James P S Walsh1, Samantha M Clarke1, Yue Meng2, Steven D Jacobsen3, Danna E Freedman1. 1. Department of Chemistry, Northwestern University , Evanston, Illinois 60208, United States. 2. HPCAT, Geophysical Laboratory, Carnegie Institution of Washington , Argonne, Illinois 60439, United States. 3. Department of Earth and Planetary Sciences, Northwestern University , Evanston, Illinois 60208, United States.
Abstract
Recent advances in high-pressure techniques offer chemists access to vast regions of uncharted synthetic phase space, expanding our experimental reach to pressures comparable to the core of the Earth. These newfound capabilities enable us to revisit simple binary systems in search of compounds that for decades have remained elusive. The most tantalizing of these targets are systems in which the two elements in question do not interact even as molten liquids-so-called immiscible systems. As a prominent example, immiscibility between iron and bismuth is so severe that no material containing Fe-Bi bonds is known to exist. The elusiveness of Fe-Bi bonds has a myriad of consequences; crucially, it precludes completing the iron pnictide superconductor series. Herein we report the first iron-bismuth binary compound, FeBi2, featuring the first Fe-Bi bond in the solid state. We employed geologically relevant pressures, similar to the core of Mars, to access FeBi2, which we synthesized at 30 GPa and 1500 K. The compound crystallizes in the Al2Cu structure type (space group I4/mcm) with a = 6.3121(3) Å and c = 5.4211(4) Å. The new binary intermetallic phase persists from its formation pressure of 30 GPa down to 3 GPa. The existence of this phase at low pressures suggests that it might be quenchable to ambient pressure at low temperatures. These results offer a pathway toward the realization of new exotic materials.
Recent advances in high-pressure techniques offer chemists access to vast regions of uncharted synthetic phase space, expanding our experimental reach to pressures comparable to the core of the Earth. These newfound capabilities enable us to revisit simple binary systems in search of compounds that for decades have remained elusive. The most tantalizing of these targets are systems in which the two elements in question do not interact even as molten liquids-so-called immiscible systems. As a prominent example, immiscibility between iron and bismuth is so severe that no material containing Fe-Bi bonds is known to exist. The elusiveness of Fe-Bi bonds has a myriad of consequences; crucially, it precludes completing the iron pnictide superconductor series. Herein we report the first iron-bismuthbinary compound, FeBi2, featuring the first Fe-Bi bond in the solid state. We employed geologically relevant pressures, similar to the core of Mars, to access FeBi2, which we synthesized at 30 GPa and 1500 K. The compound crystallizes in the Al2Cu structure type (space group I4/mcm) with a = 6.3121(3) Å and c = 5.4211(4) Å. The new binary intermetallic phase persists from its formation pressure of 30 GPa down to 3 GPa. The existence of this phase at low pressures suggests that it might be quenchable to ambient pressure at low temperatures. These results offer a pathway toward the realization of new exotic materials.
Creating and understanding
new bonding interactions is central
to chemistry; each new bond gives rise to undiscovered electronic
structure and provides novel insight into chemical bonding in materials.
Thousands of unique chemical interactions are known, and yet within
the periodic table there remain bonds that are counterintuitively
absent. This is particularly enigmatic when the two elements in question
exhibit a diverse chemistry with other elements across the periodic
table. For chemists, such systems represent unexplored regions of
phase space with tremendous potential for discovery; iron–bismuth
is a prominent example of such a system. Indeed, the immiscibility
of the elements is so severe that there have been no reports of Fe–Bi
bonds in the solid-state literature. This is particularly intriguing
from a chemical standpoint because there are numerous applications
that would benefit from the creation of this interaction, notably
magnetism and superconductivity.Our interest in the intersection
of iron and bismutharises from
the potential for transformative magnetic properties. By fusing the
paramagnetism of iron with the spin–orbit coupling inherent
to bismuth, we envision the creation of a new family of magnetic materials.
