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M.P. Balogh et al. / Journal of Alloys and Compounds 350 (2003) 136–144
curves predict a mass loss of 5.55 wt%, while the observed
TGA has a maximum weight loss of 4.2 wt%.
ranges from good to acceptable. For purified NaAlH4,
because the observed TGA curve shows hydrogen release
very close to the stoichiometric 5.55 wt%, the model by
construction fits the high-temperature endpoint closely. For
both iron ball-milled materials, the TGA experiment is
overestimated only slightly by the two calculations. For
as-received NaAlH4, the model overestimates the high-
temperature TGA weight loss by about 10%, which
corresponds to the nominal purity of the material. For WC
ball-milled pure material the TGA decomposition is some-
what less than that obtained from the two calculations.
This sample is anomalous in that the absence of any low
temperature Al signal indicates that ball-milling did not
decompose a measurable amount of NaAlH4, while the
appreciable low temperature Na3AlH6 signal indicates that
about 16% of the sample has already converted to
Na3AlH6. This explains why the Na calc curve starts at
somewhat below 100%.
The calculated TGA curves for the Ti-doped NaAlH4
(Fig. 7) are the least satisfactory of the materials tested.
Although the TGA curves calculated by both the Na and
Al method agree very nicely with each other, neither
agrees at all well with the observed TGA curve, lagging
the first decomposition by 17 8C. The observed TGA curve
does not show any feature which might be associated with
the second decomposition; rather, it seems to continuously
decrease until well above 300 8C. It seems clear that the
observed TGA curve above 230 8C shows some serious
sample decomposition which strongly interferes with our
ability to calculate the TGA from the XRD phase in-
formation. This most likely results from the decomposition
of the butoxide catalyst anions.
5. Discussion
Because the XRD data detects only Al crystallites of
appreciable lattice coherence length, and cannot in princi-
ple measure dissolved Al or very small aggregates of Al
atoms, the number Al0 which we determine from the low
temperature Al X-ray signal is an underestimate of all
initial free Al. Therefore, Eqs. (3) and (4) should, as they
do, overestimate the total decomposition which the TGA
experiment measures. This overestimate is most extreme in
the as-received and WC ball-milled pure NaAlH4, indicat-
ing that many Al atoms present in this sample are
dispersed too broadly to scatter X-rays and appear as XRD
data. These Al atoms presumably come from very slow
decomposition of the NaAlH4 at room temperature, and
cannot easily aggregate at low temperatures. This is also
the likely explanation for the absence of Al observed at
150 8C in the WC ball-milled purified NaAlH4 where the
Na3AlH6 shows a signal appreciable above 0. Proper
normalization of the calculated TGA traces would move
them closer to the experimental curve.
Thus, the decomposition of as-received NaAlH4 and all
three ball-milled NaAlH4 materials seems to be consistent
with Eqs. (1) and (2) above, with hydrogen release
correlating to a certain extent with the formation and
decomposition of Na3AlH6. The formation of Na3AlH6
can occur at various temperatures for materials prepared by
different methods, but it is always in better agreement with
the formation of Al crystallites. This seems to be in
agreement with the suggestion of Gross et al. [11] that
hydrogen is primarily bonded as AlH3. They suggested
recasting Eqs. (1) and (2) as
Comparison of Figs. 2 and 7 shows a decrease of the
temperature at which the alanate completely converts to
NaH of 60 8C in the presence of the Ti catalyst. This is in
´
excellent agreement with results observed by Bogdanovic
and Schwickardi [6] and Jensen, Zidan, Mariels, Hee and
Hagen [10]. A similar decrease due to ball-milling of the
pure material in Fe crucibles is in agreement with the more
qualitative data presented by Zaluska, Zaluski, and Strom-
Olsen [8].
¨
A recent paper by Gross, Guthrie, Takara, and Thomas
[11] utilized somewhat different equipment to obtain X-ray
diffraction phase identification data on purified and cata-
lyzed NaAlH4. Our results differ with theirs in some
details. Gross et al. [11] observed rapid and reversible
changes in the NaAlH4 peak intensities upon warming, and
attributed them to distortions in the crystal lattice. Exami-
nation of our figures shows very large NaAlH4 peak
intensity fluctuations in Fig. 3, lower fluctuations in Fig. 2,
and least in Fig. 4; the fluctuations decrease as crystallite
size decreases from 100 to 20 to 2 mm. We believe these
fluctuations are large when a small number of large
crystallites expand with heating and shift in and out of the
diffracting condition. With the ball-milled 2 mm material,
positional movements average out, and only small fluctua-
tions are seen.
Furthermore, we do not see any trace of either the X1 or
X2 phase observed by Gross et al. [11]. We do, however,
see traces of NaSiO3 and a complex Na–Al silicate
forming over 400 8C which we believe incorporate silicates
from the sample tube. Perhaps the suggestion of Gross et
al. that the X2 phase may incorporate Be from their
window is correct.
(NaH)(AlH3)↔1/3 (NaH)3(AlH3) 1 2/3 (AlH3)↔
(NaH) 1 (AlH3)
(6)
(7)
Let us take a somewhat deeper look at what the TGA
modeling calculation reveals about decomposition in so-
dium alanates. For all samples except the Ti catalyzed:
In general the normalization of our TGA calculations
AlH3↔Al 1 3/2H2,
which clearly have the desired form. In the purified
NaAlH4 the AlH3 seems to be much more long lived than