Roll waves on a layer of a muddy fluid flowing down a gentle slope—A Bingham model

DOI10.1063/1.868148zbMath0829.76005OpenAlexW2023136307MaRDI QIDQ4841927

Chiang C. Mei, Ko-Fei Liu

Publication date: 25 January 1996

Published in: Physics of Fluids (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1063/1.868148

zbMATH Keywords

long waves of finite amplitudeshallow layerlinearized instability analysisperiodic shocksKármán momentum integral approach

Mathematics Subject Classification ID

Non-Newtonian fluids (76A05) Hydrology, hydrography, oceanography (86A05) Parallel shear flows in hydrodynamic stability (76E05)

Related Items (12)

Shear-thickening suspensions down inclines: from Kapitza to Oobleck waves ⋮ Wavy regime of a power-law film flow ⋮ Fluid boundary of a viscoplastic Bingham flow for finite solid deformations ⋮ Impact force of roll waves against obstacles ⋮ Low-dimensional models of thin film fluid dynamics. ⋮ Formation and evolution of roll waves in a shallow free surface flow of a power-law fluid down an inclined plane ⋮ Shallow flows of generalised Newtonian fluids on an inclined plane ⋮ Asymptotic expansion of the velocity field within the front of viscoplastic surges: comparison with experiments ⋮ The front runner in roll waves produced by local disturbances ⋮ Linear stability of shallow morphodynamic flows ⋮ Transient fluid motions in a simplified model for oilfield plug cementing. ⋮ BGK based finite volume scheme for hydraulic applications

Cites Work

• Wave formation in laminar flow down an inclined plane
• Long waves on inclined films at high Reynolds number
• Approximate equations for the slow spreading of a thin sheet of Bingham plastic fluid
• The motion of a finite mass of granular material down a rough incline
• Slow spreading of a sheet of Bingham fluid on an inclined plane
• Stability of Liquid Flow down an Inclined Plane
• Mathematical solution of the problem of roll‐waves in inclined opel channels

This page was built for publication: Roll waves on a layer of a muddy fluid flowing down a gentle slope—A Bingham model