Origin of Ultrasonic Absorption in Heavy Water

Abstract
Hall's theory of structural relaxation is applied to explain the excess ultrasonic absorption in D2O. Two states, one characterized by higher volume and lower energy (icelike structure) and the other characterized by lower volume and higher energy (close-packed structure) are assumed to be available to each molecule of D2O. The occurrence of a density maximum ρmax at 11.2°C and a static compressibility minimum β0 min at about 75°C favors a two-state model for D2O. The absorption coefficient is calculated with three trial values of β (16×1012, 17×1012, and 18×1012 cm2/dyn). It is found that with β=17×1012 cm2/dyn, Hall's theory agrees very well with the experimental results.

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