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- W1490357132 abstract "The injection of heated water into a ground water stream of constant velocity is studied. The heated water is discharged through a fully penetrating injection well into a confined aquifer of constant thickness. For steady state conditions and under the assumption that heat conduction and dispersion in the aquifer and through the confining layers are negligible in comparison to the convective heat transport, it is shown that the flow and temperature field is dependent on the relative infiltration rate and on the relative buoyancy of well discharge. First results of a steady-state three-dimensional numerical model are given. L' injection d'eau chauffee dans un ecoulement d'eau souterraine a vitesse constante est etudie. L'eau chauffee dans un aquifere phreatique d'epaisseur constante a l'aide d'un puits d'injection penetrant toute l'epaisseur. Dans un etat stationnaire ou suppose que la conduction de chaleur et la dispersion dans l'aquifere et a trovers l' impermeable couche superficielle peuvent etre negliquees on comparaison du transport convective de chaleur. En ce cas il est montre que la distribution de la vitesse et de la temperature depend du debit relative d' infiltration et de la sous-pression hydrostatique relative de l'eau chauffee. Premiers resultats d'un modele numerique tridimensionelle sont presentes." @default.
- W1490357132 created "2016-06-24" @default.
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- W1490357132 date "1979-01-01" @default.
- W1490357132 modified "2023-09-23" @default.
- W1490357132 title "Effect of buoyancy on the flow and temperature fields near injection wells" @default.
- W1490357132 doi "https://doi.org/10.18419/opus-607" @default.
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