双垄沟播喷灌垄沟膜孔界面水分分布特征
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S275.5

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国家自然科学基金项目“双垄沟播喷灌垄—沟—膜孔界面水分汇流入渗特征与作物生理响应机制”(51769002); 甘肃省科技计划项目“引大灌区主要经济作物节水灌溉制度研究与示范”(20YF3NA011)


Characteristics of Soil Water Distribution at Interface of a Double-Ridge and Furrow-Sowing Film Hole Under Sprinkler Irrigation
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    摘要:

    [目的] 分析河西内陆干旱区甘肃省民勤县双垄沟播喷灌条件下水量在垄—沟—膜孔界面汇流入渗特征,探索农业节水与耕作技术耦合的水量传输与利用关系研究的关键科学问题,为发展高效农业节水技术提供理论依据。[方法] 通过田间试验设置24 mm (G1),30 mm (G2),36 mm (G3),42 mm (G4)4个喷灌灌水定额处理,并通过HYDRUS-2D模型模拟了双垄沟播喷灌垄沟膜孔不同位置土壤水分的差异性和土壤水分二维分布特征。[结果] 基于HYDRUS-2D构建的双垄沟播喷灌垄沟膜孔土壤水分模型精度较高,平均相对误差为6.46%~9.08%,决定系数为0.85~0.95。土壤水分分布特征表现为灌水后1 d土壤饱和湿润区主要集中在0—30 cm土层,并且24 mm (G1)处理的饱和区面积最小,存在水分亏缺现象。在0—20 cm土层,30 mm (G2),36 mm (G3),42 mm (G4)处理的饱和区面积呈现随灌水量的增加而增加的规律。而在50 cm土层以下,不同处理含水率并无显著差异。[结论] 在河西内陆干旱地区喷灌农田,灌水主要对土壤上层产生影响;HYDRUS模型模拟效果较令人满意,参数较为可靠,在双垄沟播喷灌技术灌溉制度制定时可以参考。

    Abstract:

    [Objective] Water infiltration characteristics at the ridge, furrow, and film hole interface under furrow seeding and sprinkling irrigation on double ridges of inland area of Hexi Corridor at Minqin County, Gansu Province were determined, and the relationship between water transfer and the utilization of agricultural water-saving and farm technology coupling were discussed in order to provide a theoretical basis for the development of efficient agricultural water-saving technologies. [Methods] Four sprinkler irrigation treatments of 24 mm (G1), 30 mm (G2), 36 mm (G3), and 42 mm (G4) were established in a field experiment, and the HYDRUS-2D model was used to simulate the soil moisture at different positions of the double-ridge and furrow-sowing sprinkler irrigation ridge film hole. Differences and two-dimensional distribution characteristics of soil moisture were determined. [Results] The accuracy of the HYDRUS-2D model to simulate soil moisture for the sprinkler irrigated double-ridge and furrow-sowing system at the film hole was high (average relative error was 6.46%—9.08%, and the coefficient of determination was 0.85—0.95. One day after irrigation, the saturated and humid soil area was mainly concentrated in the 0—30 cm soil layer, and the saturated area of the G1 treatment was the smallest of all of the treatments due to water deficit. In the 0—20 cm soil layer, the saturated area increased with increasing irrigation amount (i.e., G234). However, there was no significant difference in water content between different treatments below the 50 cm soil depth. [Conclusion] Sprinkler irrigation of farmland at the inland arid area of Hexi Corridor mainly affected the upper soil layer. Simulations of soil water distribution by the HYDRUS-2D model were acceptable and the parameters were reliable. The model can be used to formulate sprinkler irrigation system technology for the double-ridge production system.

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王文娟,丁林.双垄沟播喷灌垄沟膜孔界面水分分布特征[J].水土保持通报,2022,42(5):181-186

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  • 收稿日期:2021-10-13
  • 最后修改日期:2022-03-20
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  • 在线发布日期: 2022-11-22
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