T4p chi Khoa hoc DHQGHN Khoa hoc Tq nhi6n vA C6ng ngh6- Tip 29,Sti7 (2013) 65-70
Synthesis and charactenzation of Mg-Al-O
hydrotalcite - type material
Nguydn Ti6n Th6o*
Faculty of Chemistry, VNIJ (Jniversity of Science, 19 L€ Thdnh T6ng Str., Hodn Kiilm Dist., Hanoi, Vietnam
Received 06 J:uly 2012
Revised 14 August 2012; accepted 20 March 2013
Abstract.
Mg-Al
layered double -hydrotalcite (LDH) samples were prepared through the precipitation method. Both hydrotalcite samples and their calcined forms are characterized by XRD, BET, SEM, TEM and FTIR. The former shows a lamellar structure with the presence of carbonate ionsin
the interlayers. After calcination, the filamentsof
the parent solid were completely disappeared and the Mg-Al LDH is coriverted to the mutual mixtwe between MgO and AlOx. The latter yields a higher specific surface area and smaller particle domaiqs.Keywords: Mg-Al hydrotalcite, LDH, perclase, MgO, micropore.
1. Introduction
Layered double hydroxides (LDHs), named
as anionic clays or
hydrotalcite-type compounds,are a family of
materials withgeneral formula
[Ar-*2*B*3*(oH)r]^*[Yn- vn.yHzO]*- (O< x < 0.33) where A2* and 83* aredivalent and trivalent metal ions, and Yn- is an anion
with n-
valent [1,2].Their
structure is composedof brucite-like layers
Mg(OH)2, where apartial
Az+lB3+ substitution has taken place, e.g.Mg'* by
Al3*, resultingin a
netpositive charge, balanced
by
interlayer anions(generally carbonate, chlorate,
sulfate,nitrate...)
accompanied a variable amountof
water
[1].
Furthermore, someof
the Mg2*, aswell
as Al3* ions can be replaced respectively*
Tel:84-4-39331605.E-mail : n [email protected]
by
other divalent (e.g. Cu,Ni,
Co,Zn)
andlor trivalent(Ni,
Co, Fe, Cr, Ga, In) cations [1,3].Thus, there have been used as
potential materialsin many
applications suchas
ion exchangers, and absorbents...In the field of
catalysis, hydrotalcites and their derivates are
of
great interest due
to their high
surface area, phasepurity, basic
surface properties, andstructural stability 12,31. Mg-Al-
basedhydrotalcites are,
for
example, used as a basic catalyst for the transesterificationofpoultry
fatwith
methanol[5],
propane dehydrogenation [6] . Hydrotalcite-derived oxides catalyze hi gher alcohol synthesisfrom
COAI2, oxidationof
mercaptan, water gas shift reactions
[24].
Also,Mg-Al mixed
oxides preparedby
oxidative decompositionof
hydrotalcite precursors havebeen used in base-catalyzed
aldolcondensations, alkylations,
condensations, 6566
N .T. Thao lTap chi Khoa hoc DHQGHN, Khoa hoc Tu nhiAn oi C6ng nghQ, Tqp 29, 56' 1 (20L3) 55-70double-bond isomerization, reforming of
methanol
[3,4,7-lll.
In this
study,we
prepared some Mg-Al hydrotalcite-type materialswith the
Mg/Al molar ratioof 7/3
and studiedtheir
structure.Furthermore,
the
samplewill be
studied the structural change during heating condition.2. Experimental
2.1. Synthesis of Mg-Al hydrotalcite
A
desired amountof
1.60g of
sodiumcarbonate was dissolved in 25
ml
of water in a500-ml-beaker. The solution was heated to 65o
C. Then, 11.25 g of aluminum
nitratenonahydrate (AI(NO3)3.9H2O, 99
Y')
and 17.92g of
magnesiumnitrate
hexahydrate (Mg (NO3)2.6H2O,99yo) were dissolvedin
150 mlof
deionized water. The resulting suspension was added drop-wise
to the
preheated Na2CO3 solution. The pH of the solution was adjusted to approximately 9.50 using 1.5M
NaOH. Aftercompleting addition of the metal
nitrate solutions, the resulting suspension was kept at 65"C with stirring for 24 h. The precipitate was separatedftom the
solutionby filtering
and washedwith
1000ml of hot
deionied water.The filter cake was dried
in
an oven at 105 oC overnight and calcined at 450 oC for 2 hours in air to obtain the mixed Mg(Al)O. oxides.2. 2. Material characterization
XRD patterns were collected
in
a rangeof
10-80"
from a Philips X'pert
diffractometer equippedusing Cu Kcr
radiation. Scanning electron microscope(SEM)
imagesof
thecatalysts
are
acquiredon a Hitachi
5-800 operatingat l0 kV. TEM
observation wasconducted 'nrith a JEM-200CX
electron microscope.The BET surface
areas were determined byN,
adsorption on a MicrometricsASAP
2020 apparatusat
-196.C.
