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Figure 5
(a) Dependence on temperature of the eccentricity of iso-intensity lines (in red) and of the two-dimensional RMS of the ODP functions (in blue) inferred from the eccentricity values. (b) Two-dimensional RMS width of the ODP as directly obtained from the intensity profiles at a fixed q value (see Fig. 4[link]). Both plots show that a moderate decrease of the orientational order occurs as particles swell by taking in one more layer of water, at around 313 K.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 40| Part s1| March 2007| Pages s286-s291
doi:10.1107/S0021889807008552
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