
8.36
8.37
8.38
8.39
8.40
Uni
t cel
l par
amet
er/A
Temperature/K300 400 500 600 700 800 900 1000 1100 1200 1300
Fig. 2 Variation of the unit cell parameter of the spinel iron oxide
with the temperature
Kinetics of copper slag oxidation
123
Oxidized to a temperature of 1,273 K slag contains hema-
tite, amorphous silicate phase, and residual magnetite.
According to our SEM observations, the decomposition
of the fayalite phase of the slag to hematite and silicate
phase is accompanied by mass redistribution. There are
different opinions concerning the problem which of the
components will be diffused—Fe, Si, or O2. If oxidation
occurs by transport of oxygen via fayalite, oxides of iron
and silicon will be observed at the boundary gas/solid
phase surface. If oxidation takes place by diffusion of iron
or silicon from the interior to the surface, the latter will
be covered by a layer of the respective oxide. According
to Mackwell [27], iron is diffused from the interior of the
fayalite single crystal to the surface and the kinetics obeys
a parabolic law. According to Gaballah et al. [26], the
kinetics is pseudo-parabolic with formation of a silicon
oxide and an iron oxide layer. Oxygen is diffused through
the latter and hematite crystals grow on it. All particles
shown in Fig. 3 have on their surface a layer of iron
oxide where under layers of fayalite and silicate phases
follow. This presumes diffusion of iron from the particle
core to the surface and of oxygen via the boundary sur-
face toward the interior of the particle. According to
Fisler and Mackwell [37], the experiments with a plati-
num tracer show that fayalite grows at the quartz–fayalite
boundary and the process is controlled by iron and oxy-
gen diffusion.
446
357
268
179
90
1
416
L1: O Ka Sika FeKa
L2: O Ka Sika FeKa
L3: O Ka Sika FeKa 200 μm/DIV
200 μm/DIV
200 μm/DIV
333
250
167
84
1
344
258
172
86
0
Fig. 3 SEM image of the
cross-section of slag oxidized to
1,173 K and the distribution of
Fe, Si, and O2
99
100
101
102
103
104
105
Mas
s/%
DT
A/a
.u.
Temperature /K
1149
856
691582
Exo
400 600 800 1000 1200
Fig. 4 DTA–TG curves of copper slag oxidation at heating rate
8 K min-1 and 35 mL min-1 oxidizing gas flow rate: dashed line TG
curve, line DTA curve
S. Gyurov et al.
123
Kinetic analysis
The collected TG–DTA data were used to determine the
kinetic parameters (the activation energy and the pre-
exponential factor) of the oxidation processes as described
elsewhere [38–51]. The kinetic analysis is based on the
assumption that the rate constant (k) is described by the
Arrhenius equation:
k ¼ A exp �E=RTð Þ; ð5Þ
where A is the pre-exponential factor, E is the activation
energy, R is the universal gas constant, and T is the abso-
lute temperature.
The DTA data (Tp—peak temperature) were processed
and the kinetic parameters of the oxidation processes were
obtained using the methods of Kissinger and Ozawa
[48, 49]. All obtained data for activation energy (E), the
pre-exponential factor (lnA), and regression coefficient (r2)
are presented in Table 2. Figure 5 presents samples of
Kissinger and Ozawa plots, respectively, for the tempera-
tures of third peaks of the DTA curves. The activation
energy E is calculated from the slope of the obtained
straight line and the pre-exponential factor lnA from the
intercept. It is seen that there is no correlation between the
amount of oxidizing gas and the values of kinetic param-
eters. The activation energy is a constant value for a given
process and can be influenced by the gas flux only if the
reaction produces or consumes a gas component [44].
During our DTA experiments the partial pressure of oxy-
gen at the reaction surface remains constant and the amount
of gas does not affect the reaction rate.
The values of activation energy calculated by the first
and second peaks are substantially equal. They are close to
the average values reported by Sanders and Gallagher
(about 120 kJ mol-1) by the oxidation of magnetite [28].
In the temperature range 293–673 K, XRD data (Figs. 1, 2)
indicate only the oxidation of magnetite to the maghemite
as to 673 K does not exhibit peaks of hematite, further-
more, mass effect is very small as could be seen in Fig. 4.
This is due to the morphology of the slag. The magnetite
grains in copper slag occur as small inclusions in fayalite or
glass phases [32]. Oxidation of individual small magnetite
grains will produce a negligible amount of hematite.
The third peak of the DTA curves is associated with the
fayalite oxidation and decomposition to iron oxides and
amorphous silicate mass. The values of activation energy
calculated by the third maximum are in the range
164–195 kJ mol-1, which are substantially different from
those reported by Gaballah et al. [26] for the oxidation of
single crystal synthetic fayalite. The nature of the forth
peaks was not revealed in the present study. It may be due
to some structural transitions of the silicate mass as sup-
posed by Gaballah et al. [26] or to some effects due to the
grain size distribution.
