Low-temperature synthesis of Ge nanocrystals in zeolite Y
H. Migueza) and V. Fornes
´
´
´
Instituto de Tecnologıa Quımica (UPV-CSIC), Avenida de los Naranjos s/n 46022, Valencia, Spain
F. Meseguer
Instituto de Ciencia de Materiales (CSIC), Cantoblanco 28049, Madrid, Spain
F. Marquez
´
Instituto de Tecnologia Quımica (UPV-CSIC), Avenida de los Naranjos s/n 46022, Valencia, Spain
C. Lopez
Instituto de Ciencia de Materiales (CSIC), Cantoblanco 28049, Madrid, Spain
͑Received 3 April 1996; accepted for publication 1 August 1996͒
A method for obtaining Ge nanocrystals has been developed using the porous structure of zeolite Y
as a matrix. Samples were obtained by reduction of GeO2 nanocrystals, previously grown in zeolite
␣ cages, in H2 at 470 °C. This is apparently the lowest GeO2 reduction temperature reported and is
probably due to the influence of the host. Ge crystallites so formed present an absorption edge at 2.2
eV, which is shifted ϳ1.4 eV with respect to the bulk value. A softening and an asymmetric
broadening of the Raman peak were also observed. We can estimate an average diameter of 3 nm
for the Ge nanocrystals from both results. © 1996 American Institute of Physics.
͓S0003-6951͑96͒01142-4͔
Semiconductor nanocrystals have gathered great impor-
tance due to the possibility of developing novel electronic
devices and studying quantum confinement effects. Strong
exciton confinement effects are expected when crystal size
(L) value is lower than the exciton effective Bohr radius1,2
(RB). Phonon confinement occurs when L is small enough to
consider the phonon described by a wave packet instead of a
plane wave.3 Several methods using different matrices for
obtaining germanium particles with nanometric size have
been reported.4–8 In most cases high temperatures ͑700–
800 °C͒ are needed. As far as we know, only Craciun et al.5
have previously reported a low temperature (550 °C͒ synthe-
sis of germanium nanocrystals using ultraviolet oxidation of
Si0.8Ge0.2 strained layers.
Zeolites are crystalline, porous, aluminosilicate materials
which are well known as catalysts for organic reactions.9
Zeolite cages act as nanoreactors where chemical processes
take place in milder conditions than usual. Also the uniform
pore size, varying from 0.4 to 10 nm depending on the type
of zeolite, make them suitable to be used as hosts for semi-
conductor nanoparticles. Although many different zeolites
have already been used as matrices for obtaining semicon-
ductor nanocrystals with uniform size,10,11 the improvement
of their synthesis reactions has apparently not yet been re-
ported. Many works are reported on type II–VI and III–V
nanoparticles synthesized in zeolites, but few on type IV.12
We present here a novel and simple chemical method for
obtaining germanium nanocrystals using the ␣ cages of zeo-
lite Y as hosts. Zeolite Y ͑faujasite-type͒ possesses two dif-
ferent quasispherical cages, the sodalite cage or -cage ͑di-
ameter 0.8 nm͒ and the supercage or ␣-cage ͑diameter 1.3
nm͒. Initially, GeO2 crystallites were formed by the hydroly-
sis of gaseous GeCl4 at room temperature by H2O trapped in
the zeolite ␣ cages, since the GeCl4 molecule is too large to
enter the  cage. The remaining GeCl4 and HCl were re-
moved by heating and vacuum cleaning. Following this,
Ge0 nanocrystals were obtained by reduction in H2. This
process was monitored in situ using temperature pro-
grammed reduction, where a flux of H2 ͑15%͒ in Ar was
passed over the oxidized sample as the temperature increased
with a rate of dT/dtϭ1°C/min. Two different H2 uptake
peaks at 410 and 470 °C were observed, which corresponded
to GeO and Ge0, respectively, as was confirmed by x-ray
photoelectron spectroscopy in situ analysis. Ge nanocrystals
formation takes place at 470 °C, ϳ200 °C lower than the
reduction temperature of bulk GeO2.8 The low reduction
temperature of GeO2observed in zeolite Y could be related to
the effect of the zeolite cage walls on the GeO2 molecular
orbitals. Molecular orbital calculations performed by semi-
empirical and ab initio methods could support this assump-
tion. These kinds of calculations have already shown that the
lowering of the activation energy of several processes in-
volving organic molecules is due to the effect of the cage on
the molecular orbitals of the inclusions.13,14
In order to study separately the optical properties of the
sample at the different stages of the reduction process, three
different reduction experiments were performed. Figure 1
shows the H2 uptake curves obtained at different final tem-
peratures during the zeolite/GeO2 sample reduction. The fi-
nal temperatures employed were 410 °C ͓see Fig. 1͑a͒, GeO
formation͔, 470 °C ͓see Fig. 1͑b͒, Ge0 nanocrystals forma-
tion͔, and 900 °C ͓see Fig. 1͑c͔͒. The third experiment was
performed to prove that the stability of the Ge0 nanocrystals
depends on the zeolite structure, which ruptures at 900 °C.
This was proven by x-ray diffraction.
The optical absorption of the samples was measured
through diffuse reflectance ͑DR͒ spectroscopy ͑see Fig. 2͒.
The first sample ͑GeO in zeolite͒ did not absorb in the region
of interest ͓see Fig. 2͑a͔͒. The second sample ͑Ge0 nanocrys-
tals͒ presents an absorption edge at ϳ2.2 eV ͓560 nm, see
Fig. 2͑b͔͒, which is blue shifted ϳ1.4 eV with respect to the
bulk value, 0.79 eV ͑1570 nm͒. The sharpness of the absorp-
a͒
Electronic mail: becitq@itq.upv.es
Appl. Phys. Lett. 69 (16), 14 October 1996 0003-6951/96/69(16)/2347/3/$10.00 © 1996 American Institute of Physics 2347
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