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P. Kitschke et al.: Synthesis of GeO2 nanoparticles in benzyl alcoholsꢀ
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IQ2 (Quantachrome, Odelzhausen, Germany), which were evaluated
gave GeO2 particles with sizes ꢀ> ꢀ100 nm. It is proposed
that Lewis acid initiated partial polymerisation of ortho-
methoxy benzyl alcohol gave water, which results in the
formation of β-GeO2 upon hydrolysis. Nanoparticles below
by the BET method using p/p0 ratio of 0.150.
100 nm in size were obtained in benzyl alcohol under inert Syntheses
conditions. Their formation is assumed to be a result of
Reactions using ortho-methoxy benzyl alcohol were performed in an
an alkyl chloride elimination reaction mechanism. The
formation of β-GeO2 starting from benzyl alcohol under
ambient conditions is a result of slow diffusion of mois-
ture into the reaction mixture and gave the smallest GeO2
nanoparticles that exhibit sizes below 20 nm. The results
demonstrate that hydrolysis must be considered as an
important side reaction, even in a so-called non-hydro-
lytic processes, if water might be formed as a side product
or the presence of moisture is not fully excluded.
inert atmosphere (argon) glovebox. Reactions using benzyl alcohol
were performed in an inert atmosphere (argon) glovebox as well as
under ambient conditions to allow water diffusion into the reaction
mixture. Solvents were purified and dried by applying standard tech-
niques. Benzyl alcohol and ortho-methoxy benzyl alcohol were pur-
chased from Merck Schuchardt OHG (Hohenbrunn, Germany) and
Alfa Aesar (Ward Hill, MA, USA), respectively. Benzyl alcohol was used
without any purification for the synthesis under ambient conditions
(sample C). Ortho-methoxy benzyl alcohol and benzyl alcohol were
dried over molecular sieves for 3 weeks before using them for the syn-
theses under inert conditions. GeCl4 was purchased from ABCR GmbH
& Co. KG (Karlsruhe, Germany) and used without further purification.
Experimental
Synthesis of GeO2 in ortho-methoxy benzyl
alcohol – sample A
General
1H and 13C{1H}-NMR spectra were recorded on a Bruker (Bruker
Corporation, Billerica, MA, USA) ‘Avance III 500’ spectrometer at
ambient temperature. CH analysis was carried out with a ‘vario
MICRO’ from Elementar Analysensysteme GmbH (Hanau, Germany).
The PXRD patterns were collected using a STOE-STAD IP diffrac-
tometer from STOE (STOE and Cie GmbH, Darmstadt, Germany)
with Cu-Kα radiation (40 kV, 40 mA) and a Ge(111) monochroma-
tor. The crystallite size was estimated using the Scherrer equation:
K λ
GeCl4 (529.4 mg, 2.47 mmol) was added to ortho-methoxy benzyl
alcohol (12.79 mL, 103.7 mmol) and the mixture was stirred under an
inert atmosphere at room temperature for 22 h. The suspension was
centrifuged at 3000 rpm for 15 min for separating the pale pink GeO2
particles, which were then purified by centrifugation (at 3000 rpm for
15 min) of a suspension of the particles in THF (5 mL) and in ethanol
(5 mL) two times each, respectively, to quantitatively give pale pink
GeO2. The CH analysis [%] found for GeO2: C 1.06 and H 0.24. Both
PXRD and EDX analyses proved the formation of GeO2.
τ=
,
where τ is the volume weighted crystallite size, K is the
βcosθ
Scherrer constant here taken as 1.0, λ is the X-ray wavelength, θ is the
Bragg’s angle (in rad) and β is the full width of the diffraction line at
half of the maximum intensity (FWHM, background subtracted). The
FWHM is corrected for instrumental broadening using a LaB6 stand-
ard (SRM 660) purchased from NIST (National Institute of Standards
and Technology, Gaithersburg, MD, USA). The value of β was cor-
Synthesis of GeO2 in benzyl alcohol under inert
conditions – sample B
GeCl4 (942.0 mg, 4.39 mmol) was added to benzyl alcohol (20.00 mL,
192.3 mmol) and the mixture was stirred under an inert atmosphere at
reflux for 24 h. The pale yellow suspension was centrifuged at 3000 rpm
for 10 min to separate the GeO2 particles, which were then suspended
and purified by centrifugation (at 3000 rpm for 10 min) in THF (5 mL)
and in ethanol (5 mL) two times each, respectively, to quantitatively give
βi2nstrument
rected from ( βm2 easured and
are the FWHMs of measured and
standard profiles):
β2 =βm2 easured -βi2nstrument
.
The DLS measurements were performed on a Modell 802 from colourless GeO2. The CH analysis [%] found for GeO2: C 0.46 and H 0.13.
Viscotek™ (Malvern Instruments GmbH, Herrenberg, Germany) using Both PXRD and EDX analyses proved the formation of GeO2.
a laser light emitting diode at 830 nm. The THF and toluene suspen-
sions of the particles obtained by ultrasonic treatment were given in
a quartz glass cuvette for DLS measurements. Infrared spectra were
Synthesis of GeO2 in benzyl alcohol under ambient
recorded with a Nicolet IR 200 spectrometer from Thermo Scientific
conditions – sample C
(Thermo Fisher Scientific Inc., Waltham, MA, USA) in a KBr matrix.
Transmission electron micrographs and energy dispersive X-ray
spectroscopy experiments were obtained by a 200 kV-high resolution GeCl4 (713.8 mg, 3.33 mmol) was added to benzyl alcohol (14.54 mL,
transmission electron microscope [HRTEM, CM 20 FEG, Co. Philips 139.8 mmol) at 40°C. The mixture was stirred at 40°C under ambient con-
(FEI Europe, Europe NanoPort, Eindhoven, The Netherlands)] with ditions for 24 h. The colourless suspension was centrifuged at 3000 rpm
an imaging energy filter from Gatan (GIF). Specific surface analyses for 10 min to separate the GeO2 particles, which were then suspended
were performed with nitrogen adsorption-desorption isotherms at and purified by centrifugation (at 3000 rpm for 10 min) in THF (5 mL)
liquid nitrogen temperature (77 K) using a Quantachrome Autosorb and in ethanol (5 mL) two times each, respectively. Additional stirring of
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