We investigated the adsorption and reaction of pyridine on flat Pt(111) and stepped Pt(355) surfaces via high-resolution in situ x-ray photoelectron spectroscopy. The surfaces were exposed to pyridine at temperatures between 112 and 300 K while simultaneously recording XP spectra. Subsequently, the crystals were annealed and the temperature dependencies of the N 1s and C 1s core levels were studied again in a continuous and quantitative way. Various surface species were found, namely, physisorbed, flat-lying and end-on pyridine, α-pyridyl species on the terraces and on the steps and several unidentified high temperature species. We were able to show an influence of the steps of Pt(355) by pre-adsorbing silver next to the step, which selectively suppresses the step adsorption.
Using
a concerted effort from both experiment and theory, we determine
the thermal decomposition mechanism for guaiacol on Pt(111), a reaction
of interest in the area of bio-oil upgrading. This work serves as
a demonstration of the power of combining in situ temperature-programmed
X-ray photoelectron spectroscopy (TPXPS) and density functional theory
(DFT) to elucidate complex reaction mechanisms occurring on heterogeneous
surfaces. At low temperature (230 K), guaiacol was found to chemisorb
with the aromatic ring parallel to the Pt(111) surface with five distinct
carbon species and three oxygen species. As the temperature was increased,
TPXPS showed several significant changes to the surface species. The
increase in the species associated with the decomposition of the functional
groups of guaiacol is followed by their subsequent disappearance and
an increase in the nonaromatic carbon signal. On the basis of an energetic
analysis of the various mechanisms using DFT, along with the comparison
of the experimentally and theoretically derived core-level binding
energies, we determined that guaiacol’s decomposition mechanism
occurs via the dehydrogenation of both the methyl and hydroxyl functional
groups, followed by demethylation of the CH2 or CH group
to form 1,2-benzoquinone. Further heating to above 375 K likely breaks
the aromatic ring and results in the rapid formation and desorption
of CO, accounting for the disappearance of the O 1s signal above 450
K. These results show that a knowledgeable application of TPXPS and
DFT can result in the quantitative identification of surface species
during complex reactions, providing insight useful for the design
of future heterogeneous surfaces.
Five marijuana samples were compared using bulk isotope analysis compound-specific isotope ratio analysis of the extracted cannabinoids. Owing to the age of our cannabis samples, four of the five samples were compared using the isotope ratios of cannabinol (CBN), a stable degradation product of Δ(9)-tetrahydrocannabinol (THC). Bulk δ(13)C isotope analysis discriminated between all five samples at the 95% confidence level. Compound-specific δ(13)C isotope analysis could not distinguish between one pair of the five samples at the 95% confidence level. All the measured cannabinoids showed significant depletion in (13)C relative to bulk isotope values; the isotope ratios for THC, CBN, and cannabidiol were on average 1.6‰, 1.7‰, and 2.2‰ more negative than the bulk values, respectively. A more detailed investigation needs to be conducted to assess the degree fractionation between the different cannabinoids, especially after aging.
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