ARTICLE IN PRESS
S.K. Rakshit et al. / Journal of Solid State Chemistry 181 (2008) 1402–1412
1403
1150 K for 48 h. The resultant samples were characterized by X-ray
powder diffraction (XRD) technique using DIANO XRD with Cu-Ka
radiation and graphite monochromator and found to be pure
crystalline phases of LiAl5O8(s), g-LiAlO2(s) and b-Li5AlO4(s).
Three-phase mixtures {LiAl5O8(s)+Li2CO3(s)+5Al2O3(s)}, {LiAl5
O8(s)+2Li2CO3(s)+5LiAlO2(s)} and {LiAlO2(s)+2Li2CO3(s)+Li5AlO4(s)}
for KEQMS were prepared by homogeneously mixing the
individual pre-heated compounds in stoichiometric ratios and
pelletized using a steel die and then sintered at 700 K to remove
moisture. The sintered pellets were broken into small pieces and
loaded inside the Knudsen cell.
According to the phase relations in the Li2O–Al2O3 pseudo-
binary system, phase mixtures: {2LiAl5O4(s)+5Al2O3(s)+2LiF(s)},
{5LiAlO2(s)+LiAl5O4(s)+4LiF(s)} and {Li5AlO4(s)+LiAlO2(s)+4LiF(s)}
were also prepared by homogenously mixing the pre-heated
individual powders and pelletized using a steel die at a pressure of
100 MPa and sintered at 800 K for 10 h under moisture and
hydrogen-free oxygen atmosphere. These sample pellets were
then used for solid-state galvanic cell experiments. Powder
samples of LiAl5O8(s), LiAlO2(s) and Li5AlO4(s) were used for DSC.
come into the path of the molecular flow. The shutter isolates the
Knudsen effusion cell while recording the background signal.
The detected signal (Ii+) measured using Faraday cup detector
is related to the partial pressure of the vapor species (pi) by
pi ¼ KinstIþi T=ðsiaiÞ
(1)
where Kinst is the instrumental constant, Ii+ is the measured ion
current in ampere, T is the absolute temperature near the Knudsen
cell, si is the electron impact cross-section and ai isotopic
abundance of the specific ion. Eq. (1) can be represented as
ln pi ¼ ln Kinst þ lnðIþi TÞ ꢀ ln si ꢀ ln ai
(2)
For permanent gaseous species such as CO2 at mass, m ¼ 44,
ln s ¼ ꢀ45.52 at 30 eV [14] and the isotopic abundance as 100%,
Eq. (2) can be expressed as
ln Pi ¼ ln Kinst þ lnðIþi TÞ þ 45:52 ðfor i ¼ CO2Þ
(3)
2.2.1. Calibration of KEQMS
Prior to calibration of the instrument, the background signals
were monitored by heating the Knudsen chamber with empty
Knudsen cell at different temperatures from ambient to 1161 K at
pressure level ꢁ1 ꢂ10ꢀ5 Pa. The background signals as a function
of temperature are shown in Fig. 1. It is evident from the figure
that the background signals corresponding to H+2, N2+, CO+ and CO2+
do not change appreciably with change in temperature. During
experiments, the actual signals were obtained by subtracting the
ion intensities due to background.
The instrument calibration constant (Kinst) was determined by
measuring the ion intensities of CO+2 over the phase mixtures of
{CaCO3(s)+CaO(s)}, {SrCO3(s)+SrO(s)}, {BaCO3(s)+BaO(s)} and {Li2
CO3(s)+Li2O(s)}. Three different ionization energies (30, 50 and
70 eV) were used to measure the ion intensities of CO+2 to check
the linearity of pressure measurements. However, 30 eV is
sufficient to ionize all types of gaseous molecules; hence, the
actual experiments were carried out at ionization energy of 30 eV.
Prior to actual measurement, a particular phase mixture (mass
ꢁ1 g) was loaded inside the Knudsen cell and then heated at 700 K
for 4 h under high vacuum to remove the moisture and other
unwanted gaseous species.
