Abstract
Proton spin-lattice relaxation timesT1 in hexagonal ice have been measured from −10 to −80°C for different external Zeeman fieldsHR from 0.125 to 6.57 kOe. The results can be described byT1∼H 2 R exp(ΔEc/kT) (ΔEc=activation energy). In pure ice (HR ∥c-axis)ΔEc is 0.62 eV, whereas relaxation due to impurities givesΔE′c≈0.25 eV. The analysis of these results including additional data of the dielectric relaxation and the self-diffusion coefficient yields thatT1 in pure ice is determined mainly by the motion of Schottky defects. Bjerrum faults give an additional but small contribution. SettingT1=C·τc (τc=molecular correlation time which is proportional to exp(ΔEc/kT), C=constant depending onHR and molecular distances) we calculatedC with the model mentioned above and found e.g. 0.88 · 106 atHR=6.57 kOe.E′c≈0.25 eV is assumed to be the energy of migration of Bjerrum and ionic faults.
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Herrn Prof. Dr. H. O.Kneser danken wir für sein Interesse an dieser Arbeit und die Durchsicht des Manuskriptes. Die Deutsche Forschungsgemeinschaft stellte Sachmittel zur Verfügung.
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Siegle, G., Weithase, M. Spin-Gitter-Relaxation der Protonen in hexagonalem Eis. Z. Physik 219, 364–380 (1969). https://doi.org/10.1007/BF01395533
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DOI: https://doi.org/10.1007/BF01395533