In addition to fayalite, the slag also contains small
quantities of other phases, which also undergo changes
during the heat treatment. The process is complex and the
calculated values of the kinetic parameters may differ from
those of pure single-phase components of the slag due to the
fact that the processes can interfere. This explains the
observed differences of the calculated values of the activa-
tion energy in some of the samples studied. In case of a
complex process, the effective activation energy of a solid-
state reaction is generally a composite value determined by
the activation energies of various processes and by their
influence on the overall reaction rate [43–46, 52, 53]. Since
the oxidation develops in several steps with a different
activation energy, the total rate of the process varies with
temperature and degree of conversion and the effective
activation energy will be a function of those two parameters.
Kissinger and Ozawa methods have intrinsic limitation.
For example, they are not able to detect reaction com-
plexities over the course of the reaction. In more compli-
cated case, Kinetics Committee of the International
Confederation for Thermal Analysis and Calorimetry (IC-
TAC) for carrying out kinetic computations on thermal
analytical data recommended the use of isoconversional
methods [52]. The TG data were processed using the iso-
conversional principle. The kinetic parameters are deter-
mined according to the computation procedures of Ozawa–
Table 1 The peaks temperatures Tp of the DTA curves (K)
Heating rate b/K min-1 Gas flow rate 20 mL min-1 Gas flow rate 35 mL min-1 Gas flow rate 50 mL min-1
I II III IV I II III IV I II III IV
4 – 694 852 1,123 560 669 846 1,117 582 678 847 1,120
8 – 702 867 1,159 582 691 856 1,149 585 689 854 1,157
12 – 709 882 1,182 588 708 874 1,176 588 711 873 1,178
16 588 718 888 1,206 595 715 886 1,200 – 717 883 1,183
20 601 724 902 1,218 597 722 900 1,216 616 735 897 1,199
Kinetics of copper slag oxidation
123
Flynn–Wall (OFW) [50, 51] and the procedures of Kis-
singer–Akahira–Sunose (KAS) [48, 54].
The changes of degree of conversion (a) with tempera-
ture are shown in Figs. 6, 7, and 8. The activation energy
Ea and pre-exponential factor are calculated by the equa-
tions of OFW and KAS. Single OFW and KAS plots are
shown in Fig. 9, respectively. The dependences of the
activation energy Ea on the degree of conversion are pre-
sented in Figs. 10 and 11. Values of Ea obtained at dif-
ferent gas flows are approximately equal; i.e., the variation
of the gas flow rate does not affect the reaction rate of the
process. Four stages of slag oxidation can be distinguished
on the Ea curves depending on conversion progress: the
first one with constant Ea at conversion from 0.2 to 0.3; the
second with decreasing Ea at conversion from 0.3 to 0.5;
third with increasing Ea at conversion from 0.5 to 0.7; and
fourth with constant Ea at conversion from 0.7 to 0.8. As
can be seen from Figs. 10 and 11, the values of the acti-
vation energy are constant in temperature range 800–950 K
(a increased between 0.2 and 0.3). The Ea values are about
122 kJ mol-1 calculated by KAS equation and about
139 kJ mol-1 calculated by OFW equation. They are close
to Ea values calculated by second peak of DTA curves and
it could be assumed that transformation of magnetite to
hematite is the rate-controlling process of the copper slag
oxidation up to temperatures of 950 K. The second stage of
oxidation is characterized by decreasing of the calculated
activation energy to 76 kJ mol-1 (KAS) and 94 kJ mol-1
(OFW). Maximum values of the calculated activation
energy of about 170 kJ mol-1 (KAS) and 180 kJ mol-1
(OFW) remain constant until the end of the process. They
Table 2 Activation energies (E/kJ mol-1), the pre-exponential factors (lnA/s-1), and regression coefficients (r2) obtained in Kissinger and
Ozawa methods by the data from Table 1
Gas flow rate/mL min-1 I peak II peak III peak IV peak
E lnA r2 E lnA r2 E lnA r2 E lnA r2
Kissinger
20 201 26.47 0.97 193 18.68 0.97 170 8.62 0.99
35 108 14.33 0.96 107 10.01 0.99 164 14.37 0.94 161 7.69 0.99
50 101 8.83 0.93 173 15.72 0.94 215 14.18 0.99
Ozawa
20 213 38.45 0.98 170 25.72 0.95 191 21.88 0.99
35 117 26.49 0.97 118 22.63 0.99 178 26.74 0.96 242 27.44 0.99
50 112 21.46 0.94 187 21.54 0.99 230 26.1 0.98
1.2
1.4
1.6
1.8
2
2.2
2.4
2.6
2.8
3
3.2
0.81 0.83 0.85 0.87 0.89
103/Tp /K–1
ln(H
eatin
gra
te,
/K
min
–1)
–1
–1
–1
b
β
20 ml min
35 ml min
50 ml min–12.8
–12.6
–12.4
–12.2
–12
–11.8
–11.6
–11.4
–11.2
–11
0.81 0.83 0.85 0.87 0.89 0.91
103/Tp /K–1
ln( β
/Tp2 )
