1 / 37

Orleans July 2004

Orleans July 2004. Networks in physics and biology . Potential Energy Landscape in Models for Liquids. In collaboration with E. La Nave, A. Moreno, I. Saika-Voivod, E. Zaccarelli. A 3-slides preamble: Thermodynamics and Dynamics Review of thermodynamic formalism in the PEL approach

fay
Télécharger la présentation

Orleans July 2004

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Orleans July 2004 Networks in physics and biology Potential Energy Landscape in Models for Liquids In collaboration with E. La Nave, A. Moreno, I. Saika-Voivod, E. Zaccarelli

  2. A 3-slides preamble: Thermodynamics and Dynamics Review of thermodynamic formalism in the PEL approach Potential Energy Landscapes in Fragile and Strong (Network-Forming) liquids. Outline Outline

  3. Strong and Fragile liquids Dynamics A slowing down that cover more than 15 order of magnitudes P.G. Debenedetti, and F.H. Stillinger, Nature 410, 259 (2001). 1

  4. A Decrease in Configurational Entropy: Thermodynamics Why do we care Thermodyanmics Is the excess entropy vanishing at a finite T ? 1

  5. The basic idea: Separation of time scales f(t) glass liquid f(t) van Megen and S.M. Underwood Phys. Rev. Lett. 70, 2766 (1993) Glass Supercooled Liquid log(t)

  6. Potential Energy Landscape, a 3N dimensional surface Statistical description of the number, depth and shape of the PEL basins e IS P IS w The PEL does not depend on TThe exploration of the PEL depends on T

  7. Z(T)= S Zi(T) allbasins i fbasin i(T)= -kBT ln[Zi(T)] fbasin(eIS,T)= eIS+ kBTSln [hwj(eIS)/kBT] + fanharmonic(eIS, T) normal modes j

  8. Thermodynamics in the IS formalism Stillinger-Weber F(T)=-kBT ln[W(<eIS>)]+fbasin(<eIS>,T) with Basin depth and shape fbasin(eIS,T)= eIS+fvib(eIS,T) and Number of explored basins Sconf(T)=kBln[W(<eIS>)]

  9. Distribution of local minima (eIS) Configuration Space + Real Space Vibrations (evib) rN evib eIS

  10. <eIS>(T) (steepest descent minimization) fbasin(eIS,T) (harmonic and anharmonic contributions) F(T) (thermodynamic integration from ideal gas) From simulations….. F(T)=-kBT ln[W(<eIS>)]+fbasin(<eIS>,T) E. La Nave et al., Numerical Evaluation of the Statistical Properties of a Potential Energy Landscape, J. Phys.: Condens. Matter 15, S1085 (2003).

  11. Fragile Liquids: The Random Energy Model for eIS Hypothesis: e-(eIS -E0)2/2s 2 W(eIS)deIS=eaN -----------------deIS 2ps2 S ln[wi(eIS)]=a+b eIS Predictions: <eIS(T)>=E0-bs 2 - s 2/kT Sconf(T)=aN-(<eIS (T)>-E0)2/2s 2

  12. T-dependence of <eIS> SPC/E LW-OTP T-1 dependence observed in the studied T-range Support for the Gaussian Approximation

  13. BMLJ Sconf BMLJ Configurational Entropy

  14. Landscape Equation of State P=-∂F/∂V|T F(V,T)=-TSconf(T,V)+<eIS(T,V)>+fvib(T,V) In Gaussian (and harmonic) approximation P(T,V)=Pconst(V)+PT(V) T + P1/T(V)/T Pconst(V)= - d/dV [E0-bs2] PT(V) =R d/dV [a-a-bE0+b2s2/2] P1/T(V) = d/dV [s2/2R]

  15. Non Gaussian Behaviour in BKS silica

  16. Sconf Silica Non-Gaussian Behavior in SiO2 Eis e S conf for silica… Esempio di forte Non gaussian silica

  17. Density minimum and CV maximum in ST2 water Density Minima P.Poole inflection in energy inflection = CV max

  18. ST2 2650 punti Isochores of liquid ST2 water • HDL LDL ?

  19. Maximum Valency Maximum Valency Model (Speedy-Debenedetti) V(r ) SW if # of bonded particles <= Nmax HS if # of bonded particles > Nmax r A minimal model for network forming liquids The IS configurations coincide with the bonding pattern !!!

  20. It is possible to calculate exactly the basin free energy ! Basin Free energy

  21. Ground State Energy Known ! It is possible to equilibrate at low T ! Energy per Particle

  22. Viscosity and Diffusivity: Arrhenius

  23. Configurational Entropy

  24. Fragile Liquids Gaussian Energy Landscape Finite TK, Sconf(TK)=0 Strong Liquids: “Bond Defect” landscape (binomial) A “quantized” bottom of the landscape ! Degenerate Ground State Sconf(T=0) different from zero ! Suggestions for further studies…..

  25. Acknowledgements We acknowledge important discussions, comments, collaborations, criticisms from… A. Angell, P. Debenedetti, T. Keyes, A. Heuer, G. Ruocco , S. Sastry, R. Speedy … and their collaborators

  26. Stoke-Einstein Relation

  27. Citazioni goldstein, stillinger

  28. Gaussian Distribution ? eIS=SeiIS E0=<eNIS>=Ne1IS s2= s2N=N s21

  29. Diffusivity

  30. Phase Diagram NMAX-modifiedPhase Diagram

  31. The V-dependence of a, s2, E0 e-(eIS -E0)2/2s 2 W(eIS)deIS=eaN -----------------deIS 2ps2

  32. SPC/E P(T,V)=Pconst(V)+PT(V) T + P1/T(V)/T FS, E. La Nave, and P. Tartaglia, PRL. 91, 155701 (2003)

  33. D ST2 Isobars of diffusion coefficient for ST2 water

  34. Adam-Gibbs Plot

  35. Basin Free Energy kBTSln [hwj(eIS)/kBT] LW-OTP SPC/E S ln[wi(eIS)]=a+b eIS …if b=0 …..

  36. BKS Silica Eis nel tempo

More Related