Issue 16, 2013

Pressure induced topochemical polymerization of diiodobutadiyne: a single-crystal-to-single-crystal transformation

Abstract

Diiodobutadiyne forms cocrystals with bis(pyridyl)oxalamides, based on halogen bonds between the pyridine groups of the host and the iodoalkynes of the guest. These interactions align the diyne for topochemical polymerization to form poly(diiododiacetylene) or PIDA. To induce polymerization, the crystals are subjected to pressures of 3.5 GPa or above. Previously, we reported spectroscopic evidence of this pressure-induced polymerization, but attempts to recover single crystals after pressure treatment were unsuccessful. Here we present direct structural evidence of clean single-crystal to single-crystal polymerization in these cocrystals. The structure of the polymer cocrystal was solved from single-crystal diffraction data and is supported by high pressure in situ Raman spectroscopy. Careful analysis of the structural changes suggests that increasing pressure changes the packing of host molecules, and that the flexibility of the pyridine ring orientation enables the polymerization. The new sigma bonds of the polymer form at the expense of the halogen bonds in the starting cocrystal; after polymerization, the iodine atoms are no longer ideally located for strong halogen bonding with the host.

Graphical abstract: Pressure induced topochemical polymerization of diiodobutadiyne: a single-crystal-to-single-crystal transformation

Supplementary files

Article information

Article type
Paper
Submitted
13 Nov 2012
Accepted
07 Jan 2013
First published
13 Feb 2013

CrystEngComm, 2013,15, 3106-3110

Pressure induced topochemical polymerization of diiodobutadiyne: a single-crystal-to-single-crystal transformation

H. Jin, A. M. Plonka, J. B. Parise and N. S. Goroff, CrystEngComm, 2013, 15, 3106 DOI: 10.1039/C3CE26851A

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