Elementalanalysis
of Mg, Al was
doneat
Columbia Service Center.3. Results and discussion
Elemental analysis of
hydrotalcite composition indicatedthat the Mg/Al
molarratio is
closeto a
nominal value(Mg/Al :
2.06). Power X-ray diffraction patterns for the
Mg-Al
hydrotalcite(LDH) and its
calcinedproduct are presented in Figure 1.
The MgAI-LDH exhibits a single
phasecoresponding to the layered double hydroxide
with a
sharp and asymmetric reflections at 2- thetaof ll
.5, 23 .2, 34.7 , 38.8, 46.3,
60.7 , 6l .8"[3,9,10]. These peaks are well matched with the
tzrget composition bf empirical
formulaMge.TAlsj(OH)r(CO3)0.15.xH2O hydrotalcite- type compound. Also, no peaks of other oxides detected were, indicating
a
pure substanceof
the
synthesizedhydrotalcite material.
The structureof
sucha
materialis
collapsed after calcination at 450oC and forms perclase MgO (JCPDS: 4-0829)[3]
evidencedby its
X-raydiffractions at
2-
thetaof
34.7 - 42.9 and 62.5' [3,5].In
this case, neither residual hydrotacitenor
crystallineAIO*
phases were detected in additionto the
presenceof a
single poorly crystalline MgO perclase [11]. The results let ussuggest
that Al3* cations remain
closely associatedwith MgO
structure,in
consistentwith
literature [1,2,10]. Therefore, the texturalstruchre of the
calcinedoxides
should be different from the parent one. To confirm this conduction,we have
collectedthe
physical adsorpfion/desorption of nitrogen at -796"C.N.T. Thio /Tqp chi Khoahoc DHQGHN, KhoahocTrt nhi€nai COng nghQ TQp 29, sd7 (2013) 6s-70 67
600
t00
;100 iDu t00
100 0
10 ,t5 50
t5
606i
70 ?5 $02-Thtt* (')
Figure L Power XRD patterns of MgAI-LDH and Mg(Al)Ox oxides,
,150
4(li) ] ii1
-r r'ill
250
:(il
150 l0ll
0.t 0.15 0.{ 0.45 0.5 0-5J 0.6 0-65 0,7 0.75 0.lt 0.sJ 0.9 0.9i I
Rclrtirc Prcsurc ( PiPo)
Figure 2. Isotherms of Mg-Al layered double hydroxide and calcined Mg(Al)Ox.
l.)
:.
z
The isotherms of both pattems are presented
in
Figure 2. Firstly, the nitrogen adsorption-
desorption isotherm
of
theMgAI-LDH
closely resemblesa type II
isotherm.In this
case,nitrogen absorption monotonically increases
with PPo value due to sorption in
thehydrotalcite mesopores
[2].
Meanwhile, the hysteresis loop resembles to type H3 hysteresisin the
relative pressure rangeof 0.8H.95,
indicating the formation
of
a new interparticleand intragallery porosity during calcination step
(Fie. 2). Isotherm exhibits an H3-
Wpe hysteresisat high
relative pressure,which
istypical for
aggregatesof
plate-like particles giving riseto
slit-shaped pores. Thiskind of
hysteresis
is
typicalfor
the presenceof
open large pores, which allow easy diffrrsion of the reactants through the materials.Alsq
the solid containsnot only
mesoporesbut
also some small amount of micropores.6S
N.T. Thio lTap chi Khoahqc DHQGHN, Khoahoc Tq nhi€n ai C6ng nghf, TW 29, 56'1 (2013) 55-70Figure 3. SEM images of MgAI-LDH (A) and calcined Mg(Al)O. (B) and TEM micrographs of MgAI-LDH (C)
and mixed Mg(Al)O. oxides (D)
For Mg-Al-O
mixed oxides,the
physical adsorption/desorption describesthe
hysteresis loop shapeof
the calcined oxides shows a H4 hysteresis loop in the relative pressure rangeof
0.4-0.9.
This is
clearly characteristicsfor
themicroporous materials. Calcining at 400-500"C leads
to the
removalsof
carbonate ions and water possibly destroyed a layered structureof the
hydrotalcite-like compounds.The
BET surface areas of the parent one (MgAI-LDH) is about 83 m2lg while that of the calcined one isup to 153 t?te t4l. During the
thermaldecomposition of
Mg-Al
hydrotalcites at 400oC,water and CO2 are formed by dehydroxylation
of OH
groupswithin
brucite layers and bydecarboxylation of interlayer
carbonates,respectively.
