U.S. Geological Survey Water Supply, 2205. Mathematical model of the Tesuque aquifer system near Projoaque, New Mexico / Hearne, G. A.

Public ISBD Titre de série : U.S. Geological Survey Water Supply, 2205 Titre : Mathematical model of the Tesuque aquifer system near Projoaque, New Mexico Type de document : texte imprimé Auteurs : Hearne, G. A. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1985 ISBN/ISSN/EAN : CI-05101 Note générale : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Langues : Anglais (eng) Mots-clés : Bassin versant  Eau souterraine  Eau de surface  Hydrologie  Modèle mathématique  Bassin hydrologique Index. décimale : 551.48 Hydrologie : Résumé : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Note de contenu : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. U.S. Geological Survey Water Supply, 2205. Mathematical model of the Tesuque aquifer system near Projoaque, New Mexico [texte imprimé] / Hearne, G. A.  . -  U. S. Geological Survey . - U. S. Geological Survey, 1985. ISSN : CI-05101 A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Langues : Anglais (eng) Mots-clés : Bassin versant  Eau souterraine  Eau de surface  Hydrologie  Modèle mathématique  Bassin hydrologique Index. décimale : 551.48 Hydrologie : Résumé : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Note de contenu : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model.

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U.S. Geological Survey Water Supply paper, 2206. Simulation of an aquifer test on the Tesuque Pueblo Grant, New Mexico / Hearne, G. A.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2206 Titre : Simulation of an aquifer test on the Tesuque Pueblo Grant, New Mexico Type de document : texte imprimé Auteurs : Hearne, G. A. Mention d'édition : U. S. Geological survey Editeur : U. S. Geological Survey Année de publication : 1985 ISBN/ISSN/EAN : CI-05102 Note générale : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrogéologie  Géophysique  Simulation  Modélisation Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Note de contenu : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. U.S. Geological Survey Water Supply paper, 2206. Simulation of an aquifer test on the Tesuque Pueblo Grant, New Mexico [texte imprimé] / Hearne, G. A.  . -  U. S. Geological survey . - U. S. Geological Survey, 1985. ISSN : CI-05102 An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrogéologie  Géophysique  Simulation  Modélisation Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Note de contenu : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis.

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