不同改良措施对重盐碱地夹层土壤的脱盐效果分析
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新疆水利水电科学研究院

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新疆维吾尔自治区重大科技计划项目(2022A02007-3)、国家重点研发计划项目(2021YFD1900805-04、2021YFD1900803-02)、新疆天山英才领军人才培养项目(2022TSYCLJ0069)


Analysis of desalination effect of different improvement measures on interlayer soil of heavy saline alkali soil
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    摘要:

    针对现有重盐碱地改良措施中工程量大与生产成本高的现实问题,以渭干河灌区规模化高效节水建设后经集中连片形成的大面积重盐碱地夹层土壤为研究对象,通过大田小区试验,研究不同措施在冬灌条件下的土壤水盐变化规律,分析显示:各处理在灌前和灌后除G1处理外均在夹层位置处60 cm~80 cm的土壤含水率最大,3次灌后,CK处理在60 cm~80 cm土壤含水率比其它处理高出1.4%~16.2%,在0~100 cm土壤平均含水率比其它处理高出2.3%~15.5%。同时,CK处理在60 cm~80 cm土壤含盐量最高,且脱盐率较低,3次灌后脱盐率为24.9%,仅高于G4处理(14.9%)。各措施处理中,G1处理脱盐率最高,为75.9%,其次是G6和G3处理,分别为51.5%和39.4%,G2和G5比较接近,分别为38.2%和37.4%,G4最低,为33.9%。通过2次和3次冬灌后,各处理脱盐效果明显,尤其在0~20 cm土层,分别由2020年灌前的7.06 g/kg~11.61 g/kg降到2022年灌后的2.0 g/kg~5.91 g/kg,脱盐率在76.8%~382.5%%之间,使表层土壤由初始的中重度盐碱土改良为轻中度盐碱土,并拟合出盐分增量与含水率增量成反比的关系,研究结果不仅反映出粘土夹层对水盐运移的阻滞作用,也表明通过改良措施可促进土壤水分下渗并提高土壤脱盐效果,可为重盐碱地夹层土壤改良措施的选择提供数据支撑。

    Abstract:

    In view of the practical problems of large quantities and high production cost in the existing heavy saline alkali land improvement measures, taking the large-scale heavy saline alkali land interlayer soil formed after the large-scale, efficient and water-saving construction of Weigan River irrigation area as the research object, through the field plot test, the soil water and salt change law of different measures under winter irrigation conditions is studied. Analysis shows that all treatments, except for G1 treatment, have the highest soil moisture content at the interlayer position of 60 cm to 80 cm before and after irrigation. After three rounds of irrigation, the soil moisture content of CK treatment at 60 cm to 80 cm is 1.4% to 16.2% higher than other treatments, and the average soil moisture content at 0-100 cm is 2.3% to 15.5% higher than other treatments. At the same time, CK treatment had the highest salt content in the soil between 60 cm and 80 cm, and the desalination rate was low. After three rounds of irrigation, the desalination rate was 24.9%, only higher than G4 treatment (14.9%). Among all measures, G1 treatment had the highest desalination rate at 75.9%, followed by G6 and G3 treatments at 51.5% and 39.4%, respectively. G2 and G5 were relatively close at 38.2% and 37.4%, respectively. G4 had the lowest desalination rate at 33.9%. After two and three winter irrigations, the desalination effect of each treatment was significant, especially in the 0-20 cm soil layer, which decreased from 7.06 g/kg to 11.61 g/kg before irrigation in 2020 to 2.0 g/kg to 5.91 g/kg after irrigation in 2022. The desalination rate was between 76.8% and 382.5%, which improved the surface soil from the initial medium to moderate saline alkali soil to light to moderate saline alkali soil. The relationship between the increase in salt content and the increase in water content was inversely proportional, The research results not only reflect the blocking effect of clay interlayer on water and salt transport, but also indicate that improvement measures can promote soil water infiltration and improve soil desalination efficiency, providing data support for the selection of soil improvement measures in heavy saline alkali soil interlayer.

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  • 收稿日期:2024-06-25
  • 最后修改日期:2024-10-06
  • 录用日期:2025-01-23
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