5
38
M. C. COURTNEY, A. C. MACCORMACK, R. A. MORE O’FERRALL
general problem of interrelating pK values for ionisation
reactions involving different leaving groups. The attrac-
tion of establishing such relationships is that in favour-
able cases equilibrium constants can be derived from
solvolysis measurements in aqueous solution in the same
solid, leaving the unreacted fluorenone in solution.
Neutralization of the hydrochloride with aqueous ammo-
nia yielded the imine, which was crystallized from
tolnene–methanol to give yellow needles (22.5 g, 41%
36
1
yield): m.p. 123.5–124.5°C (lit. 124°C); H NMR
24
way as for the azides discussed above, i.e. by com-
bining the solvolysis rate constant with a rate constant for
the reverse reaction which is assumed to be diffusion
(CDCl ), ꢀ 7.14–8.27 (m, 8H, fluorenyl rings), 10.32 (s,
3
1H, NH).
34
controlled. Then if an equilibrium constant for one
leaving group becomes available, others may be deduced.
However, in the absence of relevant thermodynamic
measurements, more information on (equilibrium con-
stants for) s-bond interactions of the leaving groups will
be required to make the necessary interpolations. In
principle this information may be accessible from cal-
Kinetic and equilibrium measurements. Kinetic
methods for the measurement of rate constants for
dehydration of anthracene hydrate and solvolysis of
9-acetoxy-9,10-dihydroanthracene in water or water–
acetonitrile mixtures have been described, as have
product analyses and trapping experiments with azide
2
ion. Similar methods were used for the TFE–H O
2
35
culations.
solvent mixtures.
Determination of the ratio of aromatic product to
hydrate formed from solvolysis of 9-acetoxy-9,10-di-
hydroanthracene was based on differences in absorbance
at 251 nm between the beginning of the solvolysis
reaction (estimated from injection from a stock solution
EXPERIMENTAL
Instrumentation and reagents. NMR measurements
were made with a Jeol JNMGX270 spectrometer
of the substrate into non-solvolysing acetonitrile), Ainit,
1
13
operating at 270 MHz for H NMR and 68 MHz for
NMR. UV–Vis spectra were recorded using Phillips PU
600, Bausch and Lomb Spectronic and Perkin-Elmer
C
the absorbance at the completion of the reaction, A , and
0
the absorbance following addition of a small amount of a
strong acid to effect conversion of anthracene hydrate to
anthracene, Amax. In principle, some trifluorethyl ether
would also be formed in the solvolysis but inspection of
the dependence of the product ratio of alcohol and
trifluoroethyl ether upon pKR for the carbocation in
previous studies suggested that the amount would be
8
Hitachi 124 spectrophotometers, with thermostatting of
cell compartments at 25.0 Æ 0.1°C for kinetic measure-
ments. Reagents, including the solvent trifluoroethanol,
were normally purchased from Aldrich and used without
purification; acetonitrile was of HPLC grade. Water for
kinetic measurement was doubly distilled.
18
small enough (<5%) to be neglected. The ratio of
anthracene to hydrate in the solvolysis products (and thus
kp/k ) is then given by (A À Ainit)/(Amax À A ) and was
Synthesis. The preparation of 9-hydroxy-and 9-acetoxy-
H O
0
0
2
2
9
,10-dihydroanthracene has been described previously.
based on the following measurements of A and A
:
max
0
Fluorenimine was prepared by the method of Hilbert and
Pinck, with the variations described below.
0.45, 0.53; 0.46, 0.53; and 0.48, 0.54. In each case Ainit
was 0.16.
36
Addition of sodium azide to the solvolysis reaction led
Fluorenimine (7). Fluorenone (50.0 g, 0.278 mol) was
heated slightly above its melting-point (82°C) and
gaseous ammonia, dried by passage through a calcium
oxide tower, bubbled through the melt for 7 days, using a
bubbler with a sintered-glass end to give a large gas–
liquid surface area. Formation of the imine was detected
by thin-layer chromatography on silica [chloroform:
R (ketone) = 0.8; R (imine) = 0.3] although extensive
hydrolysis occurred (even on neutral alumina plates).
The reaction could be crudely monitored by the increase
in bath temperature necessary to maintain the melt in the
molten state, since the melting-point of the imine product
to a reduction in absorbance of the product from A to
0
Aaz. As described above, a ratio of rate constants for
trapping the solvolytic intermediate (presumed to be the
anthracenonium ion) by azide ion and water is obtained
À
from a plot of 1/(A À A ) against [N ], as shown in
az
init
3
Fig. 1. The measured values of A at the indicated
az
concentration of azide ion were: 0.51, 0 M; 0.38,
0.0015 M; 0.38, 0.0020 M; 0.37, 0.0030 M; 0.34,
0.0040 M; 0.295, 0.0045 M; and 0.30, 0.0060 M. In all
cases Ainit was 0.16.
f
f
Following the trapping by azide ion a further increase
in absorbance was observed which was attributed to
solvolysis of the azide trapped product 9-azido-9,10-
dihydroanthracene. Rate constants for this process
(
124°C) is higher than that of fluoreneone (82°C).
Completion of the reaction was difficult to attain because
of accumulation in the melt of water produced during the
reaction and because the solubility of the ammonia falls
with increasing temperature.
4
À1
(10 k s ) were measured at the indicated concentra-
obs
À
tions of azide ion and plotted against [N ] in Fig. 2:
3
3.42, 0.0015 M; 3.12, 0.002 M; 3.59, 0.003 M; 2.86,
0.004 M; 3.09, 0.0045 M; 2.60, 0.006 M; 2.51, 0.010 M;
2.10, 0.015 M; 1.99, 0.020 M; 1.66, 0.040 M; 1.57,
0.060 M; 1.52, 0.080 M; and 1.52, 0.1 M.
The melt was allowed to solidify and then dissolved in
chloroform and shaken with dilute hydrochloric acid. The
fluorenimine hydrochloride precipitated as an orange
Copyright 2002 John Wiley & Sons, Ltd.
J. Phys. Org. Chem. 2002; 15: 529–539