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Though reactant 1 is too large to diffuse through the pores
of a large-pore zeolite like faujasite, it may react on the acid
sites accessible through the external surface of the zeolite and
may generate the corresponding carbocation. To test that
possibility, we selected an USY acidic zeolite (Si/Al ratio =
15) that presents mesopores, giving larger external surface
area than the starting NaY zeolite. Then, an ethanolic
solution of compound 1 was added on H-USY and a rapid
change of color was observed. In situ infrared experiments
(IR, Figure S1 in the Supporting Information, SI) showed the
formation of minor amounts of ketone 1a,[7] which may
indicate that the delocalized carbocation given in Scheme 1 is
being formed and, at some extent, reacting with H2O. To
further confirm this, we synthesized the isotopically-labeled
13C-propargyl alcohol 1 (13C-1,1,3-triphenylpropargyl alcohol
1; Scheme S1)[8] and the evolution of the marked substrate in
solution in the presence of catalytic amounts of H-USY
(5 wt%) or triflic acid (HOTf, 20 mol%) was followed by
in situ 1H and 13C NMR spectroscopy. The results in Figure 1
Figure 2. Diffuse-reflectance (A) and UV/Vis (B–E) (in 1,4-dioxane)
spectra of compound 1 under acidic conditions: A) compound
1 impregnated in H-USY zeolite as an ethanolic solution, of which the
ethanol was evaporated by drying at 608C; B) compound 1 in solution
after addition of 5 mol% of triflimidic acid HNTf2 at 1008C; C) com-
pound 1 after addition of 5 mol% of HCl at 1008C; D) compound
1 after addition of 5 mol% of p-TSA at 1008C; and E) compound 1.
spectrum of the H-USY zeolite after impregnation with
1 (line A), and this band nicely fits with that of the
carbocation generated in solution with a catalytic amount of
a very soft acid such as triflimidic acid (line B). Notice that the
intensity of the band decreases for harder acids than
triflimidic acid such as HCl and para-toluenesulfonic acid
(p-TSA; lines C and D). These results are in line with the
lower amount of ketone 1a detected by NMR with the H-
USY zeolite and triflimidic acid, suggesting that the carbo-
cation forms and stays longer with the softer acids. Thus, we
can say that the carbocation of 1 can be formed on H-USY
with an efficiency that is, at least, comparable with typical
strong Brønsted acids such as HCl, p-TSA, HOTf, and HNTf2.
If the formation of the carbocation would exclusively
depend on the acid strength of the catalyst, the weaker acidity
of the H-USY zeolite should hardly promote the reaction
according to its much lower pKa (or H0) value.[9] Thus another
factor such as the properties of the counteranion is playing
a key role on the formation and stabilization of the
carbocation on the zeolite. A possible way to determine the
influence of the proton and of the counteranion on the
formation of the carbocation separately would consist in
correlating the activation energy (Ea) of the reaction with an
acidity parameter (H0 or pKa) of the catalyst.[10] If the acid
strength is the only responsible factor for the formation of the
carbocation, a linear relationship between Ea and the acid
strength should be found. On the other hand, if the counter-
anion is further stabilizing the carbocation, a lower Ea of that
expected from the corresponding pKa of the acid will be
observed.
Figure 1. In situ 1H NMR experiments of the isotopically labeled 13C-
propargyl alcohol 1 in acid conditions using 1,4-dioxane-d8 as a solvent.
A) compound 13C-1; B) compound 13C-1 in the presence of 5 wt% of
H-USY zeolite at 1008C after 15 min; C) compound 13C-1 in the
presence of 5 wt% of H-USY zeolite at 1008C after 20 h; and D) com-
pound 13C-1 in the presence of 20 mol% of HOTf at 1008C after
15 min.
1
show that the signal in the H NMR spectrum at 5.52 ppm
corresponding to the hydroxy group of the alcohol slighty
decreases for the zeolite (B and C) and disappears for triflic
acid (D). Additionally, an increase of the water signal at
2.15 ppm was observed for the zeolite (B and C) and aromatic
signals of ketone 1a appeared at ca. 8 ppm for triflic acid (D).
These results indicate that a minor product is formed with H-
USY that cannot be detected by NMR spectroscopy. A
13C NMR measurement (Figure S2) confirms this point.
To directly detect the carbocation, we performed diffuse-
reflectance UV/Vis spectroscopy measurements of the zeolite
impregnated with the propargyl alcohol. We expected that the
delocalized carbocation would have a long enough lifetime to
observe the extinction molar coefficient, even at very low
concentration. Figure 2 shows a new band in the UV/Vis
Figure 3 shows that a straight line is found for different
sulfonic acids (methylsulfonic MeSA, p-TSA, and TfOH)
indicating that mainly the acid strength controls the carbo-
cation formation when sulfonate is the counteranion. How-
ever, triflimidic acid HNTf2 shows a similar activation energy
than TfOH despite having a much lower acidity,[11] with an
additional stabilization of ca. 30–60 kJmolÀ1 (depending on
the acid parameter considered) due to the highly delocalized
triflimidate anion. Remarkably, the H-USY zeolite behaves
like HNTf2, with a stabilization of about 40 kJmolÀ1.
2
ꢀ 2015 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim
Angew. Chem. Int. Ed. 2015, 54, 1 – 6
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