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Measuring and modeling two-dimensional irrigation infiltration under film-mulched furrows

机译:覆膜沟下二维灌溉入渗量的测量与模拟

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摘要

Furrow irrigation with film-mulched agricultural beds is being promoted in the arid region of northwest China because it improves water utilization. Two-dimensional infiltration patterns under film-mulched furrows can provide guidelines and criteria for irrigation design and operation. Our objective was to investigate soil water dynamics during ponding irrigation infiltration of mulched furrows in a cross-sectional ridge-furrow configuration, using laboratory experiments and math-ematical simulations. Six experimental treatments, with two soil types (silt loam and sandy loam), were investigated to monitor the wetting patterns and soil water distribution in a cuboid soil chamber. Irrigation of mulched furrows clearly increased water lateral infiltration on ridge shoulders and ridges, due to enhancement of capillary driving force. Increases to both initial soil water content (SWC) and irrigation water level resulted in increased wetted soil volume. Empirical regression equations accurately estimated the wetted lateral distance (Rl) and downward distance (Rd) with elapsed time in a variably wetted soil medium. Optimization of model parameters followed by the Inverse approach resulted in satisfactory agreement between observed and predicted cumulative infiltration and SWC. On the basis of model calibration, HYDRUS-2D model can accurately simulate two-dimensional soil water dynamics under irrigation of mulched furrows. There were significant differences in wetting patterns between unmulched and mulched furrow irrigation using HYDRUS-2D simulation. The Rd under the mulched furrows was 32.14%less than the unmulched furrows. Therefore, film-mulched furrows are recommended in a furrow irrigation system.
机译:在中国西北的干旱地区,人们正在推广使用覆盖有农膜的沟灌,因为它可以提高水的利用率。覆膜沟下的二维入渗模式可以为灌溉设计和运行提供指导和标准。我们的目的是利用实验室实验和数学-数学模拟方法,研究在垄沟配置下,沟渠沟灌灌溉入渗过程中的土壤水分动态。研究了六种具有两种土壤类型(粉壤土和沙质壤土)的实验处理方法,以监测长方体土壤室内的湿润模式和土壤水分布。由于增加了毛细管驱动力,沟渠的灌溉明显增加了脊肩和脊上的水侧向渗透。初始土壤含水量(SWC)和灌溉水位的增加导致湿润土壤体积的增加。经验回归方程可准确估算随时间变化的湿润土壤介质中的湿润侧向距离(Rl)和向下距离(Rd)。通过逆方法进行模型参数的优化,可以在观测到的和预测的累积入渗与SWC之间取得令人满意的一致性。在模型标定的基础上,HYDRUS-2D模型可以准确地模拟沟灌条件下的二维土壤水动力学。使用HYDRUS-2D模拟进行的沟壑灌溉和沟壑灌溉之间的润湿模式存在显着差异。覆盖沟下的Rd比未覆盖沟少32.14%。因此,建议在沟灌系统中使用覆膜沟。

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  • 来源
    《寒旱区科学(英文版)》 |2016年第5期|419-431|共13页
  • 作者单位

    Linze Inland River Basin Research Station, Key Laboratory of Eco-hydrology of Inland River Basin, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Institute of Water Saving Agriculture in Arid Regions of China, Northwest A&F University, Yangling, Shaanxi 712100, China;

    Institute of Water Saving Agriculture in Arid Regions of China, Northwest A&F University, Yangling, Shaanxi 712100, China;

    Linze Inland River Basin Research Station, Key Laboratory of Eco-hydrology of Inland River Basin, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-19 03:41:29
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