Vol. 29, No. 7, 2018
Nilo et al.
1505
in solution provide a clear indication that the precipitates
are symmetric single carbon-type products.
of recrystallization on the class of the product formed is
pertinent.
2
7
The simulated spectra for cyanuric and isocyanuric
In the literature, crystallization is considered a
critical operation regarding polymorphs, where sensitive
parameters such as solvent and cooling rate of the
solution should be carefully controlled to obtain a given
“monomorph”. Many references on how to conduct
well-monitored crystallization operations, particularly
those concerning active pharmaceutical ingredients (APIs),
26
acids showed a peak at 163.87 ppm for the former species
and one at 149.90 ppm for the latter species, indicating
that isocyanuric acid is the species present in solution
and is most likely predominant in the solid product. The
value of 150.3 ± 0.25 ppm is appropriate for the carbon
atom of an imide group. The slight displacement of the
delta values of most analytes from the central value may
indicate a (small) difference in the carbon environment
of these analytes.
28
can be found in the literature.
In general, we observed (very small) changes in the
number of peaks when the analytes were recrystallized from
water but no changes inVA-classes (no strict protocols were
used in these recrystallizations). These results lead to a few
persistent questions: why does recrystallization of a cyanuric
acid analyte of a given VA-class from water tend to produce
an analyte of the same class (albeit occasionally adding or
subtracting peaks from the spectrum of the original analyte)?
Why does the analyte not move toward a more stable
configuration? If the solubilization of the analyte would result
in the complete disruption of the original solid in isolated
molecules (as observed with the dissolution of the analytes
in DMSO), then the new solid formed by recrystallization
of the dissolved individual molecules would be expected
to crystallize into a more stable structure. However, it was
observed that even when the crystallizations were conducted
under no special conditions, the VA-class of the original
analyte was conserved. The retention of the VA-classes
after recrystallization of the analytes of differentVA-classes
suggests that during the process of recrystallization, a
“memory” of the original solid form remains in the solution
with the entire polymorph or parts of it (oligomorphs)
acting as seeds. This proposal also indicates that the solid
does not decompose completely in solution to form isolated
cyanuric/isocyanuric acid molecules (at least, not under the
recrystallization conditions used in this study); otherwise,
the migration of at least one of the analytes from a given
class to another class would be expected.
Despite these observations, the behavior of some of
the analytes causes doubt about the “class conservation”
mentioned above. Infrared spectra I001504S and
I001504A of analyte 15.04, for instance, are two spectra
from the same sample prepared on two different dates,
05/07/2012 and 05/25/2016, respectively (the only
difference between these two spectra seems to be that
the analyst picked up different parts of the same sample
from the same vial at different times). Table 3 reveals that
each spectrum belongs to a different VA-class. According
to this Table, the same observation could be made with
analytes 17.06 and 47.18. A question could be raised
regarding whether these two VA-classes were present
13
The spectra of solid C NMR for the complete set of
analytes in this paper are more complex, and the discussion
of these spectra will be presented in another publication
jointly with other data.
Furthermore, these measurements allowed the
establishment of a clear distinction between VA-classes 1
and 4 and VA-classes 2 and 3 because of their solubility
in DMSO: VA-classes 1 and 4 are insoluble (with the
exception of analyte 19.06, which was, however, difficult
to dissolve), whereas VA-classes 2 and 3 are soluble.
1
3
The list is completed with the C NMR peaks of
Sigma-Aldrich cyanuric acid (150.09 ppm in DMSO) and
trichloroisocyanuric acid (145.33 ppm in acetone-d6).
Additional information can be added here: energy
dispersive X-ray spectroscopy (EDS) measurements of
analytes of VA-classes 1 and 4 that did not dissolve in
DMSO showed the presence of potassium in their structure
(
analyte 21.04, VA-class 4, 21.6% K; analyte 26.06,
VA-class 4, 11.9% K; and analyte 205.10, VA-class 1,
5.3% K). Despite being categorized in VA-class 4,
1
analyte 19.06 was different from the other analytes of
this class: it did not crystallize into plates (unlike all the
others) and presented a very low value of potassium: 0.1%.
The presence of chlorine, an indication of possible residue
from trichloroisocyanuric acid, was detected only in trace
amounts in some of the analytes and should not interfere
with the spectra of the analytes (the presence of chlorine
2
3
was verified using very sensitive Feigl tests).
13
On the one hand, the results from the C NMR spectra
of a group of analytes in solution described in this paper
showed that they had only one peak with practically equal
chemical shifts. On the other hand, the bar infrared data
of the respective solid analytes differ quite massively. The
combination of these two pieces of information suggests
the existence of different arrangements of the isocyanuric
acid in the solid analytes (polymorphism).
Since all analytes resulting from these reactions were
recrystallized from water, presenting a short discussion
regarding the observations made of the possible effect