Titre :	Simulation of the water balance of arable land and pastures
Type de document :	texte imprimé
Auteurs :	Makkink, G. F. ; Van Heemst, H. D. J.
Mention d'édition :	Centre for Agricultural Publishing and Documentation
Editeur :	Centre for Agricultural Publishing and Documentation
Année de publication :	1975
ISBN/ISSN/EAN :	978-90-220-0566-8
Note générale :	This book describes a simulation model for the water balance of areas where the groundwater may be within the reach of the crop, directly or by means of capillary rise. The computation is based on macrometeorological data, the physical proporties of the soil, the hydrological situation of the field and some pertinent data on the crop cover through out the year. For two areas, the rottegats polder (clay soil) and the leerinkbeek region (sandy soil) the simulation was validated by comparing simulated and observed results. The computer program is written in FORTRAN.
Langues :	Anglais (eng)
Mots-clés :	Ressource en eau  Simulation  Pâturage  Terre agricole  Bilan hydrique  Humidité  Evaporation  Hydrologie  Informatique  Besoin en eau des plantes
Index. décimale :	551.48 Hydrologie :
Résumé :	This book describes a simulation model for the water balance of areas where the groundwater may be within the reach of the crop, directly or by means of capillary rise. The computation is based on macrometeorological data, the physical proporties of the soil, the hydrological situation of the field and some pertinent data on the crop cover through out the year. For two areas, the rottegats polder (clay soil) and the leerinkbeek region (sandy soil) the simulation was validated by comparing simulated and observed results. The computer program is written in FORTRAN.
Note de contenu :	This book describes a simulation model for the water balance of areas where the groundwater may be within the reach of the crop, directly or by means of capillary rise. The computation is based on macrometeorological data, the physical proporties of the soil, the hydrological situation of the field and some pertinent data on the crop cover through out the year. For two areas, the rottegats polder (clay soil) and the leerinkbeek region (sandy soil) the simulation was validated by comparing simulated and observed results. The computer program is written in FORTRAN.

Simulation of the water balance of arable land and pastures [texte imprimé] / Makkink, G. F. ; Van Heemst, H. D. J.  . -  Centre for Agricultural Publishing and Documentation . - Centre for Agricultural Publishing and Documentation, 1975.
ISBN : 978-90-220-0566-8
This book describes a simulation model for the water balance of areas where the groundwater may be within the reach of the crop, directly or by means of capillary rise. The computation is based on macrometeorological data, the physical proporties of the soil, the hydrological situation of the field and some pertinent data on the crop cover through out the year. For two areas, the rottegats polder (clay soil) and the leerinkbeek region (sandy soil) the simulation was validated by comparing simulated and observed results. The computer program is written in FORTRAN.
Langues : Anglais (eng)

Mots-clés :	Ressource en eau  Simulation  Pâturage  Terre agricole  Bilan hydrique  Humidité  Evaporation  Hydrologie  Informatique  Besoin en eau des plantes
Index. décimale :	551.48 Hydrologie :
Résumé :	This book describes a simulation model for the water balance of areas where the groundwater may be within the reach of the crop, directly or by means of capillary rise. The computation is based on macrometeorological data, the physical proporties of the soil, the hydrological situation of the field and some pertinent data on the crop cover through out the year. For two areas, the rottegats polder (clay soil) and the leerinkbeek region (sandy soil) the simulation was validated by comparing simulated and observed results. The computer program is written in FORTRAN.
Note de contenu :	This book describes a simulation model for the water balance of areas where the groundwater may be within the reach of the crop, directly or by means of capillary rise. The computation is based on macrometeorological data, the physical proporties of the soil, the hydrological situation of the field and some pertinent data on the crop cover through out the year. For two areas, the rottegats polder (clay soil) and the leerinkbeek region (sandy soil) the simulation was validated by comparing simulated and observed results. The computer program is written in FORTRAN.