On the role of mechanical interactions in the steady-state gravity flow of a two-constituent mixture down an inclined plane

DOI10.1098/rspa.1996.0061zbMath0879.76114OpenAlexW2142548383WikidataQ59839462 ScholiaQ59839462MaRDI QIDQ4716835

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Publication date: 22 January 1998

Published in: Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1098/rspa.1996.0061

zbMATH Keywords

analytical solutionsStokes flownumerical solutionsice sheetzeroth approximationapproximations of higher ordersbasal rock surfacenon-uniform volume distribution of constituentssediment-ice layer

Mathematics Subject Classification ID

Multiphase and multicomponent flows (76T99) Glaciology (86A40)

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