“…1,2 Iron pyrite (FeS 2 ) is a promising photovoltaic material because of its suitable band gap (E g = 0.95 eV), strong light absorption (α > 10 5 cm -1 for hν > 1.4 eV), long minority carrier diffusion length (100-1000 nm), and essentially infinite elemental abundance. 3,4,5,6,7,8 Pyrite photoelectrochemical and solid-state Schottky solar cells have shown large short-circuit current densities (30-42 mA cm -2 ) and quantum efficiencies as high as 90%. 9,10 The main obstacle for the development of pyrite is its low open-circuit photovoltage (V OC ), which is typically only < 200 mV.8 Since 1984, a few dozen studies have explored possible causes of the low V OC , such as bulk nonstoichiometry (mostly S or Fe vacancies), 8,11,12,13 surface states that cause Fermi pinning and thermionic-field emission, and large dark currents, 14,15,16 metallic FeS-like surface layers, 17,18 and small-band gap phase impurities in the pyrite bulk (including marcasite, pyrrhotite, and amorphous iron sulfide phases).…”