2.2. Knudsen effusion quadrupole mass spectrometry (KEQMS)
The Knudsen effusion mass spectrometric technique is one of
the most informative methods for vaporization processes and
thermodynamic properties of high-temperature systems. Gener-
ally, for thermodynamic measurements, traditional magnetic
sector mass spectrometer attached to Knudsen effusion system
is preferable among quadrupole and time-of-flight mass spectro-
meters. Murray et al. [9] have shown that thermodynamic data
obtained by Knudsen effusion technique using magnetic sector
spectrometer and quadrupole mass spectrometer are in good
agreement for pure chromium and chromium–silicon samples.
However, quadrupole mass spectrometer has no significant
advantages over magnetic mass spectrometer but they are very
compact and relatively inexpensive. Stolyarova et al. [10] have
reported that quadrupole mass spectrometer coupled to Knudsen
cell can effectively be used for thermodynamic studies at high
temperature.
In this study, a residual gas analyzer (RGA) coupled to Knudsen
effusion system was used for equilibrium partial pressure
measurements. An RGA is a quadrupole mass spectrometer in
which the ionizer is immersed in the gas to be analyzed, and the
ionizer is characterized by an open construction in which the gas
may enter and leave in all directions. It is assumed that the gas is
homogenous and that changes in the gas density with time occur
slowly enough such that the instrument is always in equilibrium
with the gas. This instrument can be used to identify the kind of
molecules present in the gaseous phase and, when calibrated, can
be used to determine concentrations or partial pressures [11–13]
of individual species.
The KEQMS used in this study is an in-house designed Knudsen
vacuum chamber and arranged in such a way that it allows
reciprocally perpendicular molecular beam from the Knudsen
effusion cell. The Knudsen vacuum chamber was heated to the
desired temperature using resistance heater. The temperature
near the Knudsen cell was measured using a pre-calibrated (ITS-
90) chromel–alumel thermocouple. The Knudsen cell used was
made of 15 mol% calcia stabilized zirconia (CSZ) with a thin
cylindrical orifice of dia 0.8 mm and height 0.2 mm at the centre of
the lid. This setup is used only for partial pressures measurements
of permanent gaseous species such as CO, O2, N2, CO2, etc. and not
for condensable vapor species. A shutter is placed between the
ionizer and the Knudsen effusion chamber such that it does not
2.2.2. Partial pressure measurements of CO2(g) over equilibrium
phase mixtures
Huang et al. [15] have reported the thermodynamic data of
Na4Fe6O11(s) by measuring the partial pressure of CO2(g) over
{2Na2CO3(s)+3Fe2O3(s)} phase mixture using Knudsen effusion
mass spectrometry from 918 to 1013 K. Similar approach was
adopted in this study to determine the Gibbs energies of
formation of LiAl5O8(s), LiAlO2(s) and Li5AlO4(s) by measuring
the partial pressure of CO2(g) over the equilibrium phase mixtures
{LiAl5O8(s)+Li2CO3(s)+5Al2O3(s)}, {LiAl5O8(s)+2Li2CO3(s)+5LiAlO2(s)}
and {LiAlO2(s)+2Li2CO3(s)+Li5AlO4(s)}.
The ion intensities of CO2+ over these equilibrium phase
mixtures were measured using KEQMS. For each measurement,
two sets of experiments were carried out and the ion intensities
for other gaseous species were in background level during the
measurement. Subsequently, partial pressures of carbon dioxide,
p(CO2) over the phase mixture were obtained using Eq. (3). After
the mass spectrometric measurements, the resultant phase
mixtures were analyzed by XRD technique and found to be the
mixture of corresponding lithium aluminate, lithium carbonate
and alumina. Therefore, it was assumed that the following
equilibrium reactions were established inside the Knudsen cell
under experimental conditions:
Li2CO3ðsÞ þ 5Al2O3ðsÞ ¼ 2LiAl5O8ðsÞ þ CO2ðgÞ
(4)