The
releaseof
these gaseous products createsa
significant porous structure and substantially increases the surface areaof
calcined hydrotalcites I I 2].
Figure 3,A. reveals the lamellar structure
of
the
Mg-Al LDH
aggregates consisting of small crystalliteswith
platelet morphologyin
theaverage diameter ranging between
25
and 50pm (Fig. 3). In the
caseof the
oxides, adiminution
of
the crystallinityof
the materialsN.T.Thio lTqp chiKhoahoc DHQGHN, KrcahscTtnhi\noiC6ngnghQTap29, Sdl' (2013)
55-70
59and of the diameter of crystallites was observed.
The morphology of Mg(Al)Ox oxides was also
investigated
by TEM. In this case,
theaggregates are consisted of several platelets but
the micrographs (Fig. 3,A.) only
showfilamentous formations. These filaments are known as the characteristic
of
hydrotalcite-like compounds [13]. The filaments are constructedFigure
4
displays theIR
spectraof
Mg-Allayered double hydroxide and
calcinedMg(Al)Ox oxides. The absorption at 3500-3600 cm'', presented in both specimens, is attributed to the H-bonding stretching vibration of the OH
in
water physically absorbed.A
shoulder may be present around 3095 cm-r,for
the caseof MgA|-LDH pattern, is attributed to
thehydrogen bonding between H2O and the anion in the interlayer
[].
The main absorption bandsof
the anions are observed between 1000 and 1800 cm-r. The carbonate anions in a symmetric environment are characterized by three bands at 1369, 869,686 cm-r. The bandsat
715, 1007and 1161 cm-t
a." all
associatedwith
AI-OH vibration frequencies, whereas signalsat
660and 852 are
characteristicsfor the
two absorption bandsof the
interlayer carbonate, respectively' I I 5].by a
large numberof
verytiny
pafticles[a].
The length of the filaments was up to 200 - 400 nm (Figure 3C) while, in the case of Mg(Al)Ox oxides, a significant diminution
of
the fibrous formation is observable (Fig. 3D). FI-IR results also indicatea
significant changein
structure between the hydrotalcite parent and the calcined oxides[].
4. Conclusions
A target composition of
MgozAlo3(OH)2(CO3)o rs.xHzO layered double hydroxide sample
was
successfully preparedthrough the conventional recipe
andcharacterized
by several
techniques. The uncalcinedhydrotalcite solids
present the filaments composed of numerous tiny particles.Both BET and
TEM
indicate the appearanceof both
microporesand
mesoporesand
thelamellar structure of Mg-AI-LDH.
After calciningMg-Al- LDH,
ion carbonates locatedin the
interlayers are escaped, facilitating theporosity
of the
calcined oxides.The
layered double hydrotalcite was globally destructed at 450oC,yielding an
intimate contact betweentwo or more oxide
components. Thus, the celcined pattern exhibits better porosity and higher surface area (154m'lg)
compared with the parent hydrotalcite (83 m'lg).Figure 4. FTIR spectra of Mg-Al layered double hydroxide and calcined Mg(Al)Ox.
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z {th
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r:0 ,.i0 l:?0 ljtD l,)?U )-r?0 2?:.0 :1r-{l .lj;o r!?fi
11$rrillrNb(r (u[r)
70 N.T.Thdo lTqp chi KhoahocDHQGHN, KhoahocTu nhiAnoi C6ng nghq, TQp 29, Sd1 (2013) 55-70
Acknowledgement
This
researchis funded by
VietnamNational Foundation for Science
and Technology Development (NAFOSTED) under grant number 104.99-201 1.50.References
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tel
[10]
Il
ll
[r2]
tl3l
lt4l
t15l
Nguy6n Titin
Th6oT6ng hgp va d{c tnmg vat Hgu Mg-Al-O ki6u hydrotalcite
Khoa H6a hgc, Trrdng Dai hoc Khoa hpc
fit
nhi6n, DHQGHN19 L€ Thdnh T6ng, Hodn Kidm, Hd N|i, Vi€t Nam
MAu xric t6c hydroxit l6p d6i (LDH) diAu chti theo phucrng ph6p d6ng ktit
tta.
MAu hydrotalcite vd mdu nungcta
n6 dAu du-o. c tQc trungbing
c6c phuong phSpvft lj
hipn d4i nhu XRD, BET, SEM, TEM, FT-IR. Mdu Mg-AI-LDH c6 cAutrfc
phitin c6 chtia c6c sgi nho vd c5c ion cacbonatnim
xengita
c6c lorp. Sau khi nung, c6c sgi hydrotalcite bii5n m6t, tpo thdnh mQt h5n hqp oxit MgO vd AIO^pha hQn