Rheological characteristics of solid-fluid transition in dry granular dense flows: A thermodynamically consistent constitutive model with a pressure-ratio order parameter

DOI10.1002/NAG.834zbMath1273.74051OpenAlexW2097849481MaRDI QIDQ2854883

Chung Fang

Publication date: 24 October 2013

Published in: International Journal for Numerical and Analytical Methods in Geomechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1002/nag.834

zbMATH Keywords

constitutive modelphase transitionorder parametergranular matter

Mathematics Subject Classification ID

Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Thermodynamics in solid mechanics (74A15) Granularity (74E20) Granular flows (76T25)

Related Items (2)

A \(k\)-\(\varepsilon\) turbulence closure model of an isothermal dry granular dense matter ⋮ Rapid dry granular flows down an incline: a constitutive theory with an independent kinematic internal length

Cites Work

• Unnamed Item
• A unified evolution equation for the Cauchy stress tensor of an isotropic elasto-visco-plastic material. I: On thermodynamically consistent evolution
• Continuum equations of balance in classical statistical mechanics
• Constitutive models for granular materials including quasi-static frictional behaviour: Toward a thermodynamic theory of plasticity
• On flows of granular materials
• On the thermodynamics of a mixture of isotropic materials with constraints
• A thermo-mechanical continuum theory with internal length for cohesionless granular materials. I: A class of constitutive models.
• Shearing flows of a dry granular material—hypoplastic constitutive theory and numerical simulations
• Grain flow as a fluid-mechanical phenomenon
• A theory for the rapid flow of identical, smooth, nearly elastic, spherical particles
• Boundary conditions for high-shear grain flows
• The Thickness of Steady Plane Shear Flows of Circular Disks Driven by Identical Boundaries
• The stress tensor in a granular flow at high shear rates
• Gravity flow of cohesionless granular materials in chutes and channels
• Thermodynamically consistent modelling of abrasive granular materials. I Non–equilibrium theory
• Stress-controlled elastic granular shear flows
• Thermodynamics

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