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Volumn 47, Issue 1, 2002, Pages 81-98

Transport of a passive scalar in a stratified porous medium

Author keywords

Dispersion; Groundwater; Heterogeneous formations; Hydrogeology; Solute concentration

Indexed keywords

ANISOTROPY; HYDRAULIC CONDUCTIVITY; PROBABILITY DISTRIBUTIONS; SHEAR FLOW; VELOCITY;

EID: 0036530210     PISSN: 01693913     EISSN: None     Source Type: Journal    
DOI: 10.1023/A:1015079408153     Document Type: Article
Times cited : (26)

References (23)
  • 1
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    • Effects of local dispersion and sampling volume on the evolution of concentration fluctuations in aquifers
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    • Andricevic, R.1
  • 7
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    • Stochastic modelling of groundwater flow by unconditional and conditional probabilities: The solute transport
    • (1982) Water Resour. Res , vol.18 , Issue.4 , pp. 835-848
    • Dagan, G.1
  • 9
    • 0025586906 scopus 로고
    • Transport in heterogeneous porous formations: Spatial moments, ergodicity and effective dispersion
    • (1990) Water Resour. Res , vol.26 , pp. 1281-1290
    • Dagan, G.1
  • 10
    • 0026376829 scopus 로고
    • Dispersion of a passive solute in non-ergodic transport by steady velocity fields in heterogeneous formations
    • (1991) J. Fluid. Mech , vol.233 , pp. 197-210
    • Dagan, G.1
  • 12
    • 0030789676 scopus 로고    scopus 로고
    • The influence of pore-scale dispersion on concentration statistical moments in transport through heterogeneous aquifers
    • (1997) Water Resour. Res , vol.33 , pp. 1595-1606
    • Dagan, G.1    Fiori, A.2
  • 13
    • 0032950902 scopus 로고    scopus 로고
    • Concentration fluctuations in transport by groundwater: Comparison between theory and field experiments
    • (1999) Water Resour. Res , vol.35 , pp. 105-112
    • Fiori, A.1    Dagan, G.2
  • 14
    • 0033844573 scopus 로고    scopus 로고
    • Concentration fluctuations in aquifer transport: A rigorous first-order solution and applications
    • (2000) J. Cont. Hydr , vol.45 , pp. 139-163
    • Fiori, A.1    Dagan, G.2
  • 17


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.