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A comparison of a pseudo-homogeneous non-equilibrium model and a three-phase non-equilibrium model for catalytic distillation

✍ Scribed by Yuxiang Zheng; Flora T.T. Ng; Garry L. Rempel


Book ID
108082527
Publisher
Elsevier Science
Year
2004
Tongue
English
Weight
994 KB
Volume
100
Category
Article
ISSN
1385-8947

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## Abstract Sediment transport in rill flows exhibits the characteristics of non‐equilibrium transport, and the sediment transport rate of rill flow gradually recovers along the flow direction by erosion. By employing the concept of partial equilibrium sediment transport from open channel hydraulic