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.