A mechanistic
study was conducted on the catalytic conversion of
ethanol over La0.7Sr0.3MnO3–x
perovskite catalysts in the presence and absence
of water. The study sought insights into the path of C–C coupling
toward acetone and crotonaldehyde and also into clarifying whether
the lack of previous reports of C–C coupling over La0.7Sr0.3MnO3–x
(100) could
be due to a “pressure gap”. Several types of experiments
were performed at 400–800 K: flow experiments with a torr range
reactant gas flown over La0.7Sr0.3MnO3–x
powders; ultra-high vacuum experiments with continuous
gas exposures to a La0.7Sr0.3MnO3–x
(100) single-crystal sample; and torr range continuous
gas exposures to a La0.7Sr0.3MnO3–x
(100) single-crystal sample. When ethanol and water
were flown over La0.7Sr0.3MnO3–x
powders at 400–800 K, the products detected
were ethene, acetaldehyde, acetone, crotonaldehyde, CO, CO2, and H2. Acetone was catalytically produced over both
the La0.7Sr0.3MnO3–x
powder and the La0.7Sr0.3MnO3–x
(100) single-crystal sample at temperatures of 700–800
K when reaction conditions were on the order of 1 Torr of reactant
gas and with an excess of water relative to ethanol (1 ethanol/9 water).
Isotopic labeling with deuterium was used to gain insights into the
C–C coupling reaction mechanism and paths in species with three
and four carbons (C3 and C4 species). Additionally, steady-state isotopic
transient kinetic analysis (SSITKA) experiments + simulations using
carbon labeling of the ethanol feed were performed. Three mechanistic
paths were considered for the C–C coupling step: the first
two paths, A and B, involve coupling between two intermediates which
are both in oxygen vacancies; and the third path, C, involves coupling
between one intermediate in an oxygen vacancy and one intermediate
outside of an oxygen vacancy. The results suggest that the dominant
path to the C3 product, acetone, depends on the conditions. The less
active path (attributed to path A or B) occurs at 600–700 K
and involves coupling between two irreversibly bound species. The
more active path (attributed to path C) requires an excess of water,
becomes dominant at 600–800 K, and involves coupling between
one irreversibly bound species and one reversibly bound species. Based
on these various observations from experiments and simulations, an
elementary step is proposed for acetone formation involving a previously
unreported C4 transition state that is formed after aldol addition.
Density functional theory calculations were performed based on this
hypothesis, and it confirmed that this specific and previously unreported
aldol addition path to acetone does exist and that this path consistent
with the experimental data. In this path, C–C formation occurs
to create a C4 intermediate that is bound to an oxygen vacancy, then
a hydrogen transfer with C–C bond breaking occurs that results
in the production of the acetone molecule. The proposed mechanism
is also consistent with the experimental observation that acetone
formation has a greater than first-order dependenc...