C. Sun, Y.-Y. Zhao and J. M. Curtis
indicates that the peak at 19.3 min probably contains an sn-2
isomer. In order to confirm this and obtain more structural
information, tandem mass spectrometry was performed on
the ion at m/z 950 eluting at 19.6 and 19.3 min (Figs. 5(a1) and
5(a2)). It can be seen that the relative intensity of the product
ion at m/z 603 is considerably greater in the former case. The
ion at m/z 603 is the result of neutral loss of ammonia along with
loss of a fatty acyl chain that contains a trioxolane group
[(C57H104O9 + NH4) – C18H34O5 – NH3]+ (cleavage at position
a or equivalent). An ESI study of the ammonium ion adducts
of TAG positional isomers described by Byrdwell and Neff[22]
demonstrates that the loss of a fatty acyl chain from either the
sn-1 or the sn-3 position is energetically favored over the loss
from the sn-2 position. Thus, it is expected that loss of the fatty
acyl chain containing the trioxolane group would be more facile
at the sn-1 or sn-3 positions compared to that at the sn-2
position. Hence, the higher intensity of the fragment ion at
m/z 603 of the compound eluting at 19.6 min compared to that
eluting at 19.3 min suggests that the former has the trioxolane
group at the sn-1 or sn-3 position whereas the latter is substi-
tuted at sn-2. This interpretation is also consistent with the
above discussion concerning the abundance of these isomers.
Other product ions at m/z 493, 509 and 465 are also observed
(Figs. 5(a1) and 5(a2)). The loss of a fatty acyl chain and the
cleavage of the trioxolane group along with neutral loss
of ammonia lead to the formation of the ion at m/z 493
[(C57H104O9 + NH4) – C18H34O2 – C9H18O2 – NH3]+. This is
shown as cleavage at position b and c in the inset of Fig. 5(a1)
for the illustrative example of an sn-1 mono-ozonide with loss
of the sn-3 fatty acyl chain. Similarly, the fragment ion at m/z
509 [(C57H104O9 + NH4) – C18H34O2 – C9H18O - NH3] + results
from cleavage at positions equivalent to b and d. Previously, it
has been proposed that fragmentation at the trioxolane group
can cause the cleavage of the hydrocarbon chain adjacent to the
trioxolane group.[14] For example, cleavage of the bond between
the n-8 and n-9 positions, which results in the formation of a
cleavage at positions a, c and f) and 415 (ÀNH3, cleavage at posi-
tions a, d and g) (Fig. 5(b)) are also observed. These come from the
loss of one fatty acyl chain and the cleavage of both trioxolane
groups, which results in aldehyde/aldehyde, aldehyde/
carboxylic acid and carboxylic acid/carboxylic acid at the former
two n-9 positions. The ion at m/z 635 is the product ion from neu-
tral loss of ammonia along with fragmentation at positions d and
f. The MS/MS spectra of the [M + NH4]+ ions (m/z 998) of the
compounds eluting at 15.6, 15.9 and 16.2 min all contain the
same product ions, but with differences in their intensity ratios.
This probably arises due to the presence of positional and geo-
metrical isomers but at this point there is no further data avail-
able for us to draw any conclusion on which isomers are present.
The mass spectra from the peaks at 11.9, 12.3, 12.6 and
12.9 min all have the ion at m/z 1046 as their base peak. Clearly,
the observation of the [M + NH4]+ ion at m/z 1046 demonstrates
tri-ozonide formation. Since all of the double bonds have been
ozonized, tri-ozonide can only exist as cis/trans geometric
isomers, which is also the reason that there are four peaks
instead of one peak shown between 11.0 and 13.0 min. Figure 5
(c) is the MS/MS spectrum of a tri-ozonide [M + NH4]+ ion,
which has product ions at m/z 399 (ÀNH3, cleavage at posi-
tions a, c and g), 383 (ÀNH3, cleavage at positions a, c and f)
and 415 (ÀNH3, cleavage at positions a, d and g) similar to
the di-ozonide. Product ions at m/z 369 (ÀNH3, cleavage at
positions a, e and g) and 353 (ÀNH3, cleavage at positions
a, e and f) are also observed. The other isomeric tri-ozonide
MS/MS spectra differ only also in the relative intensities of
the product ions.
