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SCIENTIFIC PAPER
Magnesium salts as compounds of the preparation of magnesium
oxide from Tunisian natural brines
Souheil Behij; Halim Hammi*; Ahmed Hichem Hamzaoui; Adel M’nif
Technological park of Borj Cedria
National Center of Research in Materials Sciences
Valorization Laboratory of Useful Materials
Tourist road of Soliman B. P. 73 - Soliman 8027, Tunisia
Received 7.12.2011.
Revised 8.6.2012.
Accepted 8.6.2012.
* Corresponding author : Halim Hammi, Technological park of Borj Cedria, National Center of
Research in Materials Sciences, Valorization Laboratory of Useful Materials, Tourist road of Soliman
B. P. 73 - Soliman 8027, Tunisia; Tel: +216 79 325 470; Fax: +216 79 325 314; E-mail :
2
Abstract
Magnesium oxide is one of the most important magnesium compounds used in industry. The
production of MgO is often done from calcined magnesium carbonate or from natural
magnesium saline solutions (sea water and brines). In the case of these solutions, magnesium
oxide is precipitated after the addition of a strong base (eg. Ammonia). Magnesium hydroxide
is calcined after its separation from the excess resulting from the strong base through
filtration. Thus, magnesia qualities may differ depending on several physical parameters and
particularly on the nature of the compound. Consequently, two different compounds were
selected: magnesium chloride and magnesium sulphate which can be recovered from Tunisian
natural brines. Three physical factors were considered: calcination temperatures, precipitation
temperatures and calcination time of Mg(OH)2. The decomposition of Mg(OH)2 was
investigated by DTA/TGA. Mass losses vary in the range (23.0%-29.9%). Starting
decomposition temperatures are between 362°C and 385°C. The MgO produced from MgSO4
under 1000°C within 48 hours of calcination time and with 40°C as a reaction temperature for
Mg(OH)2 shows a good crystallinity and is of a cristallyte size of 86.3 nm and has a specific
surface area equal to 16.87 m2g
-1. Finally, morphological differences between MgO
agglomerates at different temperatures were observed by SEM. Consequently, magnesium
sulphate as precursor for preparing MgO is selected.
Keywords: Cristallinity; Crystallite size; Mg(OH)2; MgO or periclase; Specific surface area.
3
INTRODUCTION
Magnesium oxide (MgO or periclase) is among the most important industrial magnesium
compounds. Approximately 20% of the world’s production comes from seawater, brines and
desalination of reject brine [1]. Magnesium oxide is used as an exceptionally important
material in catalysis [2,3], toxic waste remediation [4], or as additives in refractory products,
paint, manufacture of fertilizers, animal foodstuff, building materials (Sorel cement,
lightweight building panels) and superconductor products [5-7]. A panel of fundamental and
applied studies exists in literature reviews [7-11]. It particularly shows that magnesium
hydroxide production from seawater or brines is precipitated by the addition of a strong base
(eg. Ammonia). Later on, separation is calcined to produce MgO. It is important to note that
magnesia qualities may differ depending on the physico-chemical conditions of preparation
and on the compound type which is why two compounds are selected to be tested: magnesium
chloride and magnesium sulphate. The respective final products are compared on the basis of
their X-ray diffractogram, specific surface area and microstructural differences.
To accomplich this task we first make a DTA/DTG decomposition study of Mg(OH)2
(brucite). After that, XRD Results are used to study the impact of calcination temperature, the
impact of calcination time and finally the impact of Mg(OH)2 reaction temperature.
Additionally, X-ray diffractograms are used to calculate MgO crystallite size depending on
some physical parameters such as calcination temperatures and reaction times. At a later
stage, the specific surface area is determined in order to confirm the particles’ cristallyte size
variations. Finally, MgSO47H2O is selected as the compound used for MgO preparation.
