Electronically Driven Distortions in Li Intercalates
A R T I C L E S
filled recirculating drybox with a combined O2 and H2O content of
less than 5 ppm. Orange Y2Ti2O5S2 and brown Nd2Ti2O5S2 were
prepared on the 2-10 g scale by reacting stoichiometric quantities of
Y2O3 or Nd2O3, TiO2, and TiS2 at 1100 °C in sealed silica tubes. The
lanthanide oxides (Y2O3: Aldrich 99.99%; Nd2O3: ALFA 99.99%)
were dried at 900 °C for 24 h in air and then removed to the drybox,
TiO2 (Aldrich 99.9+%) was dried at 250 °C in air, and TiS2 was
prepared by reacting Ti (ALFA 99.99%, dehydrided) with S (ALFA
99.9995%) at 600 °C for 3-4 days in evacuated silica tubes.
(Caution: the temperature was raised from 400 to 600 °C over 24 h to
avoid a buildup of sulfur pressure.) The starting materials were ground
together thoroughly and loaded into silica tubes which had been baked
at 900 °C under a vacuum of 2 × 10-2 mbar for several hours to remove
adsorbed moisture. This prebaking step was important to avoid
contamination of the oxysulfides with Ln2Ti2O7 phases (especially in
the case of Y2Ti2O5S2). The tubes were sealed under a vacuum of 2 ×
10-2 mbar, and the brown or orange oxysulfides were obtained phase
pure according to laboratory powder X-ray diffraction by heating the
tubes at 1100 °C for 3-4 days. Lithium intercalation was carried out
in three different ways using either lithium vapor or reducing solutions
containing the Li+ ion. First, 2-5 g of the oxysulfide powders were
reacted with excess n-BuLi (Aldrich, 2.5 M in hexane; Li/Ti ratios of
between 7:1 and 10:1) at between 20 and 50 °C for 1-60 days under
a nitrogen atmosphere. The samples were filtered and washed three
times with distillation-dried hexane and then dried under vacuum prior
to storage in the drybox. In the second low-temperature approach,
applied to Y2Ti2O5S2, excess lithium (Li/Ti ratios of between 1:1 and
10:1) was dissolved in 30-50 cm3 of liquid ammonia (BOC 99.98%
and dried over sodium) in one arm of a glass “H”-cell30 (designed to
withstand an internal pressure of up to 15 atm) and poured onto 0.5-3
g of Y2Ti2O5S2 located in the other arm. The solution was stirred
overnight at -78 °C after which the powder had changed in color from
orange to black. The unreacted metal-ammonia solution was separated
from the solid by means of a porous glass filter separating the two
arms of the “H”-cell, and the solid was washed by condensing the
ammonia back onto the solid and repeating the filtration step until the
liquid in contact with the solid product was colorless. The ammonia
was then removed to another vessel, and the “H”-cell was evacuated
to 2 × 10-2 mbar and removed to the drybox prior to extraction of the
solid product. In some cases, this treatment was then repeated with
fresh Li/NH3 solution for several periods of 24 h. If temperatures around
0 °C (Caution: the glassware must be designed to withstand the vapor
pressure of ammonia and the pressure of any evolved H2) were used
for the intercalation using Li/NH3, the LixY2Ti2O5S2 material formed
in the reaction was found to catalyze the decomposition of the solution
to LiNH2 and H2 over a period of a few hours (indeed, decomposition
of alkaline earth/ammonia solutions was rapid even at -78 °C, and
this route cannot be used for intercalation of the alkaline earths). These
samples prepared using “chimie douce” approaches were used for
neutron powder diffraction investigations and are summarized in Table
1. Alternatively, lithium vapor was used as the reducing agent: up to
2 g of the oxysulfide powders were placed in nickel tubes (Ni 222
alloy, 99.9% pure, 10 cm long, 9-mm inner diameter, 0.5-mm wall
thickness, and sealed at one end) and a smaller stainless steel tube (5-
mm inner diameter, open at one end) containing some lithium pieces
(Li/Ti ratios of between 2:1 and 10:1) was placed on top of the powder.
This assembly was used so that the oxysulfide powder was in contact
only with lithium vapor and not the liquid. The nickel tube was sealed
by arc-welding under argon (purified using a Ti getter at 800 °C), and
the whole was sealed in an evacuated silica jacket to avoid oxidation
of the nickel at elevated temperatures. These tubes were placed upright
in a muffle furnace and heated at 400-700 °C for periods of 1-6
weeks.
