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Mass Exchange Between Mobile Fresh Water and Immobile Saline Water in the Unsaturated Zone
H. Gvirtzman
, M. Magaritz
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peer-review
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Keyphrases
Clay
33%
Clay Minerals
33%
Dispersion Kinetics
33%
Dispersive Flow
33%
Flow Exchange
33%
Freshwater
100%
Immobile Water
33%
Initial-boundary Conditions
33%
Irrigation
33%
Mass Exchange
100%
Mass Exchange Coefficient
33%
Matrix Characteristics
66%
Measured Profile
66%
Mobile Domain
33%
Mobile Water
66%
Narrow Passage
33%
Nonequilibrium Transport
33%
Partially Saturated
33%
Physical Nonequilibrium
33%
Rain
33%
Saline Water
100%
Semi-arid Area
33%
Temporal Change
33%
Transport Model
33%
Tritium Concentration
33%
Two-component Domains
33%
Unsaturated Zone
100%
Water Domain
66%
Water Pocket
33%
Earth and Planetary Sciences
Boundary Condition
50%
Clay Mineral
50%
Fossil
50%
Freshwater
100%
Tritium
50%
Vadose Zone
100%
Engineering
Boundary Condition
33%
Convective
33%
Exchange Coefficient
33%
Fresh Water
100%
Immobile Water
33%
Mass Exchange
100%
Nonequilibrium
33%
Tritium
33%
Chemical Engineering
Clay Mineral
100%
Tritium
100%
Immunology and Microbiology
Dispersion
100%