Creating an iron–bismuth bonding interaction is also of urgent
interest to the superconductivity community, where iron–bismuth
interactions are a prerequisite to create the missing members of the
iron pnictide family of superconductors.[1] Creating new bismuth superconductors could provide crucial insight
into the mechanism of these exotic iron-based materials. Despite over
a decade of focused interest within this area, iron–bismuth
bonds remain elusive within solid-state materials.One key challenge
in creating an iron–bismuth interaction
is the immiscibility of the two elements. Even at the elevated temperature
of 1873 K, where both metals are in the liquid state, the solubility
of bismuth in iron is only 0.16 wt %.[2] This
suggests that extreme conditions may be required to access a binary
compound. Toward that end, we considered the application of geologically
relevant pressures. Bismuth is unusually well-suited to high-pressure
synthesis due to its numerous high-pressure phases and associated
structural transformations.[3,4] Indeed, recently, high
pressure was employed as a vector to access new binary compounds in
bismuth systems that were previously devoid of intermetallic phases,
including CoBi3[5] and Cu11Bi7.[6] Both of these compounds are the first structurally characterized
intermetallic phases in their respective binary systems,[7,8] and both were synthesized by reaction of the elements at high-pressure
conditions (4–6 GPa) using a large volume press (LVP). We hypothesized
during our research on the Cu11Bi7 system that
the mutual solubility of the Cu and Bi enabled its facile synthesis
at relatively low pressures.Given the immiscibility of elemental
iron and bismuth, even in
the molten state (Figure S1),[9] we postulated that we would require access to
a significantly higher pressure regime in order to create the first
iron–bismuthbinary compound. Toward that end, we employed
a diamond anvil cell (DAC), which permits in situ structural and physical characterization over a much wider range
of pressure–temperature space than can be achieved in the LVP.
Indeed, DACs are capable of pressures well beyond 250 GPa, which is
over an order of magnitude higher than the maximum pressures achievable
in LVP reactions. To contextualize this increase in pressure, while
our previous synthesis of Cu11Bi7 was performed
at pressures comparable to the core of the Moon (∼6 GPa), these
experiments at ∼30 GPa are performed at pressures comparable
to the core of Mars.[10]Herein we
report the synthesis of the first iron–bismuthbinary compound, FeBi2 (Figure ), via pressurization in a DAC at 30 GPa
and laser-heating to 1500 K. Decompression studies demonstrate that
the material retains the Al2Cu structure type down to at
least 2.9(1) GPa, suggesting that it might be possible to quench the
phase to ambient pressures at low temperatures.
Figure 1
Crystal structure of
FeBi2 determined at 29.9(1) GPa.
Purple and orange spheres represent Bi and Fe, respectively. (a) View
of two face-sharing {FeBi8} square antiprisms stacking
along the c-direction. (b) View down the c-axis showing the edge-sharing linkages formed between
the stacked columns.
Crystal structure of
FeBi2 determined at 29.9(1) GPa.
Purple and orange spheres represent Bi and Fe, respectively. (a) View
of two face-sharing {FeBi8} square antiprisms stacking
along the c-direction. (b) View down the c-axis showing the edge-sharing linkages formed between
the stacked columns.
Results and Discussion
We targeted the synthesis of a novel
iron–bismuthbinary
at pressures between 12–40 GPa using a DAC (see Supporting Information for full details). We
performed reactions within this pressure range to ensure that iron
would be present as ε-Fe (hcp), the high-pressure
phase of Fe, since our prior reactions at lower pressures—where
iron is in the α-Fe (bcc) phase—were
unsuccessful. The experiment was monitored by continuous in
situ powder X-ray diffraction (PXRD) during laser heating
of an iron and bismuth mixture inside a DAC, which allows for the
real-time visualization of phase formation as the reaction takes place.
