Analytical continuum mechanics à la Hamilton–Piola least action principle for second gradient continua and capillary fluids
Top Cited Papers
- 28 August 2013
- journal article
- research article
- Published by SAGE Publications in Mathematics and Mechanics of Solids
- Vol. 20 (4) , 375-417
Abstract
In this paper a stationary action principle is proved to hold for capillary fluids, i.e. fluids for which the deformation energy has the form suggested, starting from molecular arguments. We remark that these fluids are sometimes also called Korteweg–de Vries or Cahn–Allen fluids. In general, continua whose deformation energy depends on the second gradient of placement are called second gradient (or Piola–Toupin, Mindlin, Green–Rivlin, Germain or second grade) continua. In the present paper, a material description for second gradient continua is formulated. A Lagrangian action is introduced in both the material and spatial descriptions and the corresponding Euler–Lagrange equations and boundary conditions are found. These conditions are formulated in terms of an objective deformation energy volume density in two cases: when this energy is assumed to depend on either C and ∇ C or on C−1 and ∇ C−1, where C is the Cauchy–Green deformation tensor. When particularized to energies which characterize fluid materials, the capillary fluid evolution conditions are recovered. A version of Bernoulli’s law valid for capillary fluids is found and useful kinematic formulas for the present variational formulation are proposed. Historical comments about Gabrio Piola’s contribution to analytical continuum mechanics are also presented.Keywords
All Related Versions
This publication has 117 references indexed in Scilit:
- Theoretical nonlinear response of complex single crystal under multi-axial tensile loadingScientific Reports, 2013
- Thermomechanics of shells undergoing phase transitionJournal of the Mechanics and Physics of Solids, 2011
- On the effect of twist angle on nonlinear galloping of suspended cablesComputers & Structures, 2009
- What are the dominant thermomechanical processes in the basal sediment layer of large ice sheets?Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1998
- Moving contact lines in the Cahn-Hilliard theoryInternational Journal of Engineering Science, 1996
- ENERGY DENSITY EQUATIONS AND POWER FLOW IN STRUCTURESJournal of Sound and Vibration, 1995
- Pseudomomentum and material forces in nonlinear elasticity: variational formulations and application to brittle fractureActa Mechanica, 1992
- A phenomenological approach to phase transition in classical field theoryInternational Journal of Engineering Science, 1987
- On the derivation of thermomechanical balance equations for continuous systems with a nonmaterial interfaceInternational Journal of Engineering Science, 1987
- The method of virtual power in continuum mechanics application to media presenting singular surfaces and interfacesActa Mechanica, 1986