EXPERIMENTAL
Methodology
The industrial exploitation of the abundant natural brines in the Sebkhas and Chotts of the
Tunisian South is conditioned by the development of specific processes, the technique and
economic viabilities of which have to be demonstrated beforehand. For this purpose, we
agreed to study this kind of saline solutions previously studied by many authors[12,13],
assimilated to a quinary system represented by Na+, K
+, Mg
2+/ Cl
-, SO
2- // H2O.
Natural Brine is a highly concentrated complex aqueous solution. In the case of the brine
called Sebkha El Melah, magnesium, chloride and sulphate ions seem to be sufficiently high
to recover magnesium salts like epsomite (MgSO4.7H2O) and bischofite (MgCl2
.6H2O) useful
in a wide range of applications (such as fertilizers, Sorel cement, and refractory compounds).
4
Epsomite is obtained by polythermal crystallization conducted in two steps. The first one is
completed at 35°C, temperature during which the brine is evaporated to reach a density of
1.29 g.cm-3
and the maximum concentrations of magnesium and sulphate ions. The second
step consists in cooling the above mentioned pretreated solution at 0°C in order to crystallize
MgSO4.7H2O.
Purification of the product, realized by washing it with a saturated solution of Epsom salts,
provides 99% Epsomite purity [14].
For bischofite synthesis, the concluded process is mainly composed of six stages based on
two main unit operations, firstly isothermal evaporation and crystallization and then chemical
precipitation.
The resulting brine, composed mainly of magnesium chloride, is concentrated by isothermal
evaporation at 35°C to precipitate magnesium chloride. The recovered product, collected from
the final stage, is mainly composed of bischofite the purity of which exceeds 90% [15].
MgO powders preparation is done in two steps starting from two different precursors:
bishofite (MgCl2.6H2O) and epsomite (MgSO4
.7H2O) successfully produced from Tunisian
natrual brines.
At first, each reactant was dissolved in deionized water at room temperature to produce 0.8 M
Mg2+
solution. After that, an excess of ammonium hydroxide was added and vigorously
stirred at 50°C with pH = 10. A white precipitate of Mg(OH)2 was obtained which was
thoroughly washed with distilled water and dried at 100°C during 2 hours. At this stage, the
following reaction takes place:
Mg2+
+ 2OH- Mg(OH)2 (1)
In a second step, magnesium hydroxide powders were calcined to produce MgO. The heating
treatment was carried out in an electric furnace by raising the temperature 10°C per minute.
Therefore, the below thermal reaction takes place:
Mg(OH)2 t MgO + H2O (2)
Materials
The X-Ray Diffractometer with a PHILIPS PW 3040 generator, goniometer PW 3050/60 θ/2θ
and a cathode of copper PW 3373/00 is used to distinguish MgO from two different
precursors. Microstructural differences between MgO agglomerates were examined using
SEM FEI Quanta 200. The decomposition of precipitated Mg(OH)2 was analysed by
5
DTA/TGA (DSC) SETARAM SETSYS EVOLUTION. The specific surface area was
determined by a QuantaChrome Autosorb-1 apparatus.
RESULTS AND DISCUSSION
Starting from the two compounds prepared from the natural brine Sebkha El Melah as
described above (MgCl2.6H2O & MgSO4
.7H2O), the two successive steps of brucite and
magnesia preparation are performed as previously indicated. The thermogravimetric
decomposition (DTA/DTG) of Mg(OH)2 was studied. The recovered products are
characterized by XRD and SEM.
Mg(OH)2 characterization
Mg(OH)2 decomposition (DTA/DTG) study
The start of Mg(OH)2 decomposition is studied using a DTA/DTG experiments. Mg(OH)2
experimental diagrams related to the compounds magnesium chloride and magnesium
sulphate are respectively presented in Fig. 1(a) and Fig. 1(b) It becomes possible to compare
masses’ loss of the two obtained powders to the theoretical ones from these two diagrams.