–1
–1
20 ml min
35 ml min
50 ml min–1
aFig. 5 Relationship between
ln(b/Tp2) and 103/Tp—Kissinger
plot (a) and between ln(b) and
103/Tp—Ozawa plot (b) for
copper slag oxidation for the III
maximum of DTA curves,
obtained at different gas flow
rates
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Temperature /K
Con
vers
ion
4K min-1
8K min-1
12 K min-1
16 K min-1
20 K min-1
550 650 750 850 950 1050 1150 1250
Fig. 6 Temperature dependence of the degree of conversion, a,
during a nonisothermal oxidation of copper slag at flow rate of
oxidizing gas 20 mL min-1. Data were obtained from TG analysis at
different heating rates
S. Gyurov et al.
123
are close to E values calculated by the forth peak of DTA
curves. A more detailed study in temperature range
950–1,120 K is difficult because several simultaneous and
complex processes can occur. Khawam and Flanagan [55]
have shown that variation of activation energy with the
reaction progress is a result of the complex nature of the
solid-state reaction. The slag oxidation includes decom-
position of fayalite, adsorption of oxygen, diffusion of iron
and other species, growth of layers of iron oxide and sili-
cate phase. Therefore, the interpretation of kinetic data is
difficult and could not point unambiguously rate-control-
ling process.
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Temperature /K
Con
vers
ion
4K min–1
8K min–1
12K min–1
16K min–1
20K min–1
550 650 750 850 950 1050 1150 1250
Fig. 7 Temperature dependence of the degree of conversion, a,
during a nonisothermal oxidation of copper slag at flow rate of
oxidizing gas 35 mL min-1. Data were obtained from TG analysis at
different heating rates
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Con
vers
ion
4 K min–1
8 K min–1
12 K min–1
16K min–1
20 K min–1
Temperature /K550 650 750 850 950 1050 1150 1250
Fig. 8 Temperature dependence of the degree of conversion, a,
during a nonisothermal oxidation of copper slag at flow rate of
oxidizing gas 50 mL min-1. Data were obtained from TG analysis at
different heating rates
1
1.5
2
2.5
3
3.5
0.7 0.9 1.1 1.3
103/Tα /K-1
ln( β
)
0.2
0.4
0.6
0.8
a
-13
-12.5
-12
-11.5
-11
-10.5
-10
0.7 0.9 1.1 1.3
103/Tα /K-1
ln( β
/Tα2 )
0.2
0.4
0.6
0.8
bFig. 9 Relationship between
ln(b) and 103/Ta—OFW plot
(a) and between ln(b/Ta2) and
103/Ta—KAS plot
(b) calculated from TG data at
conversion 0.2, 0.4, 0.6, and 0.8
80
100
120
140
160
180
200
0.15 0.25 0.35 0.45 0.55 0.65 0.75 0.85
Conversion (α)
Eα
/kJ
mol
–1
–1
–1
20 mL min
35 mL min
50 mL min–1
Fig. 10 Dependence of activation energy (Ea) on the degree of
conversion (a) (Ea–a curve) for nonisothermal oxidation of copper
slag, calculated from TG data by KAS method
60
80
100
120
140
160
180
0.150 0.250 0.350 0.450 0.550 0.650 0.750 0.850Conversion (α)
Eα
/kJ
mol
–1
–1
–1
20 mL min
35 mL min
50 mL min–1
Fig. 11 Dependence of activation energy (Ea) on the degree of
conversion (a) (Ea–a curve) copper slag Ea depending on the degree
of conversion, calculated from TG data by OFW method
Kinetics of copper slag oxidation
123
Conclusions
The simultaneously performed thermal (TG/DTA), XRD,
and electron-microscopic analyses (SEM) of air oxidized
slag prove that the process is complex and takes place in
four stages. The first two stages take place in the temper-
ature range from 673 to 873 K, where the cubic phase with
a spinel type structure firstly oxidizes to metastable spinel
c-Fe2O3, and consequently to a-Fe2O3. The third stage is
the oxidation and decomposition of the fayalite phase with
the formation of two phases—hematite and amorphous
silicate at temperatures up to 873 K. Finally, the forth stage
is the decomposition of residual fayalite with simultaneous
polymorphic transitions in the silicate and iron phases.
These elementary processes overlap to a certain degree
but the use of methods, independent of the reaction model,
makes it possible to calculate the activation energy for the
single stages, as well as the changes of the activation
energy with the degree of conversion. The values for the
first and second stage are close to these, obtained by
Sanders and Gallagher, and for the fourth stage to those
obtained by Gaballah et al. The process of slag oxidation is
accompanied by structural transformation and formation of
structure of ordered platelike crystals of hematite, amor-
phous silicate phase, and residual fayalite.
Acknowledgements This research is funded by EU Operational
Program ‘‘Development of the Competitiveness of the Bulgarian
Economy’’ 2007–2013 under Contract No. BG16PO003-1.1.01.-
0224-C0001. The authors wish to thank Aurubis Bulgaria AD for the
supplied slag.
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