메뉴 건너뛰기




Volumn 63, Issue 2 I, 2001, Pages 0205011-0205014

Simple fluids with complex phase behavior

Author keywords

[No Author keywords available]

Indexed keywords

FREEZING; GLASS TRANSITION; INTEGRAL EQUATIONS; MICELLES; MONTE CARLO METHODS; PHASE DIAGRAMS; SUPERCOOLING; WATER;

EID: 4243340600     PISSN: 15393755     EISSN: 15502376     Source Type: Journal    
DOI: 10.1103/PhysRevE.63.020501     Document Type: Article
Times cited : (23)

References (30)
  • 3
    • 33645052099 scopus 로고
    • Phys. Lett. A 154, 413 (1991);
    • (1991) , vol.154 , pp. 413
    • Phys Lett, A.1
  • 5
    • 0003625785 scopus 로고
    • edited by J.P. Hansen, D. Levesque, and J. Zinn-Justin North-Holland, Amsterdam
    • P.N. Pusey, in Liquids, Freezing and the Glass Transition, edited by J.P. Hansen, D. Levesque, and J. Zinn-Justin (North-Holland, Amsterdam, 1991);
    • (1991) Liquids, Freezing and the Glass Transition
    • Pusey, P.N.1
  • 6
    • 0004286262 scopus 로고    scopus 로고
    • edited by F. Mallamace and H.E. Stanley IOS Press, Amsterdam
    • The Physics of Complex Fluids, edited by F. Mallamace and H.E. Stanley (IOS Press, Amsterdam, 1997).
    • (1997) The Physics of Complex Fluids
  • 13
    • 33744875530 scopus 로고    scopus 로고
    • e-print cond-mat/0005184.
    • G. Franzese et al., e-print cond-mat/0005184.
    • Franzese, G.1
  • 20
  • 21
    • 33744859763 scopus 로고    scopus 로고
    • 8MCsteps(dependingonthedensity)throughtherelationshipS(k)=〈p(k) ρ(-k)〉.Testrunswith
    • 8 MC steps (depending on the density) through the relationship S(k) = 〈p(k)ρ(-k)〉. Test runs with 5000 particles were performed to check for finite size effects.
    • NVT Ensemble for a System of , vol.1000 , pp. 210
  • 25
    • 33744894804 scopus 로고    scopus 로고
    • note
    • The coexistence curves are calculated by equating, at constant T and P, the chemical potentials of the coexisting phases. Generally, TSC integral equations are derived assuming that local consistency is equivalent to global consistency [18]. Since in the low T-high ρ region this approximation is not very satisfactory and global consistency is unpracticable, the pressure is calculated along mixed isochore-isothermal paths which minimize the isochore portions where the more accurate "compressibility route" pressure cannot be evaluated.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.