Skip to main content

Part of the book series: Environmental Science and Engineering ((ENVENG))

Abstract

We introduce a mathematical formalism towards the construction of a continuum-field theory for particulate fluids and solids. We briefly outline a research program aimed at unifying the fundamentals of the coarse-graining theory and the numerical method of Smoothed Particle Hydrodynamics (SPH). We show that the coarse-graining functions must satisfy well defined mathematical properties that comply with those of the SPH kernel integral representation of continuous fields. Given the appropriate dynamics for the macroscopic response, the present formalism is able to describe both the solid and fluid-like behaviour of granular materials.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 129.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 169.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 169.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Notes

  1. 1.

    For granular systems this approach seems doomed from the outset: because energy is lost through internal friction, and gained by a non-thermal source such as tapping or shearing, the dynamical equations do not leave the canonical or any other known ensemble invariant.

  2. 2.

    Remark 1 In general, an \(n\)-rank tensor function \(G:\fancyscript{D}\rightarrow \mathbb {R}^4\otimes ^{[n]}\mathbb {R}^4\) (where \(\otimes ^{[n]}\) denotes the \(n\)-rank tensor product) is not an observable. Nevertheless, each component of the tensor is an observable. Typical examples are the components of the stress tensor (\(\sigma ^{\alpha \beta }\), where Greek indices denote Cartesian coordinates), or the components of the velocity field (\(v^{\alpha }\)).

References

  • de Gennes PG (1999) Granular matter. A tentative view. Rev Mod Phys 71:S374–S382

    Article  Google Scholar 

  • Gingold RA, Monaghan JJ (1977) Smoothed particle hydrodynamics–Theory and application to non-spherical stars. Monthly Not R Astron Soc 181:375–389

    Google Scholar 

  • Glasser BJ, Goldhirsch I (2001) Scale dependence, correlations, and fluctuations of stresses in rapid granular flows. Phys Fluids 13:407–420

    Article  Google Scholar 

  • Goldhirsch I (2003) Rapid granular flows. Annu Rev Fluid Mech 35:267–293

    Article  Google Scholar 

  • Gray JP, Monaghan JJ, Swift RP (2001) SPH elastic dynamics. Comput Methods Appl Mech Eng 190:6641–6662

    Article  Google Scholar 

  • Babic M (1997) Average balance equations for granular materials. Int J Eng Sci 5:523–548

    Article  Google Scholar 

  • Irving JH, Kirkwood JG (1950) The statistical mechanical theory of transport processes. IV. The equations of hydrodynamics. J Chem Phys 18:817–829

    Article  Google Scholar 

  • Jaeger HM, Nagel SR, Behringer RP (1996) Granular solids, liquids, and gases. Rev Mod Phys 68:1259–1273

    Article  Google Scholar 

  • Kadanoff LP (1999) Built upon sand: theoretical ideas inspired by granular flows. Rev Mod Phys 71:435–444

    Article  Google Scholar 

  • Kirkwood JG (1946) The statistical mechanical theory of transport processes I. General theory. J Chem Phys 14:180–201

    Google Scholar 

  • Li S, Liu WK (2007) Meshfree particle methods. Springer-Verlag, Berlin

    Google Scholar 

  • Liu GR, Liu MB (2003) Smoothed particle hydrodynamics: a meshfree particle method. World Scientific, Singapore

    Book  Google Scholar 

  • Liu MB, Liu GR, Lam KY (2003) Constructing smoothing functions in smoothed particle hydrodynamics with applications. J Comp Appl Math 155:263–284

    Article  Google Scholar 

  • Liu MB, Liu GR (2006) Restoring particle consistency in smoothed particle hydrodynamics. Appl Num Math 56:19–36

    Article  Google Scholar 

  • Liu MB, Liu GR (2010) Smoothed particle hydrodynamics (SPH): an overview and recent developments. Arch Comput Methods Eng 17:25–76

    Article  Google Scholar 

  • Lucy LB (1977) A numerical approach to the testing of the fission hypothesis. Astro J 82:1013–1024

    Article  Google Scholar 

  • Monaghan JJ (1992) Smoothed particle hydrodynamics. Ann Rev Astron Astrophys 30:543–574

    Article  Google Scholar 

  • Murdoch AI, Kowalski SJ (1992) On fluid-fluid coupling within porous media: a mixture theoretic approach based upon molecular considerations. Transp Porous Media 8:47–70

    Article  Google Scholar 

  • Murdoch AI, Bedeaux D (1994) Continuum equations of balance via weighted averages of microscopic quantities. Proc R Soc A 445:157–179

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Leonardo Trujillo .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2014 Springer International Publishing Switzerland

About this chapter

Cite this chapter

Marín, J.F., Petit, J.C., Sigalotti, L.D.G., Trujillo, L. (2014). Integral Representation for Continuous Matter Fields in Granular Dynamics. In: Sigalotti, L., Klapp, J., Sira, E. (eds) Computational and Experimental Fluid Mechanics with Applications to Physics, Engineering and the Environment. Environmental Science and Engineering(). Springer, Cham. https://doi.org/10.1007/978-3-319-00191-3_33

Download citation

Publish with us

Policies and ethics