4.5 Article

Raman study of pressure-induced phase transitions in crystals of orthorhombic and monoclinic polymorphs of L-cysteine: dynamics of the side chain

期刊

JOURNAL OF RAMAN SPECTROSCOPY
卷 41, 期 12, 页码 1748-1758

出版社

WILEY
DOI: 10.1002/jrs.2624

关键词

Raman spectroscopy; high pressure; phase transitions; amino acid; polymorphism

资金

  1. RFBR [08-03-00143, 09-03-00451]
  2. Presidium of RAS [27.44]
  3. Department of Chemistry and Materials Sciences of RAS [5.6.4.]
  4. SB RAS [13, 109]
  5. CRDF
  6. Russian Ministry of Science and Education [456]
  7. FASI [02.740.11.5102]

向作者/读者索取更多资源

The series of phase transitions on increasing pressure and on reverse decompression was followed in crystals of monoclinic and orthorhombic polymorphs of L-cysteine by using Raman spectroscopy, with the samples placed in a diamond anvil cell together to ensure identical pressures on the two samples. The effects of hydrostatic pressure on the two polymorphs are shown to be radically different. Depending on the starting polymorph, different phases are formed under identical compression/decompression conditions. The effect of pressure on the monoclinic polymorph was studied for the first time. Phase transitions in monoclinic L-cysteine (at similar to 2.9 and similar to 3.9 GPa) are completely reversible without a noticeable hysteresis. The changes in the spectra suggest that the H-bond network is distorted and S-H center dot center dot center dot O bonding dominates over S-H center dot center dot center dot S bonding at high pressures, but the molecular conformations change continuously during these transitions. The data on the orthorhombic polymorph of L-cysteine show that not only the H-bond network is distorted, but also the conformation of the L-cysteine zwitterion changes very substantially. The previously observed discrepancy in the results related to the occurrence of a phase existing between 2.1 and 2.3 GPa reported by Minkov et al. (J. Phys. Chem. B. 2008; 112, 8851) but not observed by Moggach et al. (Acta Crystallogr. B. 2006; 62, 296) could be interpreted; different phases can be formed at the same pressure, depending on how this pressure was reached: on direct compression, or in the compression-decompression-compression cycle. Copyright (C) 2010 John Wiley & Sons, Ltd.

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