US geological Survey Water Supply Paper, 2337. Use of temperature profiles beneath streams to determine rates of vertical ground-water flow ans vertical hydraulic conductivity / Lapham, W. W.

Public ISBD Titre de série : US geological Survey Water Supply Paper, 2337 Titre : Use of temperature profiles beneath streams to determine rates of vertical ground-water flow ans vertical hydraulic conductivity Type de document : texte imprimé Auteurs : Lapham, W. W. Mention d'édition : US geological Survey, Federal Center Editeur : US geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-05686 Note générale : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Langues : Anglais (eng) Mots-clés : Température  Hydrogéologie  Eau souterraine  Sédiment  Conductivité hydraulique Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Note de contenu : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. US geological Survey Water Supply Paper, 2337. Use of temperature profiles beneath streams to determine rates of vertical ground-water flow ans vertical hydraulic conductivity [texte imprimé] / Lapham, W. W.  . -  US geological Survey, Federal Center . - US geological Survey, Federal Center, 1989. ISSN : CI-05686 This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Langues : Anglais (eng) Mots-clés : Température  Hydrogéologie  Eau souterraine  Sédiment  Conductivité hydraulique Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Note de contenu : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media.

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