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Water balance simulation of a dryland soil during fallow under conventional and conservation tillage in semiarid Aragon, Northeast Spain

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dc.creator Moret-Fernández, David
dc.creator Braud, Isabelle
dc.creator Arrúe Ugarte, José Luis
dc.date 2008-06-12T10:48:45Z
dc.date 2008-06-12T10:48:45Z
dc.date 2007-01
dc.date.accessioned 2017-01-31T01:40:12Z
dc.date.available 2017-01-31T01:40:12Z
dc.identifier Soil and Tillage Research, Volume 92, Issues 1-2, January 2007, Pages 251-263
dc.identifier 0167-1987
dc.identifier http://hdl.handle.net/10261/5030
dc.identifier 10.1016/j.still.2006.03.012
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/5030
dc.description The definitive version is available at: http://www.sciencedirect.com/science/journal/01671987
dc.description In Central Aragon, winter cereal is sown in the autumn (November–December), commonly after a 16–18 months fallow period aimed at conserving soil water. This paper uses the Simple Soil–Plant–Atmosphere Transfer (SiSPAT) model, in conjunction with field data, to study the effect of long fallowing on the soil water balance under three tillage management systems (conventional tillage, CT; reduced tillage, RT; and no-tillage, NT). This was on the assumption that soil properties would remain unchanged during the entire fallow season. Once the model was validated with data obtained before primary tillage implementation, the differences between simulated and observed soil water losses for the CT and RT treatments could be interpreted as the direct effect of the soil tillage system. The model was calibrated and validated in a long-term tillage experiment using data from three contrasting long-fallow seasons over the period 1999–2002, where special attention was paid to predicting soil hydraulic properties in the pre-tillage conditions. The capacity of the model to simulate the soil water balance and its components over long fallowing was demonstrated. Both the fallow rainfall pattern and the tillage management system affected the soil water budget and components predicted by the model. The model predicted that about 81% of fallow seasonal rainfall is lost by evaporation in long-fallow periods with both a dry autumn in the first year of fallow and a rainfall above normal in spring. Whereas, when the fallow season is characterised by a wet autumn during the first year of fallow the model predicted a decrease in soil water evaporation and an increase in water storage and deep drainage components. In this case, the predicted water lost by evaporation was higher under NT (64%) than under RT (56%) and CT (44%). The comparison between measured and simulated soil water loss showed that the practice of tillage decreased soil water conservation in the short term. The long-term analysis of the soil water balance showed that, in fallow periods with a wet autumn during the first year of fallow, the soil water loss measured under CT and RT was moderately greater than that predicted by the model.
dc.description This research was supported by the Comisión Interministerial de Ciencia y Tecnología of Spain (grants AGF98-0261-CO2-02 and AGL2001-2238-CO2-01 and PNFPI pre-doctoral fellowship awarded to the first author) and the European Union (FEDER funds).
dc.description Peer reviewed
dc.format 454211 bytes
dc.format application/pdf
dc.language eng
dc.publisher Elsevier
dc.rights openAccess
dc.subject Water balance
dc.subject Modelling
dc.subject Soil water conservation
dc.subject Tillage management
dc.subject Long-fallowing
dc.title Water balance simulation of a dryland soil during fallow under conventional and conservation tillage in semiarid Aragon, Northeast Spain
dc.type Artículo

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