Figure 1(a)
Figure 1(b)
The above two DTA-DTG analyses show two endothermic peaks respectively related to
dehydration process and to magnesium hydroxide decomposition. The second phenomenon
occurs at 362°C and 385°C respectively for the compounds magnesium chloride and
magnesium sulphate. However, in terms of brucite (Mg(OH)2) theoretical decomposition,
30.864% mass loss should be achieved, which is slightly larger than the observed one
29.883% and 23.022% respectively. This is due to the incompletion of the decomposition
reaction within this temperature range. These results are in good agreement with others
presented elsewhere [16-18].
As a preliminary conclusion it comes into view that Mg(OH)2 prepared from the two studied
compounds is of good chemical purity but its morphology varies from one compound to
another. Furthermore starting decomposition temperature differs depending on the
compound’s nature. In order to clarify the compound’s impact on the final product, we
studied MgO prepared under different physical conditions.
Mg(OH)2 X ray diffraction description
The magnesium hydroxide prepared from the two above compounds was characterized by X-
rays, it was found that the produced compounds correspond to Mg(OH)2 regardless of the
considered compound. Figure 2 shows a marked diffractogramme of the compound obtained
from MgSO4.7H2O; an identical one is produced when MgCl2 is used as precursor.
6
Figure 2
Mg(OH)2 SEM description
The morphology of Mg(OH)2 from different precursors is explored by SEM analysis. Brucite
was dried accordingly at 100°C and after cooling was observed. Microstructural differences
were detected for the two compounds (Fig. 3). This observation indicates that magnesium
oxide products may present different physical properties related to the compound.
Magnesium hydroxide derived from magnesium sulphate shows a plate-like shape, the
particles were joined to each other forming spherical particles around 15 m which tend to
form large agglomerates (30 m).
Figure 3
MgO characterization
MgO X-ray diffraction study
X-ray diffraction will allow, in a first step, to qualitatively compare the crystallinity of the
obtained materials; such a parameter is related to the peaks’ intensity and their affinities. In a
second step, the diffractograms will be used to calculate the average crystallite size of the
prepared MgO in a more quantitative term. Regarding these two parameters, the following
effects are investigated: calcination temperature, calcination time and reaction temperature.
crystallinity
o Calcination temperature effect
As previously concluded, Mg(OH)2 decomposition starts at the range varying from 362 to
385°C, thus a calcination temperature ranging from 500°C to 1000°C for a duration of 2 hours
was operated in order to study the effect of such a factor on the different obtained products
from the two studied compounds. Figure 4a and b illustrate X-ray diffractograms
respectively for the precusors magnesium chloride and magnesium sulphate.
Figure 4
Figure 5 shows that all samples are magnesium oxide formed with CFC structure (NaCl type).
The best crystallinity corresponds to the calcination temperature of 1000°C with regard to the
two compounds. Nevertheless, it is important to note that MgO, obtained from MgSO4.7H2O,
presents the highest intensity and the sharpest peak at the same temperature. In addition,
unlike the MgCl2 compound, MgSO4.7H2O shows a gradual increase of intensity parallel to
that of temperature. These remarks clearly indicate the influence of the compound on the
properties of the final product (MgO).
7
o Calcination time effect
MgO calcination time is studied in the range 2h to 48h. Fig. 5 illustrates XR diffractogramms
for MgO obtained from magnesium sulphate at 1000°C (a similar result is concluded for the
other compound). Therefore, increasing the calcination time improves the crystallinity. As a
result, 48 hours of calcination time give the best results. CFC magnesium oxide is always
obtained.
Figure 5
o Reaction temperature effect
Mg(OH)2 reaction temperature parameter was studied in the range 25°C – 75°C. Fig.6
illustrates only XRD results for MgO obtained from the compound magnesium sulphate at
1000°C and with 48 h of calcination time. The variations of the peak intensities, which play
the function of temperature, are irregular. However, in terms of crystallinity, the below
diffractograms enable us to deduce that 40°C is the best reaction temperature for the two
compounds.
Figure 6
average crystallite size
The above diffractogramms are handled to determine the average crystallite size, L, of the
prepared powders. For this pupose, we applied Scherrer formula:
cos
9.0L (3)
where:
is the wavelength of the X-ray,
is the diffraction angle associated with a Bragg peak,
2
1
22 )( sm is the corrected full widh at half maximum (FWHM),
m being the FWHM of the well defined (200) Bragg peak,
s being that of a standard crystallized sample of MgO (Across sample).
