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基于SHAW模型的南疆典型棉田适宜冬春灌盐分淋洗策略

Appropriate Winter and Spring Irrigations for Salt Leaching in Typical Cotton Field of Southern Xinjiang Based on SHAW Model

  • 摘要: 为探究南疆地区棉田休闲期土壤水热盐运移过程及适宜的冬春灌盐分淋洗策略,基于当地棉田测坑连续两年作物休闲期(2019—2020年、2020—2021年)0~80 cm的土壤水、热、盐监测数据,对SHAW模型进行率定和验证;并设置64个冬春灌情景,包括8个冬灌定额(0、600、1 200、1 800、2 400、2 700、3 000、3 600 m3/hm2)和8个春灌定额(0、300、600、900、1 200、1 800、2 100、2 400 m3/hm2),进一步模拟了不同冬春灌组合模式下休闲期的土壤水热盐运移规律。结果表明:SHAW模型能够较可靠地模拟南疆地区休闲期冻融土壤水热盐运移规律。其中,土壤温度的模拟精度最高,不同土壤深度R2均不小于0.95;而土壤含水率和含盐量受到土壤水分相变的影响导致模拟精度稍差,最小R2分别为0.61和0.73。不同冬灌处理在冻结期未冻水含量大幅降低,冬灌定额越大的处理,未冻水含量越少。冬灌水量越大,冻结期表层土壤温度变化幅度越小,且至融化期土壤增温缓慢,但春灌后不同处理的温度差别减小。土壤表层含盐量在灌水后显著降低,而在冻结过程中出现明显的上升现象,且深层土壤盐分上升明显滞后于表层土壤。土壤冻结水融化后对表层土壤盐分进行了二次淋洗,因此补充少量的春灌便可显著降低土壤表层含盐量,满足棉花出苗期的盐分要求。综合考虑南疆地区水资源现状及不同冬春灌组合模式对播前土壤水热盐的影响,推荐采用的节水灌溉模式为冬灌+少量春灌造墒,适宜灌水定额为冬灌2 250 m3/hm2、春灌300 m3/hm2。提出的冬春灌组合盐分淋洗模式可为南疆地区农业水资源可持续利用和土壤次生盐渍化治理提供理论依据。

     

    Abstract: In order to understand the mechanism of soil moisture, heat and salt migration and explore the optimal strategy of combined winter and spring irrigations in the cotton field of Southern Xinjiang during fallow season, the SHAW model was calibrated and verified by using monitored soil moisture, heat and salt data of 0~80 cm soil in the cotton test pits during two fallow seasons(2019—2020 and 2020—2021). Then 64 scenarios with eight winter irrigation treatments(0 m/hm~2, 600 m/hm~2, 1 200 m/hm~2, 1 800 m/hm~2, 2 400 m/hm~2, 2 700 m/hm~2, 3 000 m/hm~2 and 3 600 m/hm~2) and eight spring irrigation treatments(0 m~3/hm~2, 300 m~3/hm~2, 600 m~3/hm~2, 900 m~3/hm~2, 1 200 m~3/hm~2, 1 800 m~3/hm~2, 2 100 m~3/hm~2 and 2 400 m~3/hm~2) were simulated by SHAW to investigate the soil moisture, heat and salt transport behavior in fallow season under different winter and spring irrigation combinations. The results showed that SHAW model could reliably simulate the water, heat and salt transport in freezing-thawing soil in Southern Xinjiang during fallow period. The simulation accuracy of soil temperature was the highest, R~2 of different soil depths was not less than 0.95, while poor for soil water content and salt content with the minimum R~2 of 0.61 and 0.73, respectively. The unfrozen water content of different winter irrigation treatments was decreased significantly in the freezing period, and the unfrozen water content was decreased with the increase of winter irrigation quota. The greater the amount of winter irrigation was, the smaller the range of surface soil temperature in freezing period was. However, the larger the amount of winter irrigation was, the less fluctuation the soil surface temperature in frozen period and the slower the temperature increase in spring period were. However, the soil temperature tended to be similar after spring irrigation. The salt content of soil surface was decreased significantly after irrigation, but increased significantly during soil freezing period, and the increase of salt content in deep soil lagged behind that in surface soil. The frozen water in the soil melted in spring period which could leach the salt in topsoil, thus with supplement of a small amount of spring irrigation the surface soil salinity could decrease dramatically and satisfy the requirement of cotton germination. Considering the current situation of water resources in Southern Xinjiang and the influence of various combinations of winter and spring irrigations on soil moisture, heat and salt before sowing, the recommended water-saving irrigation mode was winter irrigation plus a small amount of spring irrigation to improve soil moisture, and the appropriate irrigation quota was winter irrigation of 2 250 m~3/hm~2 and spring irrigation of 300 m~3/hm~2. The proposed strategy of combined winter and spring irrigations for salt leaching could provide theoretical basis for sustainable agricultural water utilization and soil secondary salinization control in Southern Xinjiang.

     

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