2 research outputs found
Kinetics and Mechanism of Ethanol Dehydration on γ‑Al<sub>2</sub>O<sub>3</sub>: The Critical Role of Dimer Inhibition
Steady state, isotopic, and chemical
transient studies of ethanol dehydration on Îł-alumina show unimolecular
and bimolecular dehydration reactions of ethanol are reversibly inhibited
by the formation of ethanol–water dimers at 488 K. Measured
rates of ethylene synthesis are independent of ethanol pressure (1.9–7.0
kPa) but decrease with increasing water pressure (0.4–2.2 kPa),
reflecting the competitive adsorption of ethanol–water dimers
with ethanol monomers; while diethyl ether formation rates have a
positive, less than first order dependence on ethanol pressure (0.9–4.7
kPa) and also decrease with water pressure (0.6–2.2 kPa), signifying
a competition for active sites between ethanol–water dimers
and ethanol dimers. Pyridine inhibits the rate of ethylene and diethyl
ether formation to different extents verifying the existence of acidic
and nonequivalent active sites for the dehydration reactions. A primary
kinetic isotope effect does not occur for diethyl ether synthesis
from deuterated ethanol and only occurs for ethylene synthesis when
the β-proton is deuterated; demonstrating olefin synthesis is
kinetically limited by either the cleavage of a C<sub>β</sub>-H bond or the desorption of water on the γ-alumina surface
and ether synthesis is limited by the cleavage of either the C–O
bond of the alcohol molecule or the Al–O bond of a surface
bound ethoxide species. These observations are consistent with a mechanism
inhibited by the formation of dimer species. The proposed model rigorously
describes the observed kinetics at this temperature and highlights
the fundamental differences between the Lewis acidic Îł-alumina
and Brønsted acidic zeolite catalysts
Effects of Composition and Structure of Mg/Al Oxides on Their Activity and Selectivity for the Condensation of Methyl Ketones
The effects of chemical
composition and pretreatment on Mg–Al
hydrotalcites and alumina-supported MgO were evaluated for the gas-phase,
self-condensation reaction of C<sub>3</sub>–C<sub>5</sub> biomass-derived
methyl ketones. We show that the selectivity toward the acyclic dimer
enone and the cyclic enone trimer can be tuned by controlling the
temperature of hydrotalcite calcination. Methyl ketone cyclization
is promoted by Lewis acidic sites present on the hydrotalcite catalysts.
XRD and thermal decomposition analysis reveal that the formation of
periclase MgO starts above 623 K accompanied by complete disappearance
of the hydrotalcite structure and is accompanied by an increase in
hydroxyl condensation as the formation of well-crystallized periclase. <sup>27</sup>Al MQMAS and <sup>25</sup>Mg MAS NMR show that at progressively
higher temperatures, Al<sup>3+</sup> cations diffuses out of the octahedral
brucite layers and incorporate into the tetrahedral and octahedral
sites of the MgO matrix thereby creating defects to compensate the
excess positive charge generated. The oxygen anions adjacent to the
Mg<sup>2+</sup>/Al<sup>3+</sup> defects become coordinatively unsaturated,
leading to the formation of new basic sites. A kinetic isotope effect, <i>k</i><sub>H</sub>/<i>k</i><sub>D</sub> = 0.96, is
observed at 473 K for the reaction of (CH<sub>3</sub>)<sub>2</sub>CO versus (CD<sub>3</sub>)<sub>2</sub>CO, which suggests that carbon–carbon
bond formation leading to the dimer aldol product is the rate-determining
step in the condensation reaction of methyl ketones. We also show
that acid–base catalysts having similar reactivity and higher
hydrothermal stability to that of calcined hydrotalcites can be achieved
by creating defects in MgO crystallites supported alumina as a consequence
of the diffusion of Al<sup>3+</sup> cations into MgO. The physical
properties of these materials are shown to be very similar to those
of hydrotalcite calcined at 823 K