Crystal Growth & Design
Article
the results of XPRD analyses indicate only 2 transformed to
Form I, while 1, 3, and 4 remained unchanged. Indeed, the
solids of 1−4 can keep their crystalline forms in phosphate
buffer of 6.8 for 3.5, 2.0, 6.0, and 15.0 h, respectively (Figure 7),
and then 1, 2, and 4 transformed to Form I, while 3 trans-
formed to Form III. The above results indicate that both the
solubility and stabilities of 1−4 in phosphate buffer are better
than those of agomelatine with acetic acid and ethylene glycol
we reported before. It is interesting to note that the stabilities
of 1−4 in phosphate buffer are related to the solubility of
corresponding coformers (Figure 8), as the solubility values of
glycolic acid (b), urea (a), isonicotinamide (c), methyl 4-hydroxy-
benzoate (d), and agomelatine Form II in phosphate buffer of
pH 6.8 are 1786, 873, 163, 30, and 0.51 mg/mL, respectively,
and the stability of corresponding 2, 1, 3, and 4 is 2.0, 3.5, 6.0,
and 15.0 h in phosphate buffer of pH 6.8, respectively,
indicating the larger difference of solubility between the
agomelatine and coformer in a given cocrystal leads to the
lower stability of the cocrystal, as the coformer with larger
solubility in a cocrystal is easier to dissolve in water and leads to
the cocrystal decomposed more quickly in water.
(2009ZX09501-022), and China Postdoctoral Science Founda-
tion (Grant No. 20110490919).
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CONCLUSIONS
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Six kinds of synthons were used to construct the cocrystals of
agomelatine, and four cocrystals of agomelatine with urea,
glycolic acid, isonicotinamide, and methyl 4-hydroxybenzoate
were obtained and determined by single crystal X-ray
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ASSOCIATED CONTENT
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S
* Supporting Information
The XPRD patterns and IR spectra for 1−4. This material is
AUTHOR INFORMATION
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Corresponding Author
Notes
The authors declare no competing financial interest.
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ACKNOWLEDGMENTS
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This work was supported by 973 Program of China
(2012CB821705), NSFC (20831005, 21101173, 91127002
and 21121061), the National Key Program of China
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dx.doi.org/10.1021/cg201423q | Cryst. Growth Des. 2012, 12, 2226−2233