Technical Bulletin (ILWMR). Calculation of vertical moistuce flow in a soil body during evaporation, infiltration and redistribution / Kastanek, F.

Public ISBD Titre de série : Technical Bulletin (ILWMR) Titre : Calculation of vertical moistuce flow in a soil body during evaporation, infiltration and redistribution Type de document : texte imprimé Auteurs : Kastanek, F. Année de publication : 1973 ISBN/ISSN/EAN : CI-09957 Note générale : Water movement in soil is governed by two basic principles: the law of continuity, the law of resistance. Combination of these two principles gives a differential equation which can describe the movement of noisture in soils. With the aid of theoretical considerations it is possible to divide the soil profile into different zones, for each of which the boundary conditions can be defined. For each such zone one can calculate the distribution of noisture content and water potential using the law of continuity and the law of resistance in accordance with the boundary conditions... Langues : Anglais (eng) Mots-clés : Climatologie  Evaporation  Humidité  Infrastructure  Sol  Calcul de l'humidité Index. décimale : 551.6 Climatologie et temps Résumé : Water movement in soil is governed by two basic principles: the law of continuity, the law of resistance. Combination of these two principles gives a differential equation which can describe the movement of noisture in soils. With the aid of theoretical considerations it is possible to divide the soil profile into different zones, for each of which the boundary conditions can be defined. For each such zone one can calculate the distribution of noisture content and water potential using the law of continuity and the law of resistance in accordance with the boundary conditions... Note de contenu : Water movement in soil is governed by two basic principles: the law of continuity, the law of resistance. Combination of these two principles gives a differential equation which can describe the movement of noisture in soils. With the aid of theoretical considerations it is possible to divide the soil profile into different zones, for each of which the boundary conditions can be defined. For each such zone one can calculate the distribution of noisture content and water potential using the law of continuity and the law of resistance in accordance with the boundary conditions... Technical Bulletin (ILWMR). Calculation of vertical moistuce flow in a soil body during evaporation, infiltration and redistribution [texte imprimé] / Kastanek, F. . - 1973. ISSN : CI-09957 Water movement in soil is governed by two basic principles: the law of continuity, the law of resistance. Combination of these two principles gives a differential equation which can describe the movement of noisture in soils. With the aid of theoretical considerations it is possible to divide the soil profile into different zones, for each of which the boundary conditions can be defined. For each such zone one can calculate the distribution of noisture content and water potential using the law of continuity and the law of resistance in accordance with the boundary conditions... Langues : Anglais (eng) Mots-clés : Climatologie  Evaporation  Humidité  Infrastructure  Sol  Calcul de l'humidité Index. décimale : 551.6 Climatologie et temps Résumé : Water movement in soil is governed by two basic principles: the law of continuity, the law of resistance. Combination of these two principles gives a differential equation which can describe the movement of noisture in soils. With the aid of theoretical considerations it is possible to divide the soil profile into different zones, for each of which the boundary conditions can be defined. For each such zone one can calculate the distribution of noisture content and water potential using the law of continuity and the law of resistance in accordance with the boundary conditions... Note de contenu : Water movement in soil is governed by two basic principles: the law of continuity, the law of resistance. Combination of these two principles gives a differential equation which can describe the movement of noisture in soils. With the aid of theoretical considerations it is possible to divide the soil profile into different zones, for each of which the boundary conditions can be defined. For each such zone one can calculate the distribution of noisture content and water potential using the law of continuity and the law of resistance in accordance with the boundary conditions...

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