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Dynamic Simulation of Soil Salt Transport in Arid Irrigation Areas under the HYDRUS-2D-Based Rotation Irrigation Mode

机译:基于HYDRUS-2D的旋转灌溉模式下干旱灌区土壤盐分运移的动态模拟。

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摘要

This research aims to explore the dynamic transport of water and salt in soil under different irrigation modes and disclose the desalting effect of different irrigation factors in inland arid irrigation areas. Jingdian Irrigation District in Gansu Province, which is located in the arid region of Northwest China, is selected as a typical experimental area. Soil water and salt dynamic migration model is constructed based on HYDRUS-2D software, and field irrigation experiments are designed according to actual irrigation conditions in crop growth period. The model is used to simulate the salt transport process between saturated soil and unsaturated soil as well as the effects of different irrigation quotas, irrigation rounds and quota allocations on soil desalting. Through simulation, the vertical movement pattern of water and salt in the soil of the test area is analyzed, and the optimal design of the soil desalting irrigation plan is carried out. The results demonstrate that: after two-round irrigation, the average soil salinity of the tillage layer at each test points decreases significantly under evapotranspiration; the infiltration of irrigation water has an obvious impact on soil desalting; the deviation between the simulated and the measured value is less than 0.5%, which proves the model fitting result reliable; with fixed irrigation cycle and times, the soil desalting efficiency is higher when the irrigation quota falls in the range of 4000 6000 m(3)/hm(2); when the first round of irrigation water only saturates the moisture content and gradually increases the irrigation quota in the subsequent rounds, it is more conducive to the dissolution and discharge of soil salinity. In summary, the results of this study can provide technical support for the protection of water and soil resources, as well as the improvement of saline-alkali land in inland arid irrigation areas.
机译:本研究旨在探讨不同灌溉方式下土壤中水和盐的动态运移,并揭示内陆干旱灌区不同灌溉因子的脱盐效果。位于中国西北干旱地区的甘肃省靖甸灌区被选为典型的试验区。基于HYDRUS-2D软件建立了土壤水盐动态迁移模型,并根据作物生长期的实际灌溉条件进行了田间灌溉试验。该模型用于模拟盐分在饱和土壤和非饱和土壤之间的迁移过程,以及不同灌溉定额,灌溉轮次和定额分配对土壤脱盐的影响。通过模拟,分析了试验区土壤中水盐的垂直运动规律,进行了土壤脱盐灌溉方案的优化设计。结果表明:经过两轮灌溉后,蒸散条件下各试验点耕作层的平均土壤盐分明显降低。灌溉水的渗透对土壤脱盐有明显的影响。模拟值与实测值的偏差小于0.5%,证明模型拟合结果可靠。在固定灌溉周期和灌溉时间的情况下,当灌溉限额在4000 6000 m(3)/ hm(2)范围内时,土壤脱盐效率更高;当第一轮灌溉水仅使含水量饱和并在随后的几轮中逐渐增加灌溉配额时,更有利于土壤盐分的溶解和排放。总之,本研究结果可为内陆干旱灌溉区的水土资源保护和盐碱地改良提供技术支持。

著录项

  • 来源
    《Water Resources Management》 |2019年第10期|3499-3512|共14页
  • 作者单位

    North China Univ Water Resources & Elect Power, Collaborat Innovat Ctr Water Resources Efficient, 136 Jinshui Rd, Zhengzhou 450045, Henan, Peoples R China;

    North China Univ Water Resources & Elect Power, Collaborat Innovat Ctr Water Resources Efficient, 136 Jinshui Rd, Zhengzhou 450045, Henan, Peoples R China;

    Dingshengxiang Pumps Ind Ltd Co, Zhengzhou, Liaoning, Peoples R China;

    North China Univ Water Resources & Elect Power, Collaborat Innovat Ctr Water Resources Efficient, 136 Jinshui Rd, Zhengzhou 450045, Henan, Peoples R China;

    North China Univ Water Resources & Elect Power, Collaborat Innovat Ctr Water Resources Efficient, 136 Jinshui Rd, Zhengzhou 450045, Henan, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Arid irrigation area; Rotation flow; HYDRUS-2D model; Water and salt movement; Desalination effect;

    机译:干旱灌溉面积;旋转流动;氢气-2D模型;水和盐运动;脱盐效果;

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