TY - JOUR
T1 - High-pressure polymorphism in l-threonine between ambient pressure and 22 GPa
AU - Giordano, Nico
AU - Beavers, Christine M.
AU - Kamenev, Konstantin V.
AU - Marshall, William G.
AU - Moggach, Stephen A.
AU - Patterson, Simon D.
AU - Teat, Simon J.
AU - Warren, John E.
AU - Wood, Peter A.
AU - Parsons, Simon
N1 - Funding Information:
This research used resources of the Advanced Light Source, which is a DOE Office of Science User Facility under contract no. DE-AC02-05CH11231. CMB and beamline 12.2.2 are supported by the Consortium for Materials Properties Research in Earth Sciences (COMPRES) under NSF Cooperative Agreement EAR 1606856. We also gratefully acknowledge The STFC (UK) for provision of beamtime at SRS Daresbury Laboratory and the ISIS Facility. NG is supported by an EPSRC Doctoral Training Account studentship (No. 1637415) and an ALS Doctoral Fellowship. SDP was supported by an EPSRC Doctoral Training Account studentship and the Cambridge Crystallographic Data Centre. We also thank Mr Matthew Reeves (University of Edinburgh) for his assistance with his program MR-PIXEL which facilitates preparation of data for PIXEL calculations. Computational work made use of high performance computing facilities at The University of Edinburgh.
Funding Information:
This research used resources of the Advanced Light Source, which is a DOE Office of Science User Facility under contract no. DE-AC02-05CH11231. CMB and beamline 12.2.2 are supported by the Consortium for Materials Properties Research in Earth Sciences (COMPRES) under NSF Cooperative Agreement EAR 1606856. We also gratefully acknowledge The STFC (UK) for provision of beamtime at SRS Daresbury Labo- ratory and the ISIS Facility. NG is supported by an EPSRC Doctoral Training Account studentship (No. 1637415) and an ALS Doctoral Fellowship. SDP was supported by an EPSRC Doctoral Training Account studentship and the Cambridge Crystallographic Data Centre. We also thank Mr Matthew Reeves (University of Edinburgh) for his assistance with his program MR_PIXEL which facilitates preparation of data for PIXEL calculations. Computational work made use of high performance computing facilities at The University of Edinburgh.
Publisher Copyright:
© 2019 The Royal Society of Chemistry.
PY - 2019
Y1 - 2019
N2 - The crystal structure of l-threonine has been studied to a maximum pressure of 22.3 GPa using single-crystal X-ray and neutron powder diffraction. The data have been interpreted in the light of previous Raman spectroscopic data by Holanda et al. (J. Mol. Struct. (2015), 1092, 160-165) in which it is suggested that three phase transitions occur at ca. 2 GPa, between 8.2 and 9.2 GPa and between 14.0 and 15.5 GPa. In the first two of these transitions the crystal retains its P212121 symmetry, in the third, although the unit cell dimensions are similar either side of the transition, the space group symmetry drops to P21. The ambient pressure form is labelled phase I, with the successive high-pressure forms designated I′, II and III, respectively. Phases I and I′ are very similar, the transition being manifested by a slight rotation of the carboxylate group. Phase II, which was found to form between 8.5 and 9.2 GPa, follows the gradual transformation of a long-range electrostatic contact becoming a hydrogen bond between 2.0 and 8.5 GPa, so that the transformation reflects a change in the way the structure accommodates compression rather than a gross change of structure. Phase III, which was found to form above 18.2 GPa in this work, is characterised by the bifurcation of a hydroxyl group in half of the molecules in the unit cell. Density functional theory (DFT) geometry optimisations were used to validate high-pressure structural models and PIXEL crystal lattice and intermolecular interaction energies are used to explain phase stabilities in terms of the intermolecular interactions.
AB - The crystal structure of l-threonine has been studied to a maximum pressure of 22.3 GPa using single-crystal X-ray and neutron powder diffraction. The data have been interpreted in the light of previous Raman spectroscopic data by Holanda et al. (J. Mol. Struct. (2015), 1092, 160-165) in which it is suggested that three phase transitions occur at ca. 2 GPa, between 8.2 and 9.2 GPa and between 14.0 and 15.5 GPa. In the first two of these transitions the crystal retains its P212121 symmetry, in the third, although the unit cell dimensions are similar either side of the transition, the space group symmetry drops to P21. The ambient pressure form is labelled phase I, with the successive high-pressure forms designated I′, II and III, respectively. Phases I and I′ are very similar, the transition being manifested by a slight rotation of the carboxylate group. Phase II, which was found to form between 8.5 and 9.2 GPa, follows the gradual transformation of a long-range electrostatic contact becoming a hydrogen bond between 2.0 and 8.5 GPa, so that the transformation reflects a change in the way the structure accommodates compression rather than a gross change of structure. Phase III, which was found to form above 18.2 GPa in this work, is characterised by the bifurcation of a hydroxyl group in half of the molecules in the unit cell. Density functional theory (DFT) geometry optimisations were used to validate high-pressure structural models and PIXEL crystal lattice and intermolecular interaction energies are used to explain phase stabilities in terms of the intermolecular interactions.
UR - http://www.scopus.com/inward/record.url?scp=85070097453&partnerID=8YFLogxK
U2 - 10.1039/c9ce00388f
DO - 10.1039/c9ce00388f
M3 - Article
AN - SCOPUS:85070097453
SN - 1466-8033
VL - 21
SP - 4444
EP - 4456
JO - CrystEngComm
JF - CrystEngComm
IS - 30
ER -