Besides the formation of ozonides, the peaks at 13.6 and
13.9 min in Fig. 4(b) show the presence of ozonolysis
intermediates. Thus, the ion at m/z 792 is the base peak of the
mass spectra of peaks at 13.6 and 13.9 min (Fig. 4, inset (c)).
From the elemental composition (Table 1) and knowledge
of the ozonolysis reaction pathway, this ion is likely the
decomposition product of a mono-ozonide with an alde-
hyde group at an n-9 position. Since this aldehyde can
be present on the sn-2 or sn-1 position, two isomeric peaks
are observed. Other intermediate ions such as m/z 888 and
840 are also observed, which are the decomposition pro-
ducts of di-ozonides and tri-ozonides with an aldehyde
group at n-9, respectively.
In addition to the intermediates and products listed in
Table 1, high molecular weight products were also formed.
Figure 6 shows the XIC over the range of m/z 1000 to 2000
from the reaction of triolein with ozone for 60, 105 and
120 min. At 60 min of ozonolysis, an ion at m/z 1776 appears
with low intensity in the mass spectrum compared to the base
peak at m/z 998, a di-ozonide (Fig. 6, inset (a)). However, after
120 min of ozonolysis, peaks at similar retention times have
mass spectra in which the ion at m/z 998 is absent whereas
the ion at m/z 1776 is the base peak (Fig. 6, inset (b)). Hence,
longer reaction times are resulting in the formation of higher
amounts of high molecular weight products. The structure of
the ion at m/z 1776 is proposed in inset (c) of Fig. 6, which
might be formed by the cycloaddition of the ozonolysis inter-
mediate having an aldehyde group at n-9 (m/z 888) with the
corresponding Criegee intermediate. It should be noted that
the ozonolysis intermediate with an [M + NH4]+ ion at m/z
888 was also observed (Table 1). Although the dimer
[M + NH4]+ ion at m/z 1776 has the same retention time as
the di-ozonide [M + NH4]+ ion at m/z 998, it can be seen from
product ion at m/z 465 [(C57H104O9 + NH4) – C18H34O2
–
C10H19O3 – NH3]+ (cleavage at position b and e or equivalent).
The peaks in the chromatogram at retention times of 15.6,
15.9 and 16.2 min (Fig. 4(b)) were found to have the same
[M + NH4]+ ion at m/z 998 as the base peak in each case. This
indicates the formation of at least three isomeric forms of the
di-ozonide. Since the di-ozonide has an additional oxygen-
containing functional group with three more oxygens com-
pared to the mono-ozonide, it has higher polarity and would
be expected to elute earlier in NARP chromatography. This is
consistent with the peak elution order seen in Fig. 4(b). The
di-ozonide from triolein can exist as sn-1,3 or sn-1,2 positional
isomers. In addition, each positional isomer can also have
cis/trans geometric isomers,[23] some of which may be separated
under the chromatographic conditions used here. Theoretically,
there can be three cis/trans isomers of an sn-1,3 di-ozonide plus
three cis/trans isomers of an sn-1,2 di-ozonide. However, in the
present experiment, a total of only three peaks are separated, so
assignment of the exact isomeric structure of each peak is not
yet possible.
The MS/MS spectrum of the di-ozonide [M + NH4]+ ion
shows the same product ions at m/z 493 (ÀNH3, cleavage at
positions b and c), m/z 509 (ÀNH3, cleavage at positions b
and d) and m/z 465 (ÀNH3, cleavage at positions b and e) as
was seen for the mono-ozonide. In addition, product ions at
m/z 399 (ÀNH3, cleavage at positions a, c and g), 383 (ÀNH3,
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Rapid Commun. Mass Spectrom. 2012, 26, 921–930