Thermodynamics of Magnesium Hydride Nanoparticles
A R T I C L E S
Table 2. Summary of MgH2 Particle and Crystal Size Information
equilibrium pressure then the resultant thermodynamic values
calculated from these pressures will be biased.
As Determined by TEM and XRD18
Hydrogen equilibrium pressure measurements can be used
to determine thermodynamic quantities using the van’t Hoff
relationship for hydrogen desorption:
TEM average
particle size
XRD average
crystallite size
MgH2-A
MgH2-B
MgH2-C
MgH2-D
1-2 µm
15-40 nm
12-20 nm
2-7 nma
N/A
10.1 ( 0.3 nm
7.6 ( 0.3 nm
6.7 ( 0.4 nm
6.7 ( 0.7 nm
6.4 ( 0.1 nm
feq
∆H
RT
∆S
R
ln
) -
+
(2)
( )
f0
MgH2-Purchased
a Only crystallites could be discerned from the homogeneous sample.
where feq is the fugacity of hydrogen under equilibrium at a
given temperature T, f0 is a reference fugacity of 1 bar, and R
) 8.3145 J/K/mol H2 is the gas constant. The fugacity is the
activity of the real gas which provides a better representation
of the chemical potential of the system than pressure. In turn,
the fugacity (and hence pressure) can be calculated from ∆H
and ∆S using the exponential of eq 2 as follows (where f0 )
1):
pressure data extend up to ∼280 bar where the compressibility
of hydrogen is vital in determining accurate fugacity values.
Reprocessing Stampfer’s pressure data reveals that the fugacity
values that were calculated using the Beattie-Bridgeman EOS
do not match fugacities calculated using more recent EOS
models.30,33 The disparity leads to a change in Stampfer’s
reported ∆H and ∆S values from 74.4 ( 0.3 kJ/mol H2 and
135.1 ( 1.9 J/mol H2/K to 76.2 ( 1.1 kJ/mol H2 and 137.4 (
1.4 J/mol H2/K respectively. The uncertainties for the repro-
cessed data were calculated using the weighted least-squares
method explained in the Supporting Information. Given the large
∼2% difference in calculated ∆H and ∆S values by using
different EOS models, it can be seen that an accurate fugacity
is essential in determining accurate thermodynamics from a van’t
Hoff plot, especially when dealing with high measured pressures.
Reilly and Wiswall22 also calculated the decomposition ther-
modynamics of the Mg-H system as shown in Table 1. Although
they report that the enthalpy and entropy are converted to 25
°C, reprocessing their data shows that these thermodynamic
properties are in fact not converted and are valid at their
temperature range midpoint (313 °C). Reprocessing of Reilly’s
raw pressure data using fugacity (calculated using a modern
EOS) also results in different enthalpy and entropy values (∆H
) 78.8 kJ/mol H2 and ∆S ) 140.9 J/mol H2/K) than those
originally reported in Table 1.
MgH2 Samples. Four samples of MgH2 were mechanochemi-
cally synthesized according to eq 1 using various amounts of
LiCl buffer added to premilled starting reagents prior to milling.
Large quantities of LiCl buffer act to separate the synthesized
MgH2 particles, essentially restricting particle growth and
promoting nanoparticle formation. The LiCl is also essential in
forming a barrier to particle growth during thermodynamic
investigations where samples are heated up to 360 °C. Each of
the four mechanochemically synthesized samples differed
dramatically in its structural features as investigated with
transmission electron microscopy (TEM) in the synthesis
study.18 MgH2 particle and crystal sizes are provided in Table
2 for all of the samples analyzed.
∆H ∆S
-
+
(
)
feq ) e
(3)
RT
R
The determination of ∆H and ∆S from a van’t Hoff plot (ln
feq against 1/T) relies upon a straight line fit to the experimental
data. The thermodynamic parameters are only weakly temper-
ature dependent27 allowing the linear approximation to be valid
over a limited but large temperature range.28 The pressure and
fugacity can be related when the compressibility of hydrogen
is taken into account by using29
Vm
p
f
p
1
p
ln
)
-
dp
(4)
∫
(
)
( )
0
RT
where Vm is the molar volume of H2 which is calculated from
an equation of state (EOS) for hydrogen. The Hemmes equation
of state (EOS)30 and the method of McLennan and Gray31 were
used to account for the compressibility of hydrogen. The
fugacity is often assumed to be equal to pressure due to the
small deviation from the ideal gas law at low pressures.
However, for our equilibrium measurements at 360 °C the
difference between the measured pressure and the fugacity was
of a similar magnitude to the uncertainty in the measured
pressure. Consequently all measured pressures were converted
to their fugacities using eq 4 to provide higher accuracy
thermodynamic data.
The requirement of fugacity in determining thermodynamics
from a van’t Hoff plot is especially important when dealing
with higher pressure data. For example Stampfer, J. F., Jr. et
al.21 utilize the Beattie-Bridgeman EOS32 to account for the
compressibility of hydrogen and to calculate the fugacity of
hydrogen at a given pressure and temperature. Stampfer’s
The MgH2 particle size decreases from several micrometers
in size for MgH2-A to 12-20 nm for MgH2-C. Comparison of
the particle size from TEM of MgH2-C with its crystallite size
from XRD suggests that the MgH2 particles consist of a few
individual crystallites. TEM of MgH2-D was largely homoge-
neous with no obvious particle morphology. Thus only crystallite
(22) Reilly, J. J.; Wiswall, R. H. Inorg. Chem. 1968, 7, 2254–2256.
(23) Pedersen, A. S.; Kjøller, J.; Larsen, B.; Vigeholm, B. Int. J. Hydrogen
Energy 1983, 8, 205–211.
(24) Friedlmeier, G. M.; Bolcich, J. C. Int. J. Hydrogen Energy 1988, 13,
467–474.
(25) Klose, W.; Stuke, V. Int. J. Hydrogen Energy 1995, 20, 309–316.
(26) Shao, H.; Wang, Y.; Xu, H.; Li, X. Mater. Sci. Eng., B 2004, 110,
221–226.
(27) Atkins, P.; Paula, J. d. Atkins’ Physical Chemistry, 7th ed.; Oxford
University Press: New York, 2002.
(32) Holley, C. E., Jr.; Worlton, W. J.; Zeigler, R. K. Compressibility
Factors and Fugacity Coefficients Calculated from the Beattie-
Bridgeman Equation of State for Hydrogen, Nitrogen, Oxygen, Carbon
Dioxide, Ammonia, Methane and Helium; Los Alamos Scientific
Laboratory, LA-2271, 1958.
(33) Lemmon, E. W.; McLinden, M. O.; Friend, D. G. Thermophysical
Properties of Fluid Systems. In NIST Standard Reference Database
Number 69; Linstrom, P. J., Mallard, W. G., Eds.; National Institute
of Standards and Technology: Gaithersburg, MD, 2005.
(28) Ragone, R.; Colonna, G. J. Phys. Chem. 1995, 99, 13050.
(29) Marchi, C. S.; Somerday, B. P.; Robinson, S. L. Int. J. Hydrogen
Energy 2007, 32, 100–116.
(30) Hemmes, H.; Driessen, A.; Griessen, R. J. Phys. C: Solid State Phys.
1986, 19, 3571–3585.
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