Abstract
Following the pioneering work by G. J. Kynch [7], the theory of one-dimensional kinematic waves has been applied to a variety of settling processes due to gravity and centrifugal forces, respectively, cf. [6], [10], [12] and [14] for surveys. While most of the work on gravity settling is concerned with constant cross sections, cross sectional areas changing with the distance from the axis of rotation play an important role in centrifugation processes. In particular, in cylindrical centrifuges without compartments the cross-sectional area is proportional to the radial coordinate, giving rise to rather peculiar kinematic-wave phenomena [2]. It is obvious that the formulation of the problem in terms of only one spatial coordinate (“one-dimensional flow”) is strictly valid in that case.
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Schneider, W. (2003). On the One-Dimensional Flow Approximation in Sedimentation Processes. In: Gyr, A., Kinzelbach, W. (eds) Sedimentation and Sediment Transport. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-0347-5_19
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DOI: https://doi.org/10.1007/978-94-017-0347-5_19
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