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Evaluating the Effects of Mulch and Irrigation Amount on Soil Water Distribution and Root Zone Water Balance Using HYDRUS-2D

机译:使用HYDRUS-2D评估覆盖和灌溉量对土壤水分分布和根区水平衡的影响

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Water scarcity is the most critical constraint for sustainable cotton production in Xinjiang Province, northwest China. Drip irrigation under mulch is a major water-saving irrigation method that has been widely practiced for cotton production in Xinjiang. The performance of such an irrigation system should be evaluated for proper design and management. Therefore, a field experiment and a simulation study were conducted to (1) determine a modeling approach that can be applied to manage drip irrigation under mulch for cotton production in this region; and (2) examine the effects of irrigation amount and mulch on soil water distribution and root zone water balance components. In the experiment, four irrigation treatments were used: T1, 166.5 m3; T2, 140.4 m3; T3, 115.4 m3; and T4: 102.3 m3. The HYDRUS-2D model was calibrated, validated, and applied with the data obtained in this experiment. Soil water balance in the 0–70 cm soil profile was simulated. Results indicate that the observed soil water content and the simulated results obtained with HYDRUS-2D are in good agreement. The radius of the wetting pattern, root water uptake, and evaporation decreased as the amount of irrigation was reduced from T1 to T4, while a lot of stored soil water in the root zone was utilized and a huge amount of water was recharged from the layer below 70 cm to compensate for the decrease in irrigation amount. Mulch significantly reduced evaporation by 11.7 mm and increased root water uptake by 11.2 mm. Our simulation study suggests that this model can be applied to provide assistance in designing drip irrigation systems and developing irrigation strategies.
机译:水资源短缺是中国西北部新疆省棉花可持续生产的最关键制约因素。地膜下滴灌是一种主要的节水灌溉方法,在新疆棉花生产中已广泛采用。应该评估这种灌溉系统的性能,以进行适当的设计和管理。因此,进行了田间试验和模拟研究,以(1)确定一种可用于管理该地区棉花覆盖下滴灌的建模方法; (2)研究灌溉量和覆盖对土壤水分分布和根区水分平衡组成的影响。在实验中,使用了四种灌溉处理方式:T1,166.5 m 3 ; T2,140.4 m 3 ; T3,115.4 m 3 ;和T4:102.3 m 3 。对HYDRUS-2D模型进行了校准,验证,并应用了该实验中获得的数据。模拟了0–70 cm土壤剖面中的土壤水分平衡。结果表明,HYDRUS-2D观测到的土壤含水量与模拟结果吻合良好。随着灌溉量从T1减少到T4,湿润模式的半径,根系水分吸收和蒸发减少,而在根系区域中利用了很多存储的土壤水,并且从该层补充了大量的水。低于70厘米以补偿灌溉量的减少。地膜覆盖使蒸发量减少了11.7毫米,根水吸收增加了11.2毫米。我们的模拟研究表明,该模型可用于设计滴灌系统和制定灌溉策略。

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