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Copyright: American Scientific Publishers
Copyright © 2006 American Scientific Publishers
All rights reserved
Printed in the United States of America
Journal of
Nanoscience and Nanotechnology
Vol. 6, 726–730, 2006
Preparation of Vermiculite Nanoparticles Using
Thermal Hydrogen Peroxide Treatment
Zdenˇ ek Weiss,
†
Marta Valášková,
∗
Jana Seidlerová, Monika Šupová-Kˇ rístková,
Ondˇ rej Šustai, Vlastimil Matˇ ejka, and Pavla
ˇ
Capková
Institute of Materials Chemistry, Technical University Ostrava, 17. listopadu 2172,
708 33 Ostrava-Poruba, Czech Republic
Powdered natural Mg-vermiculite (Letovice, Czech Republic), with the formula (Mg
035
K
002
Ca
001
(Mg
239
Fe
3+
051
Fe
2+
002
Al
008
(Si
264
Al
133
Ti
003
O
10
(OH)
2
· 497H
2
O and particle size <5 m, was used
for the investigation of exfoliation after hydrogen peroxide and/or microwave treatment (600 W).
A sample heated in the microwave oven for 40 min exhibits a 11% mass loss and reduction of the
001 peak intensity in the X-ray diffraction pattern. The basal 001 peak intensity of untreated Mg-
vermiculite sample (I
001
= 100%) drops to 35% in the microwave treated sample. Only the sample
treated for 5 h at 80
C fully rehydrated after 120 min at room temperature. A more pronounced
reduction of the 001 peak intensity (to 8%) was observed after hydrogen peroxide treatment of
the sample at 25
C. The combination of a five-hour hydrogen peroxide treatment at 80
C and
subsequent microwave heating leads to an effective extinction of the 001 diffraction in the XRD
pattern. The 001 diffraction profile becomes very diffuse with peak intensity less than 1%. The
degree of reduction of the 001 diffraction intensity also depends on the time and temperature
of hydrogen peroxide treatment and on the peroxide concentration. An even more pronounced
reduction of the peak intensity is caused by exfoliation of particles to nano-domains coupled with a
randomization of the c-axes.
Keywords: Mg-Vermiculite, Exfoliation, Nano-Domains, Hydrogen Peroxide, Microwave, X-ray
Diffraction.
1. INTRODUCTION
The layered silicates (phyllosilicates) represent important
native materials, which are utilized in different areas of
industry. In recent years phyllosilicates have found wide
exercise in the field of polymer/layered silicate nanocom-
posites (PLSN). The advantages of PLSN include impro-
ved stiffness, strength, toughness, and thermal stability as
well as reduced gas permeability and coefficient of thermal
expansion (e.g. Thostenson,
1
Alexandre, and Dubois.
2
)
The size of phyllosilicate nanoparticles is important
parameter for manufacturing of this nanocomposites. The
best properties are achieved when very fine phyllosilicate
particles are homogenously dispersed in polymer matri-
ces. For this reason new, more effective methods for the
delamination/exfoliation of phyllosilicates are developed.
Thermal and chemical treatment can be used for
exfoliation/delamination of phyllosilicates. Especially suit-
able are phyllosilicates containing molecular water in
the interlayer, because their exfoliation results from a
∗
Author to whom correspondence should be addressed.
spontaneous escape of the interlayer molecular water.
Montmorillonite, hectorite, and saponite are among the
most commonly used phyllosilicates for the prepara-
tion of PLSN (Okamoto
3
). Vermiculite is other kind
of phyllosilicate that is abundant and much cheaper as
compared with montmorillonite, hectorite, and saponite.
Mg-vermiculite belongs to 2:1 phyllosilicates containing
hydrated cations in the interlayer. According to its struc-
ture determined by Shirozu and Bailey,
4
the interlayer Mg
is octahedrally coordinated with water molecules form-
ing a mon-octahedral sheet. The interlayer and the 2:1
layer thicknesses are equal to 7.5 Å and 6.6 Å, respec-
tively. The removal of the interlayer water molecules dur-
ing thermal decomposition leads to the formation of less
hydrated vermiculite phases (e.g. Weiss and Rowland,
5
de
la Calle et al.,
6
Graf von Reichenbach and Beyer
7 8
). Mg-
vermiculite in equilibrium with a humid atmosphere at
25
C exhibits the first basal spacing at 14.36 Å. How-
ever, the X-ray diffraction (XRD) patterns of dehydrated
and rehydrated Mg-vermiculite in open-air humid atmo-
sphere display a significant variation of the position of the
726 J. Nanosci. Nanotechnol. 2006, Vol. 6, No. 3 1533-4880/2006/6/726/005 doi:10.1166/jnn.2006.116