Considering the two tested reactants, the crystallite sizes with calcination temperature,
calcination time and reaction temperatures are shown respectively in Fig. 7, Fig. 8 and Fig.9.
Figure 7
Figure 8
Figure 9
8
Fig. 7 shows that for the two precursors, the crystallite size increases in accordance with the
increase of calcination temperature. Crystallite sizes are within the ranges: (64.7 nm to 115.4
nm) and (18.1 nm to 86.3 nm) respectively for the compounds magnesium chloride and
magnesium sulphate. Therefore, the MgO obtained from magnesium sulphate has the smallest
particle size. This result enhances the relation between the full width at half maximum of
Bragg peaks and crystallite size. In fact, the FWHM is the result of the convolution of an
instrumental contribution and a size effect.
For the compound magnesium sulphate, the crystallite size increases with calcination time
(Fig. 8). For the other one (magnesium chloride), the evolution of crystallite is irregular. The
final sizes are lower than those obtained from magnesium sulphate after 48 hours of
calcination time. Calcination time effect on crystallite size seems to be more important than
that of the temperature effect (150 nm in 48 h and 80 nm at 1000°C).
Fig. 9 shows that MgO produced from magnesium chloride has an irregular evolution of
crystallite sizes. It is therefore difficult to confirm the previous conclusion, but for energy
considerations 40°C will be retained as the reaction temperature.
BET Specific surface
In order to confirm the above results, the specific surface area by BET for MgO powders
burnt-off at 1000°C during 24 hours are set up. The obtained results are 9.31 m2g
-1 and 16.87
m2g
-1 for magnesium chloride and magnesium sulphate respectively. These results confirm
that the sample obtained from the magnesium sulphate has the highest specific surface area
which is in concordance with the data [19-22] indicating that small particles have the highest
surface areas.
SEM study
The morphology of MgO powders obtained from different compounds is explored by SEM
analysis. Periclase powders (MgO) obtained at 1000°C during 48 hours from the two
compounds after cooling and SEM examination show the presence of fine particles, less than
1 m, forming agglomerates (less than 5 m) with homogeneous distribution (Fig.10).
At 1000°C, a well-defined plate-like morphology was observed which can be related to
periclase phase, a similar morphology has been reported elsewhere [23] .
CONCLUSION
The results of this study demonstrate that the MgO obtained from the two compounds has
different physical proprieties such as the crystallite size, shape, and structure. A set of
9
parameters like calcination temperature, calcination time and temperature of brucite
precipitation has to be controlled to produce a high quality product.
Intermediate and final products were characterized by X-ray diffraction, DTA/DTG analysis,
BET and SEM.
This study shows that 40°C is an appropriate temperature to obtain Mg(OH)2 from the
compounds used in the experiments.
The calcination temperature for MgO production with high crystallinity is set to be within the
range 800-1000°C. Within this interval, the maximum brucite decomposition into periclase is
achieved. Calcination time of 48h confirm the above result with a very pure product. Finally,
magnesium oxide obtained from magnesium sulphate is the best approach to obtain the ideal
product, due to its higher surface area, and eventually, to its smallest primary particle size at
the limits of calcination temperature. Besides, the specific area value can be related to the
microstructure of the sections disposed around a central nucleus. According to these results,
we select magnesium sulphate as the precursor to obtain magnesium oxide.
ACKNOWLEDGMENTS
This work was supported by the National Centre of Material Science Research. The authors
would like to thank the technical team for helpful assistance with the XRD, SEM and
DTA/DTG studies.
10
REFERENCES
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[5] W. Wang, X. Qiao, J. Chen, J. .Am. Ceram. Soc. 91 (2008) 1697-1699.
[6] Y.S. Yuan, M.S. Wong, S.S. Wang, J. Mater. Res. 11 (1996) 8-17.
