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RESEARCH PRODUCT
Improvement of FAO-56 Model to Estimate Transpiration Fluxes of Drought Tolerant Crops under Soil Water Deficit: Application for Olive Groves
Juan Manzano JuarezGiuseppe ProvenzanoGiorgio BaiamonteGiovanni Rallosubject
Hydrological modellingDrought toleranceAmendmentFAO-56 agro-hydrological model Water stress function Water uptake ability Table olive orchards Midday stem water potential Relative transpirationMidday stem water potentialCropSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliRelative transpiration.Energy exchangeWater Science and TechnologyCivil and Structural EngineeringTranspirationWater stress functionHydrologybusiness.industryRelative transpirationFAO-56 agro-hydrological modelTable olive orchardsAgricultural and Biological Sciences (miscellaneous)Water uptake abilityRelative transpiration; Midday stem water potential; Table olive orchards; FAO-56 agro-hydrological modelAgricultureSoil waterEnvironmental scienceINGENIERIA AGROFORESTALbusinessdescription
[EN] Agro-hydrological models are considered an economic and simple tool for quantifying crop water requirements. In the last two decades, agro-hydrological physically based models have been developed to simulate mass and energy exchange processes in the soil-plant-atmosphere system. Although very reliable, because of the high number of required variables, simplified models have been proposed to quantify crop water consumes. The main aim of this paper is to propose an amendment of the Food and Agricultural Organization (FAO) of the United Nations FAO-56 spreadsheet program to introduce a more realistic shape of the stress function, valid for mature olive orchards (Olea europaea L.). The modified model is successively validated by means of the comparison between measured and simulated soil water contents and actual transpiration fluxes. These outputs are finally compared with those obtained with the original version of the model. Experiments also allowed assessing the ability of simulated crop water stress coefficients to explain the actual water stress conditions evaluated on the basis of measured relative transpirations and midday stem water potentials. The results show that the modified model significantly improves the estimation of actual crop transpiration fluxes and soil water contents under soil water deficit conditions, according to the RMSEs associated with the revised model, resulting in significantly higher than the corresponding values obtained with the original version. (C) 2014 American Society of Civil Engineers.
| year | journal | country | edition | language |
|---|---|---|---|---|
| 2014-09-01 |