Light-induced electron transfer between chromophoric
organic matter
and Fe(III)-oxides lies at the heart of aqueous Fe(II) fluxes in the
photic zone of natural systems. Understanding this photoreductive
dissolution process is also essential for developing water purification
techniques based on this class of materials. Previously, optical transient
absorption spectroscopy (TAS) measurements revealed that nanosecond
relaxation times of photoexcited rhodamine B (RhB) dye increased when
sorbed onto hematite nanoparticles (HNPs), consistent with electron
transfer to the oxide. In the present study, we exploit time-resolved
X-ray absorption spectroscopy (XAS) at the Fe K-edge to follow the
Fe oxidation state for this same process to (i) confirm that RhB photoexcitation
leads to interfacial electron transfer and Fe reduction and (ii) quantify
the lifetime of injected electrons as a function of solution conditions.
Regardless of RhB dye availability and pH, direct band gap photoexcitation
of HNPs yields an Fe(II)-like small polaronic absorption signature
with a lifetime of ∼1 ns, an order of magnitude longer than
previously reported. However, when RhB is present at low pH under
conditions where dye favorably interacts with the positively charged
hematite surface, a second relaxation process approaching microsecond
time scales is observed that likely represents back-reaction with
the photoexcited adsorbed dye. At pH above neutral, the efficiency
of the interfacial electron transfer is diminished by a weaker interaction
between sorbed dye and particle surfaces.