[7] P. Yang, C. M. Lieber, Science. 273 (1996) 1836 1840- .
[8] G.W. Wagner, P.W. Bartram, O. Koper, K.J. Klabunde, J. Phys. Chem. B. 103 (1999) 3225-3228.
[9] A.I. Boldyrev, J. Simons, J. Am. Chem. Soc. 119(20), (1997) 4618–4621.
[10] M. Zhou, H. Zhu, Y. Jiao, Y. Rao, S. Hark, Y. Liu, L. Peng, Q. Li, J. Phys. Chem. C. 113 (20), (2009)
8945–8947.
[11] M. Sterrer, O. Diwald, E. Knozinger, J. Phys. Chem. B. 104 (2000) pp 3601-3607.
[12] R. Cohen-Adad, Chr. Balarew, S. Tepavitcharova, D. Rabadjieva, Pure Appl. Chem. 74 (2002) 1811-1821
[13] H. Hammi, J. Musso, A. M’nif, R. Rokbani, J. Calphad 27 (2003) 71-77
[14] H. Hammi, A. Mnif, R. Rokbani, J. Phys IV. Pr10 (2001) 157-163. [15] R. Fezei, H. Hammi, A. Mnif, LAAR. 39 (2009) 375-380.
[16] E. Alvarado, L. M. Torres-Martinez, A. F. Fuentes, P. Quintana, Polyhedron. 19 (2000) 2345-2351.
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Mater. Lett. 35 (1998) 317-323.
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[21] A.Pilarska, E.Markiewicz, F.Ciesielczyk, T. Jesionowski, Drying Technology, 29 (2011)1210–1218
[22] W. Wang, X. Qiao, J. Chen, H. Li, Mater. Lett. 61 (2007) 3218-3220.
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11
Figure captions
Fig. 1. DTA/DTG of Mg(OH)2 obtained from two different precursors : (a) MgO from
chlordie, (b) MgO from sulphate
Fig.2. Diffractogram of Mg (OH)2 prepared from MgSO4.7H2O.
Fig.3. Microstructure of Mg(OH)2 powders obtained from different precursors (2500x)
Fig.4. Calcination temperature effect on MgO obtained from different compounds :
(a) Magnesium chloride, (b) Magnesium sulphate.
Fig.5. Diffractogram showing the calcination time on MgO obtained from magnesium
sulphate precursor.
Fig.6. MgO obtained from magnesium sulphate diffractograms vs reaction temperature
Fig.7. Development of crystallite size with temperature on the crystallisation of MgO.
Fig.8. Development of crystallite size with calcination time on the crystallisation of MgO.
Fig.9. Development of crystallite size with reaction temperature on the crystallisation of
MgO.
Fig.10. Microstructure of MgO powders obtained from different precursors (5000x)
13
Position [°2Theta]
20 30 40 50 60 70 80 90 100 110
Counts
0
2000
4000
1 1
1;
bru
cite
3 1
1;
bru
cite
2 1
2;
bru
cite
2 2
2;
bru
cite
5 1
0;
bru
cite
6 0
1;
bru
cite
3 3
3;
bru
cite
6 2
1;
bru
cite
6 1
3;
bru
cite
3 0
5;
bru
cite
4 4
4;
bru
cite
6 4
4;
bru
cite
5 1
6;
bru
cite
5 5
5;
bru
cite
8 6
1;
bru
cite
Mg(OH)2
Search Unit Cell Result 1
Figure 2
Mg(OH)2 sulfate Mg(OH)2 chloride
Figure 3
2
Counts
15
Figure 6
Figure 7
Figure 8
0
20
40
60
80
100
120
140
400 500 600 700 800 900 1000 1100
Temperature (°C)
Cry
sta
llit
e s
ize (
nm
)
Chloride
Sulfate
0
20
40
60
80
100
120
140
160
2 6 12 24 48 Calcination time ( hours )
Chloride
Sulfate
Cry
sta
llit
e s
ize (
nm
)
Counts
2