磁化水滴灌对盐碱化农田土壤水盐及离子分布的影响
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李国苗(1998-),女,硕士研究生,主要从事盐渍化土壤水盐养分动态研究。E-mail:1368353396@qq.com

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S156.4

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国家自然科学基金项目(52369009);内蒙古自然科学基金项目(2023MS05024);盐碱地生态修复与节水减排控盐关键技术研究学科项目(YLXKZX-NND052)


Effects of Magnetized Water Drip Irrigation on Soil Water, Salt and Ion Distribution in Saline-Alkali Farmland
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    摘要:

    [目的]为探讨不同灌溉水源滴灌条件下磁化强度对土壤水盐运移规律的影响,明确适宜的磁场强度。[方法]于2023年5月至2024年10月在达拉特旗进行田间试验。设置2种灌溉水源(黄河水F、微咸水B)和4种磁化梯度(M)(0.5 T、0.3 T、0.1 T、0 T),探究不同处理对土壤水盐动态、盐分淋洗及离子迁移规律的影响机制。[结果]磁化水滴灌显著提高根层土壤水分体积分数,促进盐分淋溶,缓解作物根层水盐胁迫,并有效降低土壤中Cl-、SO42-和Na+的质量分数。在不同磁化强度条件下,FM处理和BM处理表现出显著差异,其中磁场强度为0.3 T时,FM3、BM3处理根层土壤体积含水率和脱盐率较FM0、BM0分别提高3.03%~3.35%、1.58%~3.16%和8.83%~14.56%、7.07%~13.62%,同时,对土壤Cl-和Na+的脱除效果较好,FM3处理脱除率分别达19.17%~31.67%、33.95%~42.91%,BM3处理分别为5.20%~21.03%、20.41%~26.02%。磁化强度为0.5 T时,SO42-的脱除率最高,FM5和BM5分别为30.97%~35.22%、25.81%~26.02%。磁化水滴灌有效减少土壤水盐胁迫面积,在改善土壤水盐环境方面具有潜力。通过拟合分析表明,0.29~0.38 T为优化根层水盐环境的适宜磁场区间。综上所述,2种灌溉水源磁化后滴灌均可提高根层土壤水分体积分数,促进盐分淋溶。[结论]磁化水滴灌显著改善根区土壤水盐环境,0.3~0.4 T为沿黄灌区重度盐碱化农田最适宜的磁化强度,研究结果可为沿黄灌区盐碱地改良和水资源的高效利用提供理论依据支撑。

    Abstract:

    [Objective] To investigate the effects of magnetic field intensity on the movement patterns of soil water and salt under drip irrigation with different water sources, and to determine the optimal magnetic field strength. [Methods] A field experiment was conducted from May 2023 to October 2024 in Dalate Banner. The experiment included two types of irrigation water sources(Yellow River water [F] and slightly saline water [B]) and four levels of magnetic field intensity(M)(0.5 T, 0.3 T, 0.1 T and 0 T). The study examined the mechanisms by which different treatments affect soil water and salt dynamics, salt leaching and ion migration. [Results] Magnetized water drip irrigation significantly increased the soil volumetric water content in the crop root zone, promoted salt leaching, alleviated water-salt stress in the root zone, and effectively reduced the mass fractions of Cl-, SO42-and Na+ in the soil. Under different magnetic intensities, FM and BM treatments showed significant differences. When the magnetic field intensity was 0.3 T, the root-zone soil volumetric water content of FM3 and BM3 treatments increased by 3.03%-3.35% and 1.58%-3.16%, respectively, and the desalination rates increased by 8.83%-14.56% and 7.07%-13.62%, respectively, compared with FM0 and BM0. These treatments also achieved better Cl-and Na+ removal, with FM3 showing removal rates of 19.17%-31.67% and 33.95%-42.91%, and BM3 achieving 5.20%-21.03% and 20.41%-26.02%, respectively. When the magnetic field intensity was 0.5 T, SO42-removal was most effective, with FM5 and BM5 reaching 30.97%-35.22% and 25.81%-26.02%, respectively. In addition, magnetized water drip irrigation effectively reduced areas affected by soil water-salt stress and showed potential in improving the soil water-salt environment. Fitting analysis indicated that a magnetic field range of 0.29-0.38 T was optimal for improving the root-zone water-salt environment. Drip irrigation with magnetized water using both irrigation sources can enhance root-zone soil moisture and promote salt leaching. [Conclusion] Magnetized water drip irrigation significantly improves the root-zone soil water-salt environment. A magnetic field strength of 0.3-0.4 T is optimal for highly saline-alkali farmland in the Yellow River irrigation area. These findings provide theoretical support for improving saline-alkali land and the efficient utilization of water resources in the Yellow River irrigation area.

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李国苗, 刘霞, 王丽萍, 屈忠义, 李响, 乔天, 于函宏, 赵靖怡.磁化水滴灌对盐碱化农田土壤水盐及离子分布的影响[J].水土保持学报,2025,39(4):187~197

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  • 收稿日期:2025-03-18
  • 最后修改日期:2025-05-05
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  • 在线发布日期: 2025-09-10
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