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...