Irrigation recommendation in a semi-arid drip-irrigated artichoke orchard using a one-dimensional monthly transient-state model

详细信息    查看全文

• 作者：Fernando Visconti^a ; ^{fernando.visconti@uv.es" class="auth_mail} ; José ; Miguel de Paz^a ; Delfina Martí ; nez^b ; Mª ; José ; Molina^b
• 关键词：Dd ; soil water downward flux below depth d ; EC25 ; electrical conductivity at 25  ; ° ; C ; ECe ; electrical conductivity at 25  ; ° ; C in the saturation extract ; ET0 ; reference evapotranspiration ; ETa ; actual evapotranspiration ; ETc ; crop evapotranspiration ; Fc ; maximum canopy ground cover ; Fc ; m ; canopy ground cover in month m ; fW ; fraction of soil area wetted by irrigation ; I ; irrigation amount ; If ; number of irrigation days ; IA ; index of agreeement ; Kcbmax ; maximum basal crop coefficient
• 刊名：Agricultural Water Management
• 出版年：31 May, 2014
• 年：2014
• 卷：138
• 期：Complete
• 页码：26-36
• 全文大小：2291 K

文摘

Irrigation in semi-arid areas can be optimally scheduled using models that maximize accuracy while minimizing data requirements. In this work, the validation of the one-dimensional transient-state SALTIRSOIL_M model able to monthly simulate the soil water content (胃), downward water flux (D), and the electrical conductivity in the saturation extract (ECe) is presented. The 胃 and the ECe were monthly monitored at 15 and 45 cm depth in a plot in commercial production of globe artichoke under semi-arid climate and drip-irrigation in SE Spain during the 2011-2012 growing season. Data on water quality, weather, irrigation management, crop development and soil were also collected and used to simulate the 胃, D, and ECe throughout the growing season at both depths with the SALTIRSOIL_M model. Reference and simulations of 胃 and D reasonably agreed with one another at both depths. ECe at 45 cm depth was estimated correctly enough by the model but was underestimated at 15 cm depth. The higher concentrations of nitrate, potassium, and hence other cations, which were observed at 15 cm as a consequence of fertilization could explain this. The model was subsequently used to estimate the optimum water management in the plot. Use of 325-450 mm yr^鈭? instead of 694 mm yr^鈭?, and by means of evenly distributed pulse irrigations instead of continuous ones, would have met the crop evapotranspiration requirements while avoiding excessive drainage, and maintaining soil salinity well below damaging values.