This remarkable capability facilitates the exploration of pressure–temperature
phase space for a given composition, and also aids in the optimization
of the experimental procedure. We employed MgOas a thermal insulator
between the sample and the diamond anvils during the laser heating,
and also as a pressure-transmitting medium. Fortuitously, its well-defined
equation of state also enabled its use as a precise pressure calibrant
at the reaction site.[11]We heated
pressurized samples of elemental iron and bismuth using
a microfocused infrared laser (fwhm = 40–80 μm) while
performing in situ PXRD at beamline 16-ID-B, HPCAT,
Advanced Photon Source (APS). Between 12 and 30 GPa, we did not observe
the formation of any novel phases during heating, even up to 2000
K. However, at pressures above 30 GPa, and upon heating to approximately
1500 K, peaks belonging to a new phase began to appear in the diffraction
pattern. These peaks grew in intensity for about 4 min, at which point
no further changes were observed. We then switched off the laser heating
to thermally quench the reaction. The reaction can be reproduced successfully
by pressurizing iron and bismuth in the range of 30–35 GPa
and heating at or above ca. 1500 K (see the Supporting Information for details).Examination of the diffraction
patterns acquired at high pressure
reveals four phases: MgO (fcc), Bi(V) (bcc), ε-Fe (hcp), and a new phase. The observation
of a high quality MgO diffraction pattern enables us to employ it
as a pressure calibrant by studying the change in lattice parameters
at pressure. By placing the compressed MgO lattice parameters into
its well-described equation of state, we can determine that the initial
pressure before heating was 32.2(1) GPa, and fell to 29.9(1) GPa after
thermal quenching.The in situ PXRD experiments
at the synchrotron
source offered sufficient resolution to enable the simultaneous modeling
of all four phases using the TOPAS software package (Figure ).[12] The gradual appearance of the new phase over a 4 min time window
enabled us to easily isolate and index its associated peaks. The relatively
small number of peaks in the diffraction pattern was indicative of
a high symmetry crystal system, which we indexed to the tetragonal
space group, I4/mcm. A search of known binary structure types with this
space group yielded the Al2Cu structure type, in which
several ironbinary compounds crystallize.[13−15] The new phase
was well modeled with Rietveld refinement asFeBi2 in the
Al2Cu structure type, with lattice parameters of a = 6.3121(3) Å and c = 5.4211(4)
Å (at 29.9(1) GPa). The early transition
metal–antimonides, TiSb2[16] and VSb2,[17,18] crystallize within the same Al2Cu structure type at ambient pressures, while CrSb2 and FeSb2 undergo a pressure-induced transition from
the marcasite FeS2 structure type into the Al2Cu structure type at pressures of 5.5 GPa[19] and 14.3 GPa,[13] respectively. FeBi2 can therefore be considered as a structural analogue of the
high-pressure phase of FeSb2.
Figure 2
Background-subtracted
X-ray diffraction pattern of the reaction
site after cooling to room temperature (λ = 0.406626 Å, P = 29.9(1) GPa). The experimental trace is plotted in blue,
with asterisks denoting the peaks arising from MgO (green), unreacted
Bi(V) (purple), and unreacted ε-Fe (orange). The simulated pattern
of FeBi2 based on the final fit parameters is plotted in
pink.
Background-subtracted
X-ray diffraction pattern of the reaction
site after cooling to room temperature (λ = 0.406626 Å, P = 29.9(1) GPa). The experimental trace is plotted in blue,
with asterisks denoting the peaks arising from MgO (green), unreacted
Bi(V) (purple), and unreacted ε-Fe (orange). The simulated pattern
of FeBi2 based on the final fit parameters is plotted in
pink.The structure of FeBi2 is composed of iron atoms coordinated
by eight bismuth atoms to form square antiprisms with the C4 axes parallel to the unit cell c-axis (Figure a).
The square faces are not perfectly staggered, with an angle of 37.5(1)°
between them. This structure is reminiscent of the recently isolated
ternary cluster anion [Ni2Sn7Bi5]3–, which features a 12-atom Sn/Bi cage surrounding
two nickel atoms.[20] In FeBi2, the {FeBi8} square antiprisms share both of their square
faces with adjacent antiprisms to form columns along the c-direction (Figure a), and these columns share edges with neighboring columns throughout
