Technical Bulletins (New series), 7. Unsaturated zone and evapotranspiration / Bakel, P.J. T. (Van)

Public ISBD Titre de série : Technical Bulletins (New series), 7 Titre : Unsaturated zone and evapotranspiration Type de document : texte imprimé Auteurs : Bakel, P.J. T. (Van) Mention d'édition : Institute for Land and water Management Research Editeur : Institute for Land and water Management Research Année de publication : 1981 ISBN/ISSN/EAN : CI-04949 Note générale : This paper mainly deals with the hydrological precesses in the unsaturated zone. Firstly the most relevant theory concuring this zone is given. The saturated groundwater system and the atmospheric sustem constitute the boundaries of the unsatured zone. The relationship between these three system are discussed in short. An important issue is the mathematical description of water updake by plnt roots. Only the most common methods to quantifly this uptake are treated. An overview of the various categories of methods available to evaluate effects of changes in soil water conditions on evapotranspiration is presented - The probelms encountered in proctice mostly relate to the translation of model results to fiels situations. The various aspects with respect to this problem are discussed. Finally conclusions and recommendations are made. Langues : Anglais (eng) Mots-clés : Evapotranspiration  Eau souterraine  Physique du sol  Modèle mathématique Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : This paper mainly deals with the hydrological precesses in the unsaturated zone. Firstly the most relevant theory concuring this zone is given. The saturated groundwater system and the atmospheric sustem constitute the boundaries of the unsatured zone. The relationship between these three system are discussed in short. An important issue is the mathematical description of water updake by plnt roots. Only the most common methods to quantifly this uptake are treated. An overview of the various categories of methods available to evaluate effects of changes in soil water conditions on evapotranspiration is presented - The probelms encountered in proctice mostly relate to the translation of model results to fiels situations. The various aspects with respect to this problem are discussed. Finally conclusions and recommendations are made. Note de contenu : This paper mainly deals with the hydrological precesses in the unsaturated zone. Firstly the most relevant theory concuring this zone is given. The saturated groundwater system and the atmospheric sustem constitute the boundaries of the unsatured zone. The relationship between these three system are discussed in short. An important issue is the mathematical description of water updake by plnt roots. Only the most common methods to quantifly this uptake are treated. An overview of the various categories of methods available to evaluate effects of changes in soil water conditions on evapotranspiration is presented - The probelms encountered in proctice mostly relate to the translation of model results to fiels situations. The various aspects with respect to this problem are discussed. Finally conclusions and recommendations are made. Technical Bulletins (New series), 7. Unsaturated zone and evapotranspiration [texte imprimé] / Bakel, P.J. T. (Van)  . -  Institute for Land and water Management Research . - Institute for Land and water Management Research, 1981. ISSN : CI-04949 This paper mainly deals with the hydrological precesses in the unsaturated zone. Firstly the most relevant theory concuring this zone is given. The saturated groundwater system and the atmospheric sustem constitute the boundaries of the unsatured zone. The relationship between these three system are discussed in short. An important issue is the mathematical description of water updake by plnt roots. Only the most common methods to quantifly this uptake are treated. An overview of the various categories of methods available to evaluate effects of changes in soil water conditions on evapotranspiration is presented - The probelms encountered in proctice mostly relate to the translation of model results to fiels situations. The various aspects with respect to this problem are discussed. Finally conclusions and recommendations are made. Langues : Anglais (eng) Mots-clés : Evapotranspiration  Eau souterraine  Physique du sol  Modèle mathématique Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : This paper mainly deals with the hydrological precesses in the unsaturated zone. Firstly the most relevant theory concuring this zone is given. The saturated groundwater system and the atmospheric sustem constitute the boundaries of the unsatured zone. The relationship between these three system are discussed in short. An important issue is the mathematical description of water updake by plnt roots. Only the most common methods to quantifly this uptake are treated. An overview of the various categories of methods available to evaluate effects of changes in soil water conditions on evapotranspiration is presented - The probelms encountered in proctice mostly relate to the translation of model results to fiels situations. The various aspects with respect to this problem are discussed. Finally conclusions and recommendations are made. Note de contenu : This paper mainly deals with the hydrological precesses in the unsaturated zone. Firstly the most relevant theory concuring this zone is given. The saturated groundwater system and the atmospheric sustem constitute the boundaries of the unsatured zone. The relationship between these three system are discussed in short. An important issue is the mathematical description of water updake by plnt roots. Only the most common methods to quantifly this uptake are treated. An overview of the various categories of methods available to evaluate effects of changes in soil water conditions on evapotranspiration is presented - The probelms encountered in proctice mostly relate to the translation of model results to fiels situations. The various aspects with respect to this problem are discussed. Finally conclusions and recommendations are made.

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