100
M. Senzlober et al. / Journal of Fluorine Chemistry 99 (1999) 99±104
heated to 2508C. After puri®cation by repeated sublimation
in vacuo, a 71% yield of (1a) was obtained as colourless,
strongly light-refracting crystals of m.p. 408C. When the
¯uorination was not brought to completion, some squaric
The contents of trap 3 could be separated into a fraction
consisting mostly of (5) and (6), while a second fraction was
enriched in (7). All products were identi®ed by their IR
spectra: (5) [16], (6) [17], (7) [18].
acid ¯uoridechloride (1b) could be detected by 19F and 13
C
The C3F4 isomers (5), (6) and (7) have previously been
observed as products of the decomposition of (2a) in the gas
phase at a pressure of several mbar [3]. Moreover, (6) has
been detected as a secondary product formed by reactions of
:CF2 with F2C==C: [19]. It has been argued that F2C==C:
may be readily formed by thermal rearrangement of (2a).
Thus, the formation of (6) by thermolysis of (1a) may well
involve the formation of (2a) as a primary product, into
which, after isomerization to di¯uorovinylidene, :CF2
inserts. Alternatively, rapid attack of :CF2 on di¯uoroviny-
lidene formed by thermolysis of (4) [20] (which was
de®nitely identi®ed as the major component in trap 2) also
may lead to (6).
Compound (7) has been observed as one of the products
in the photochemical decomposition of both di¯uoromaleic
anhydride [21] and CFI==CFI [22], both reactions also
yielding (2a). Indeed, (7) may be the common precursor
of (5) and (6), both products being formed in the CO2 laser
pyrolysis of (7) [23].
NMR spectroscopy (see below). As a more volatile by-
product, 1,4-di¯uoro-2-butyne-1,4-dione [10,11] was
obtained in the 1268C trap and identi®ed by mass, IR
and NMR spectra. Some CF2O was found in the LN2 trap.
(1a) was identi®ed by mass spectra, 13C and 19F NMR
spectra, gas phase infrared spectra, and Raman spectra
obtained of the solid and a solution in CDCl3. The assign-
ment of the vibrational spectra was supported by ab initio
calculations (see below).
In order to collect information and experience on the
thermolysis of dihalogeno derivatives of (1), in general, we
have studied, beforehand, the thermolysis of (1c), squaric
acid chloridebromide (1d), X1 = Cl, X2 = Br, and (1e),
X1 = X2 = Br. The latter two are accessible by the reaction
of (1c) with trimethylsilyl bromide [12], pure (1e) being
obtained when an excess of Me3SiBr was employed, while a
1 : 2 : 1 mixture of (1c), (1d) and (1e) was produced with a
1 : 1 ratio of the reactants.
The dihalogeno derivatives of (1) were pyrolyzed at
7008C in the gas phase at a pressure of 10 3 mbar by
passing them slowly through a quartz tube of 50 cm length
and 2.5 cm inner diameter. The reaction products were
pumped through a series of traps held at 78, 126 and
1968C. The different condensates were analyzed by low
resolution IR spectroscopy. The dihaloalkynes (2c), C2ClBr
(2d) and C2Br2 (2e) were obtained from (1c), (1d) and (1e),
respectively, in yields between 40 and 50% and identi®ed by
comparing their IR spectra with those reported in the
literature [13,14].
To our surprise, the pyrolysis of (1a) under the same
conditions did not yield any (2a) at all. Work-up in vacuo of
the volatile reaction products by fractional condensation at
1268C (trap 1), 1608C (trap 2) and 1968C (trap 3), and
investigation of the trap contents by low resolution IR
spectroscopy, and in part, by mass spectroscopy (see below)
gave the following results:
At pressures ꢁ0.1 mbar, none of the C3F4 isomers has
been detected among the decomposition products of (2a)
[21,22]. On the other hand, decomposition of (2a) in solu-
tion, and as a solid at 1968C, yields C2F4, most likely by
dimerization of :CF2 [3]. Concomitantly, a solid `carbon
polymer' built up of sp3 carbon centers (ꢁ (CC), Raman,
1
1326 cm [24]) deposits. The presumed decomposition
pathway of (1a) is shown in Scheme 2.
From the observed pyrolysis products of (1a), we con-
clude that, in spite of our inability to produce any (2a) owing
to secondary reactions, C2F2 is formed. Although (1a) is
obviously not suitable as a precursor for (2a), we are
planning to further investigate the decomposition of (1a)
under rigorously different conditions to support this con-
clusion.
3. Spectroscopic properties of squaric acid difluoride
ꢀ Trap 1 contained an involatile, yellow polymeric material
that changes in colour to black when exposed to air. We
presume that this material emerges from the polymeriza-
tion of difluoropropadienone (4) in analogy to observa-
tions by Brahms and Dailey [15].
We have studied (1a) and (1b) by 13C and 19F NMR
spectroscopy, and furthermore, (1a) by mass, IR and Raman
spectroscopy.
3.1. NMR spectra
ꢀ Trap 2. The material obtained in this trap was mostly (4),
which was identified by its IR spectrum [15]. In addition,
a second volatile, yet unidentified product exerting IR
absorptions at 2258(s), 1735(s), 1278(s), 1197(w) and
980(w) cm 1, and an involatile polymer formed by sec-
ondary reactions, were detected by IR spectroscopy.
ꢀ Trap 3 contained, along with some SiF4 and the uni-
dentified volatile product also found in trap 2, the three
C3F4 isomers CF3C>CF (5), CF2CCF2 (6) and cyclo-
C3F4 (7).
The NMR data of (1a) and (1b) are listed in Table 1, while
Fig. 1 displays the 13C and 19F NMR spectra of (1a). In
principle, both ole®nic and carbonyl resonances represent
the X parts of ABX spin systems. Due to the large differ-
ences in coupling constants J(AX), 364.0 Hz, and J(BX),
2.7 Hz, as well as the very small AB (3J(FF)) coupling of
1.0 Hz, the signal of the 13CFA == 12CFB fragment reveals a
®rst-order doublet of doublets pattern. In contrast, high-