the ab-plane (Figure b). At 30 GPa, the eight Fe–Bi interactions
around each iron atom are equivalent by symmetry, with interatomic
distances of 2.719(2) Å. For comparison, molecularFe–Bi
bonds are known to exist in iron carbonyl species, where they possess
lengths up to 2.85 Å.[21−23] The sum of the covalent radii
of iron and bismuth is 1.25 Å (rFe) + 1.46 Å (rBi) = 2.71 Å,[24] which compares very well with the value obtained
for Fe–Bi in FeBi2 at the formation pressure. We
should note that covalent radii may underestimate bond lengths in
intermetallic compounds, due to the increased electron delocalization
across the structure coupled with the larger number of interactions
common in intermetallic compounds, as compared with the highly directional
interactions found in molecules. However, these numbers are still
useful as a first approximation of bonding distances in intermetallic
compounds. The shortest Fe–Fe distances in FeBi2are those along the c-axis, 2.7107(3) Å, which
is longer than the Fe–Fe distance found in high-pressure FeSb2 (2.536 Å at 28.2 GPa),[13] but
shorter than those featured in the Al2Cu-type compound
FeZr2, 2.798(2) Å.[15]There are three unique Bi–Bi interactions within each antiprism:
one that forms the edges of the square faces, 3.333(2) Å, and
two that form the sides of the triangular faces that connect the upper
and lower square faces in each prism, 3.106(3) Å and 3.419(3)
Å. An even shorter Bi–Bi interaction exists between bismuth
atoms on adjacent antiprism columns (Figure ), with a distance of 2.948(5) Å. The
large range of distances for the Bi–Bi bonds led us to further
examine the nature of these interactions. The shortest Bi–Bi
distance of 2.948(5) Å is quite short for a Bi–Bi bond,
indicating that the interaction is higher order than that of a single
Bi–Bi bond. Although high pressure may contribute to the bond
contraction, it is worthwhile to note that the single Bi–Bi
bond in elemental Bi(V) at 30 GPa is significantly longer (3.1044(3)
Å) than the distance seen here. Indeed, the short Bi–Bi
bond in FeBi2 is reminiscent of the Bi2 dimer
found in the alkali metal–bismuthidebinaries, such asCs3Bi2, 2.976(2) Å, and K3Bi2, 3.014 Å,[25] and in the transition
metal–bismuth intermetallic compounds, PtBi2[26] and RhBi2.[27] Within these compounds, a Bi22– species,
with an extra electron delocalized within the structure, is commonly
invoked to understand the electronic structure. The frequently observed
Bi–Bi structural motif suggests that this proximal interaction
may be important in the formation of this structure. Indeed, there
are a number of molecular species featuring a similarly short Bi–Bi
bond,[28−33] indicating that this may be a crucial stabilizing factor. As the
pressure is released, this Bi–Bi bond distance elongates to
3.2270(4) Å at 3 GPa, indicating that the stabilizing influence
of this dinuclear interaction has diminished (Figure ).
Figure 3
View down the c-axis at 3 GPa
(a) and 30 GPa (b),
illustrating the effect of increased pressure on the Fe–Bi
interaction and the intercolumn Bi–Bi interaction. Purple and
orange spheres represent Bi and Fe atoms, respectively.
View down the c-axis at 3 GPa
(a) and 30 GPa (b),
illustrating the effect of increased pressure on the Fe–Bi
interaction and the intercolumn Bi–Bi interaction. Purple and
orange spheres represent Bi and Fe atoms, respectively.Compounds displaying long-term stability under
ambient conditions
after high-pressure synthesis are referred to as quenchable. In order
to assess whether the structure could be quenched to ambient pressures,
we incrementally decompressed a sample of FeBi2. Rietveld
refinement of PXRD patterns collected after each decompression step
shows a smooth change in the unit cell parameters of FeBi2as the pressure is released (Figure ). Peaks belonging to the FeBi2 phase were
evident down to 2.9(1) GPa, but were no longer present upon the final
decompression to 0.5(1) GPa, indicating that the compound either decomposed
or lost crystallinity.
Figure 4
Experimental pressure dependence of the normalized unit
cell parameters
upon decompression of FeBi2. Dashed lines are fits of the
experimental data using the third-order Birch–Murnaghan isothermal
equation of state, as described in the Supporting Information.
