Journal of the American Chemical Society
Communication
observed15−18 and/or represents only a minority product.22
This can be understood upon closer inspection. From Figure
1a, D2 desorption peaks at ∼400 K. For alcohols, the
desorption from Ti5c sites is usually maximized between 280
and 350 K,29 at least 50 K lower than the temperature of
hydrogen formation. This means that at the temperature of
hydrogen formation, most of the alcohol molecules have
already desorbed, and only alkoxy species formed by alcohol
dissociation on VO sites are present. As such, the probability of
having two neighboring Ti5c-bound alcohol molecules at
temperatures required for H2 formation is negligible. In
contrast, the glycol molecules with two hydroxyl groups bind
more strongly with TiO2(110) and hence desorb at a much
higher temperature than alcohols (see Figure S3 in SI). More
importantly, the fraction of glycols that desorb intact is small
(∼20% for EG) as the majority is being converted to
products.23 Therefore, there is sufficient coverage of glycols
on TiO2(110) at ∼400 K for the formation of two neighboring
glycol species and D2.
In summary, we have shown that molecular hydrogen
formation from glycols on TiO2(110) is dictated by many
factors, that include glycol coverage, steric constraints of glycol
molecules, surface order, and the charge state of TiO2(110).
Hydrogen formation is only observed at high glycol coverages.
Increasing the steric hindrance of glycols is found to inhibit and
eventually eliminate hydrogen formation. Damaging the surface
order or scavenging the available surface charge of TiO2(110)
are also shown to completely suppress hydrogen formation.
These findings provide strong evidence that hydrogen
formation results from the bimolecular reaction between two
hydroxyl groups of neighboring Ti5c-bound glycols, and that the
redox reaction is driven by defect electrons of TiO2(110).
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Notes
The authors declare no competing financial interest.
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We thank R. Rousseau and N. G. Petrik for numerous
stimulating discussions. This work was supported by the U.S.
Department of Energy, Office of Basic Energy Sciences,
Division of Chemical Sciences, Geosciences & Biosciences,
and performed in EMSL, a national scientific user facility
sponsored by the Department of Energy’s Office of Biological
and Environmental Research and located at Pacific Northwest
National Laboratory (PNNL). PNNL is a multiprogram
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