Water molecular reorientation in ice and tetrahydrofuran clathrate hydrate from lineshape analysis of 17O spin-echo NMR spectra
Lineshape analysis of 17 O spin-echo NMR spectra has been used to study water molecular reorientations in ice-Ih and THF Structure II clathrate hydrate. The kinetics was determined by the changes of the lineshapes of the 17 O central transitions at different temperatures. A model involving 12 orient...
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Published in | Canadian journal of chemistry Vol. 89; no. 9; pp. 1055 - 1064 |
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Format | Journal Article |
Language | English |
Published |
Ottawa
NRC Research Press
01.09.2011
Canadian Science Publishing NRC Research Press |
Subjects | |
Online Access | Get full text |
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Summary: | Lineshape analysis of
17
O spin-echo NMR spectra has been used to study water molecular reorientations in ice-Ih and THF Structure II clathrate hydrate. The kinetics was determined by the changes of the lineshapes of the
17
O central transitions at different temperatures. A model involving 12 orientations and 4-step jumps of water molecular orientations was proposed. Semi-classical exchange formalism was employed to simulate the lineshape of the central transitions of the
17
O nuclei. Lineshape analysis gave the quadrupolar coupling constant C
Q
= 6.43 MHz and the asymmetry parameter η = 0.935, for both ice-Ih and THF gas hydrate. The theoretical lineshape simulations resulted in activation energies of water molecular reorientations E
a
= 55.2 ± 2.1 kJ mol
–1
and E
a
= 30.5 ± 0.8 kJ mol
–1
for ice-Ih and THF hydrate, respectively. The range of dynamic rates in THF clathrate hydrate is such that before melting, a pseudo-isotropic lineshape is observed that retains a second-order quadrupolar shift. The water reorientation process is discussed in light of recent results on Bjerrum defect injection obtained from molecular dynamics simulation and structural studies. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
ISSN: | 0008-4042 1480-3291 |
DOI: | 10.1139/v11-040 |