Experimental pressure dependence of the normalized unit
cell parameters
upon decompression of FeBi2. Dashed lines are fits of the
experimental data using the third-order Birch–Murnaghan isothermal
equation of state, as described in the Supporting Information.Completing the iron pnictide
series of compounds enables us to
gain insight into the structural properties of these materials. First-principles
calculations carried out on the known Al2Cu structure type
iron pnictides, FeP2, FeAs2, and FeSb2, suggest a decrease in compressibility as the reference volume (V0) increases.[34] Specifically,
there is an inverse linear relationship between V0 (145.2 Å3, 177.4 Å3,
and 237.0 Å3, respectively) and the bulk modulus, B0 (153, 109, and 68 GPa, respectively), for
this family of compounds. In order to evaluate the compressibility
of FeBi2, we fit the evolution of the FeBi2 lattice
parameters (Table S6) as a function of
pressure with a third-order Birch–Murnaghan isothermal equation
of state (BM3) using the software package EosFit-7c.[35]For FeBi2, we obtain V0 =
273(3) Å3, B0 = 99(5)
GPa, and B0′ = 2.7(2). Using a second-order fit
(B0′ = 4 implied), we obtain V0 = 278(1) Å3 and B0 =
75(2) GPa. If we compare the BM3 values to those reported for FeSb2, which is a close structural analogue to FeBi2, we find that FeBi2 is roughly 45% more incompressible
than FeSb2. If the trend of increasing compressibility
were to continue upon moving down the iron pnictide series, then V0 = 273(3) Å3 would lead to
an expected value of B0 ≃ 49 GPa
for FeBi2. Since we actually observe a decreased compressibility
in FeBi2 compared to FeSb2, this trend does
not appear to extend to the bismuthides. We hypothesize that this
unexpected result could stem from the increased importance of relativistic
effects in bismuth,[36] which are known to
cause discontinuities in chemical trends going down the pnictogen
series. The potential for anomalous behavior arising from relativistic
effects provides further motivation for the creation and investigation
of new bismuth-based intermetallic compounds.The extrapolated
zero-pressure unit cell lengths obtained from
the axial compressibility plots are a0 = 6.98(2) Å and c0 = 5.666(4) Å.
We can use these values to estimate the structural parameters under
ambient conditions, which then allows us to compare structural parameters
with other reported solid-state structures. One parameter that we
are particularly interested in is the Fe–Bi distance. Fe–Bi
bonds are, to the best of our knowledge, completely absent from solid-state
materials. The extrapolated zero-pressure Fe–Bi distance in
FeBi2 is 2.96 Å. At the elevated pressure of 29.9(1)
GPa, the Fe–Bi bond distance in FeBi2 is 2.719(2)
Å.Based on the structural metrics and examination of the
pnictide
literature, we hypothesize that two driving forces behind the formation
of the phase are the pressure-induced stabilization of the Fe–Bi
bond and the intercolumn Bi–Bi bonding interaction (Figure ). The numerous examples
of compounds featuring Bi–Bi bonds across the solid-state and
molecular literature bolster our supposition that creating stronger
bonding interactions between pairs of bismuth atoms is a stabilizing
factor. Indeed, this may serve as a design principle for the synthesis
of additional bismuth based phases. As the pressure is decreased,
the stabilizing influence of these bonds is expected to diminish until
eventually phase separation (decomposition) becomes the thermodynamically
favored process. Therefore, one possible explanation for the loss
of the diffraction pattern of the compound below 2.9(1) GPa at room
temperature is that, at this pressure, ambient temperature provides
sufficient thermal energy to enable decomposition of the metastable
phase. Future work will explore the quenchability of this phase at
low temperatures, and with slow gas membrane decompression, since
the rate of pressure release is known to be an important factor in
quenching metastable phases.[37−39]
Conclusions
We
synthesized the first compound in the iron–bismuth system,
which also features the first Fe–Bi bond in the solid state.
This compound persists down to at least 2.9(1) GPa, offering the potential
for future quenchability. Ongoing work is focused on the scale-up
of this reaction with a unique, highly specialized press capable of
reaching the required pressures in order to enable studies of the
electronic properties of this fascinating new material.The
results reported here ignite promise for new discoveries within
the iron pnictide systems, and demonstrate the value of high pressure
as a viable route toward new intermetallic compounds, and indeed toward
creating new bonds in the solid state. In particular, the stabilizing
effect of the Bi–Bi interaction within this compound offers
significant promise for the high-pressure synthesis of iron–bismuth
superconductors within the ThCr2Si2 structure
type. Simple visual inspection of the Bi–Bi distances in the
known BaMn2Bi2 structure hints that high pressure
could be an appropriate vector to synthesize the iron analogue. Future
work will focus on completing the series of pnictide superconductors
via high-pressure synthesis.
Authors: Samantha M Clarke; James P S Walsh; Maximilian Amsler; Christos D Malliakas; Tony Yu; Stefan Goedecker; Yanbin Wang; Chris Wolverton; Danna E Freedman Journal: Angew Chem Int Ed Engl Date: 2016-09-26 Impact factor: 15.336