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Titre de série : Electrotechnique et normalisation (FR) Titre : Eléments d'automatismes Type de document : texte imprimé Auteurs : Ney, H. Mention d'édition : Nathan Editeur : Nathan Année de publication : 1985 ISBN/ISSN/EAN : 978-2-09-181341-7 Langues : Français (fre) Mots-clés : ELECTRICITE TECHNIQUE ELECTRONIQUE TECHNIQUE PNEUMATIQUE SYSTEME AUTOMATIQUE LOGIQUE BINEAIRE PROGRAMMATEUR ELECTROMECANIQUE Index. décimale : 537 Electricité et électronique : Classer ici l'électromagnétisme Electrotechnique et normalisation (FR). Eléments d'automatismes [texte imprimé] / Ney, H. . - Nathan . - Nathan, 1985.
ISBN : 978-2-09-181341-7
Langues : Français (fre)
Mots-clés : ELECTRICITE TECHNIQUE ELECTRONIQUE TECHNIQUE PNEUMATIQUE SYSTEME AUTOMATIQUE LOGIQUE BINEAIRE PROGRAMMATEUR ELECTROMECANIQUE Index. décimale : 537 Electricité et électronique : Classer ici l'électromagnétisme Réservation
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Code-barres Cote Support Localisation Section Disponibilité ER99B964.75699 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75700 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75701 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75702 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75703 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75704 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75705 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ER99B964.75706 ER 3964.2 $r non conforme -- Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76291 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76292 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76293 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76294 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76295 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76296 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76297 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible ET99B738.76298 ET ENER(54) Monographie Bibliothèque CDI-Kamboinsé Fond documentaire Disponible Verspreide overdrukken - Miscillaneous Reprints, 222. Theory and system of automatic determination of soil moisture characteristics and unsaturated hudraulic conductivities / Boels, D.
Titre de série : Verspreide overdrukken - Miscillaneous Reprints, 222 Titre : Theory and system of automatic determination of soil moisture characteristics and unsaturated hudraulic conductivities Type de document : texte imprimé Auteurs : Boels, D. ; Van Gils, BHM ; Wit, K. E. Mention d'édition : IWC Editeur : IWC Année de publication : 1978 ISBN/ISSN/EAN : CI-03699 Note générale : This moisture characteristic and the unsatured hydraulic conductivy are calculated from the measured water pressures at different depths in a soil core and the weights during evaporation at the top of thecore the mesured water presure is assumed to represent the mean preasure to be described with sufficient accuracy by a polynon in each pressure interval is solved from a set of equations. Assuming the hydraulic conductivity - water pressure relation ship can be described by an exponentiol relationship with varying constants in the different pressure at two deppths and three sequential moments, and the rate of change in water content below some definde depth in the core during two sequential time periods. In the satured conductivity is relatively hight, a steady-state infiltartion method is applied to determine the unsaturated hydraulic conductivity at high water Langues : Anglais (eng) Mots-clés : Methodologie Infiltration Hydraulique Eau Evaporation Humidité SOL Pédologie Système automatique Théorie Index. décimale : 621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique Résumé : This moisture characteristic and the unsatured hydraulic conductivy are calculated from the measured water pressures at different depths in a soil core and the weights during evaporation at the top of thecore the mesured water presure is assumed to represent the mean preasure to be described with sufficient accuracy by a polynon in each pressure interval is solved from a set of equations. Assuming the hydraulic conductivity - water pressure relation ship can be described by an exponentiol relationship with varying constants in the different pressure at two deppths and three sequential moments, and the rate of change in water content below some definde depth in the core during two sequential time periods. In the satured conductivity is relatively hight, a steady-state infiltartion method is applied to determine the unsaturated hydraulic conductivity at high water Note de contenu : This moisture characteristic and the unsatured hydraulic conductivy are calculated from the measured water pressures at different depths in a soil core and the weights during evaporation at the top of thecore the mesured water presure is assumed to represent the mean preasure to be described with sufficient accuracy by a polynon in each pressure interval is solved from a set of equations. Assuming the hydraulic conductivity - water pressure relation ship can be described by an exponentiol relationship with varying constants in the different pressure at two deppths and three sequential moments, and the rate of change in water content below some definde depth in the core during two sequential time periods. In the satured conductivity is relatively hight, a steady-state infiltartion method is applied to determine the unsaturated hydraulic conductivity at high water Verspreide overdrukken - Miscillaneous Reprints, 222. Theory and system of automatic determination of soil moisture characteristics and unsaturated hudraulic conductivities [texte imprimé] / Boels, D. ; Van Gils, BHM ; Wit, K. E. . - IWC . - IWC, 1978.
ISSN : CI-03699
This moisture characteristic and the unsatured hydraulic conductivy are calculated from the measured water pressures at different depths in a soil core and the weights during evaporation at the top of thecore the mesured water presure is assumed to represent the mean preasure to be described with sufficient accuracy by a polynon in each pressure interval is solved from a set of equations. Assuming the hydraulic conductivity - water pressure relation ship can be described by an exponentiol relationship with varying constants in the different pressure at two deppths and three sequential moments, and the rate of change in water content below some definde depth in the core during two sequential time periods. In the satured conductivity is relatively hight, a steady-state infiltartion method is applied to determine the unsaturated hydraulic conductivity at high water
Langues : Anglais (eng)
Mots-clés : Methodologie Infiltration Hydraulique Eau Evaporation Humidité SOL Pédologie Système automatique Théorie Index. décimale : 621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique Résumé : This moisture characteristic and the unsatured hydraulic conductivy are calculated from the measured water pressures at different depths in a soil core and the weights during evaporation at the top of thecore the mesured water presure is assumed to represent the mean preasure to be described with sufficient accuracy by a polynon in each pressure interval is solved from a set of equations. Assuming the hydraulic conductivity - water pressure relation ship can be described by an exponentiol relationship with varying constants in the different pressure at two deppths and three sequential moments, and the rate of change in water content below some definde depth in the core during two sequential time periods. In the satured conductivity is relatively hight, a steady-state infiltartion method is applied to determine the unsaturated hydraulic conductivity at high water Note de contenu : This moisture characteristic and the unsatured hydraulic conductivy are calculated from the measured water pressures at different depths in a soil core and the weights during evaporation at the top of thecore the mesured water presure is assumed to represent the mean preasure to be described with sufficient accuracy by a polynon in each pressure interval is solved from a set of equations. Assuming the hydraulic conductivity - water pressure relation ship can be described by an exponentiol relationship with varying constants in the different pressure at two deppths and three sequential moments, and the rate of change in water content below some definde depth in the core during two sequential time periods. In the satured conductivity is relatively hight, a steady-state infiltartion method is applied to determine the unsaturated hydraulic conductivity at high water Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B699.108058 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108056 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108057 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108055 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108053 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108054 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108052 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B699.108051 CI-03699 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible