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Volumn 58, Issue 2, 1998, Pages 2090-2096

Macroscopic equations of motion for two-phase flow in porous media

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[No Author keywords available]

Indexed keywords


EID: 0000299374     PISSN: 1063651X     EISSN: None     Source Type: Journal    
DOI: 10.1103/PhysRevE.58.2090     Document Type: Article
Times cited : (73)

References (47)
  • 2
    • 0004062210 scopus 로고
    • Butterworth-Heinemann, Boston
    • P. Adler, Porous Media (Butterworth-Heinemann, Boston, 1992).
    • (1992) Porous Media
    • Adler, P.1
  • 24
    • 85036143004 scopus 로고    scopus 로고
    • Interfacial Phenomena in Petroleum Recovery, edited by N. Morrow (Dekker, New York, 1991), Vol. 36
    • Interfacial Phenomena in Petroleum Recovery, edited by N. Morrow (Dekker, New York, 1991), Vol. 36.
  • 27
    • 11644288134 scopus 로고
    • M. Allen, G. Behie, J. Trangenstein, Springer-Verlag, Berlin
    • J. Trangenstein, in Multiphase Flow in Porous Media, edited by M. Allen, G. Behie, and J. Trangenstein (Springer-Verlag, Berlin, 1988), p. 87.
    • (1988) Multiphase Flow in Porous Media , pp. 87
    • Trangenstein, J.1
  • 33
    • 0024055823 scopus 로고    scopus 로고
    • I. Chatzis, M. Kuntamukkula, and N. Morrow, SPE Reservoir Eng., August 1988, p. 902
    • I. Chatzis, M. Kuntamukkula, and N. Morrow, SPE Reservoir Eng., August 1988, p. 902.
  • 37
    • 85036425736 scopus 로고    scopus 로고
    • P. Øren, J. Billiotte, and W. Pinczewski, SPE Formation Evaluation, March 1992, p. 70
    • P. Øren, J. Billiotte, and W. Pinczewski, SPE Formation Evaluation, March 1992, p. 70.
  • 43
    • 0242294413 scopus 로고
    • edited by M. Allen, G. Behie, J. Trangenstein Springer-Verlag, Berlin
    • M. Allen, in Multiphase Flow in Porous Media, edited by M. Allen, G. Behie, and J. Trangenstein (Springer-Verlag, Berlin, 1988), p. 1.
    • (1988) Multiphase Flow in Porous Media , pp. 1
    • Allen, M.1
  • 44
    • 0004260484 scopus 로고
    • Springer, Berlin, C. Truesdell
    • Rational Thermodynamics, edited by C. Truesdell (Springer, Berlin, 1984).
    • (1984) Rational Thermodynamics
  • 46
    • 85036348679 scopus 로고    scopus 로고
    • Because the rock matrix is assumed to be rigid and impermeable one has [Formula Presented] which implies dissipation. Because of this and Eq. (25) the balance laws for the matrix phase would either be trivial or ill defined
    • Because the rock matrix is assumed to be rigid and impermeable one has RR1=RR2=RR3=RR4=∞, which implies dissipation. Because of this and Eq. (25) the balance laws for the matrix phase would either be trivial or ill defined.
  • 47
    • 85036231194 scopus 로고    scopus 로고
    • Balance equations for the rock matrix do not arise (see Ref. c46
    • Balance equations for the rock matrix do not arise (see Ref. 46).


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.