Simulação da dinâmica da água em dois solos regados

• DOI: 10.19084/rca.15846
• Publication Date: 2010-01-01
• Authors: Barão, L.; Leitão, P. Chambel; Braunschweig, F.; Neves, R. J.; Gonçalves, M. C.; Ramos, T. B.; Castanheira, N. L.
• Keywords: model soil water content; teor de água no solo; crescimento de plantas; Modelo; 15. Life on land; crop growth; propriedades hidráulicas; 6. Clean water; hydraulic properties

Simulation results for water content dis­tribution obtained with HYDRUS, RZWQM and MOHIDLAND models were compared with field data. These models differ mainly in calculating root water uptake and computing crop water requirements. Simulations were carried out in different horizons of an Hortic An­throsol and an Eutric Fluviosol, located in the Alentejo region (Portugal). Soil water content was measured, with a TDR sys­tem at different depths. Soil hydraulic properties were determined in the labora­tory, and described in HYDRUS and MOHIDLAND with the Mualem-van Genuchten, and in RZWQM with the modified Brooks and Corey equations. Reference evapotranspiration was calcu­lated with the Penman-Monteith and the Shuttleworth-Wallace method using at­mospheric data from the meteorological stations located near the field plots. Parti­tion between transpiration and evapora­tion was calculated using the Leaf Area Index values, and the RZWQM crop module. Results show a good agreement between model simulations and field measurements for the three models.<br/>Revista de Ciências Agrárias, vol. 33 n.º 1 (2010)<br/>