TY - JOUR
T1 - Selective Nucleation and Growth of an Organic Polymorph by Ledge-Directed Epitaxy on a Molecular Crystal Substrate
AU - Bonafede, Salvatore J.
AU - Ward, Michael D.
PY - 1995
Y1 - 1995
N2 - Selective growth of a thermodynamically less preferred polymorph of the salt (DMTC+)(TMO-)•CHCl3(DMTC = 3,3’-dimethylthiacarbocyanine; TMO = 3,3’,5,5’-tetramethyltrimethine oxonol) has been achieved from CHCl3 solutions by nucleation on single-crystal succinic acid (SA) substrates. This process occurs by a ledgedirected epitaxy (LDE) mechanism in which the dihedral angle between two close-packed planes of a substrate ledge site matches that of two close-packed planes of a prenucleation aggregate corresponding to the observed polymorph. The observed orientation of (DMTC+)(TMO-)•CHCl3 is consistent with interaction of the close-packed (010) and (014) planes of its aggregate with succinic acid (010) and (111) planes that define ledges along the [101] direction of the substrate. These ledge sites are produced readily by cleavage of SA single crystals. The identity of the polymorph and its orientation are confirmed by visible spectroscopy, crystal morphology, and atomic force microscopy. While LDE allows for two possible orientations of (DMTC+)(TMO-)•CHCl3, the orientation observed is that in which the lattice mismatch along the interface is minimized. These observations illustrate that crystallization processes based on LDE may be valuable for selective growth of polymorphs.
AB - Selective growth of a thermodynamically less preferred polymorph of the salt (DMTC+)(TMO-)•CHCl3(DMTC = 3,3’-dimethylthiacarbocyanine; TMO = 3,3’,5,5’-tetramethyltrimethine oxonol) has been achieved from CHCl3 solutions by nucleation on single-crystal succinic acid (SA) substrates. This process occurs by a ledgedirected epitaxy (LDE) mechanism in which the dihedral angle between two close-packed planes of a substrate ledge site matches that of two close-packed planes of a prenucleation aggregate corresponding to the observed polymorph. The observed orientation of (DMTC+)(TMO-)•CHCl3 is consistent with interaction of the close-packed (010) and (014) planes of its aggregate with succinic acid (010) and (111) planes that define ledges along the [101] direction of the substrate. These ledge sites are produced readily by cleavage of SA single crystals. The identity of the polymorph and its orientation are confirmed by visible spectroscopy, crystal morphology, and atomic force microscopy. While LDE allows for two possible orientations of (DMTC+)(TMO-)•CHCl3, the orientation observed is that in which the lattice mismatch along the interface is minimized. These observations illustrate that crystallization processes based on LDE may be valuable for selective growth of polymorphs.
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U2 - 10.1021/ja00135a001
DO - 10.1021/ja00135a001
M3 - Article
AN - SCOPUS:85006900123
SN - 0002-7863
VL - 117
SP - 7853
EP - 7861
JO - Journal of the American Chemical Society
JF - Journal of the American Chemical Society
IS - 30
ER -