Ln2Ti2O5S2 (Ln ) Pr - Er, Y). These compounds resemble
the n ) 2 R-P phases, but the 12-coordinate site in the
perovskite-like slabs is vacant, and the ordering between oxide
and sulfide results in the oxide ions being confined to the
perovskite slabs, while the sulfide ions occupy the rock salt
layers. These compounds contain a reducible transition-metal
cation, and their structural features resemble those of the ReO3
structure as well as those of layered transition-metal sulfides,
both of which will accept reducing intercalants. We have
recently demonstrated21 that sodium may be inserted either into
the 12-coordinate site in the perovskite-like oxide slab (under
thermodynamic control), producing R-NaxY2Ti2O5S2 (0 < x e
1), or into a tetrahedral site in the sulfide layer (under kinetic
control), producing â-NaY2Ti2O5S2 (with no apparent range of
compositions), which is to our knowledge the first example of
reductive intercalation into the rock salt layers of a Ruddlesden-
Popper-type phase. The two phases of formula NaY2Ti2O5S2
(Ti oxidation state of +3.5) are both black with dominant Pauli
paramagnetism, and detailed investigations of the R-NaxY2-
Ti2O5S2 (0 e x e 1.0) intercalates22 and the intercalates with
alkali metals inserted into the sulfide layers23 are reported
elsewhere. Here we describe the effect on the crystal structures
of the insertion of variable amounts of lithium into the vacant
sites in the oxide slabs of Y2Ti2O5S2. Some initial measurements
on lithium intercalates of Nd2Ti2O5S2 are reported, but the
yttrium system is reported in detail as this is the only member19
for which measurements of magnetic properties are not com-
plicated by the presence of a paramagnetic lanthanide ion. The
smaller size of lithium means that, unlike in the sodium case,
there is no kinetic barrier to insertion into the perovskite blocks
even well below room temperature, and this is always favored
over insertion into the rock salt-type sulfide layers. Furthermore,
the lithium ion is accommodated in a different site in the oxide
layers to that occupied by the sodium ion in the analogous
sodium intercalates,21 and lithium intercalates LixLn2Ti2O5S2 for
0 < x e 1.85(5) (i.e., approaching full occupancy of the lithium
sites (x ) 2) and with Ti oxidation states approaching +3) are
chemically accessible. The details of the structures of these
intercalates are strongly dependent on electron count. This work
is complementary to the many investigations of reduced titanium
oxides including Ti2O3,24 LnTiO3 (Ln ) Ce - Lu, Y),25
La1-xSrxTiO3,26 NaTiO2,27 and the superconducting spinel
LiTi2O4,28,29 which show the interplay between crystal structure,
electronic structure, and temperature for reduced titanate systems
in the proximity of the metal-insulator boundary.
Experimental Section
Synthesis. The Li intercalates are all extremely air-sensitive and
oxidize in a matter of seconds when exposed to air. All manipulations
of solids were therefore carried out in a Glovebox Technology argon-
(21) Denis, S. G.; Clarke, S. J. Chem. Commun. 2001, 2356.
(22) Clarke, S. J.; Denis, S. G.; Rutt, O. J.; Hill, T. L.; Hayward, M. A.; Hyett,
G.; Ga´l, Z. A. Chem. Mater. 2003, 15, 5065.
(23) Rutt, O. J.; Hill, T. L.; Ga´l, Z. A.; Hayward, M. A.; Clarke, S. J. Inorg.
Chem. 2003, 42, 7906.
(24) Mott, N. F. J. Phys. 1981, 42, 277.
(25) Greedan, J. E. J. Less-Common Met. 1985, 14, 335.
(26) Hays, C. C.; Zhou, J.-S.; Markert, J. T.; Goodenough, J. B. Phys. ReV. B
1999, 60, 10367.
(27) Clarke, S. J.; Fowkes, A. J.; Harrison, A.; Ibberson, R. M.; Rosseinsky,
M. J. Chem. Mater. 1998, 10, 372.
(28) Johnston, D. C.; Prakash, H.; Zachariasen, W. H.; Viswanathan, R. Mater.
Res. Bull. 1973, 8, 777.
(29) Harrison, M. R.; Edwards, P. P.; Goodenough, J. B. Philos. Mag. B 1985,
52, 679.
(30) Wayda, A. L.; Dye, J. L. J. Chem. Educ. 1985, 62, 356.
9
J. AM. CHEM. SOC. VOL. 126, NO. 7, 2004 1981