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    盐渍化灌区非生育期土壤水、热、盐运移规律及其交互效应

    Law of Soil Water,Heat and Salt Transport and Its Interaction Effect in Non-Growth Period of Salinization Irrigation Area

    • 摘要: 为了揭示盐渍化灌区非生育期土壤水、热、盐运移过程的本质,探索最适宜灌区农业可持续发展模式及水资源优化配置策略,于2019~2021年在河套灌区典型中度盐碱地开展了2个完整非生育期的田间定位试验.旨在为准确评估非生育期盐渍化灌区土壤水、热、盐耦合运移特征奠定基础.研究结果表明:非生育期土壤热量总体由深层向表层传导,冻结前期和冻结期以此为主,而消融期则方向相反.秋灌与水分相变是驱动水盐迁移的关键因素.土壤冻结促使60%~80%的水分和15%~20%的盐分向深层运移,而在消融阶段,向浅层输送的水分达130.77%~168.43%,盐分增加21.11%~24.01%.冻结前秋灌带来的脱盐效果短暂,尤其在浅层甚至难以维持至冻结期,因此适度推迟秋灌更有利于节水控盐.随着非生育期的推进,气温对土壤温度及水分对盐分的影响深度逐渐减弱,互作效应降低;而土壤温度与盐分之间的关联则有所增强,冻结期土壤温度对含水率的影响尤为显著.

       

      Abstract: In order to reveal the essence of soil water,heat and salt transport process in non-growth period of salinization irrigation area,and explore the most suitable agricultural sustainable development model and optimal allocation strategy of water resources in irrigation area,two complete non-growth period field positioning experiments were carried out in typical moderate saline-alkali land in Hetao irrigation area from 2019 to 2021,aiming to lay a foundation for accurately evaluating the characteristics of soil water,heat and salt coupling transport in non-growth period salinization irrigation area.The results showed that the soil heat in the non-growth period was generally transmitted from the deep layer to the surface layer,which was mainly in the pre-freezing period and the freezing period,while the ablation period was in the opposite direction.Autumn irrigation and water phase transition are the key factors driving water and salt migration:soil freezing promotes about 60%~80% of water and 15%~20% of salt to move to the deep layer,while the ablation stage transports 130.77%~168.43% of water to the shallow layer and increases 21.11%~24.01% of salt.The desalination effect brought by autumn irrigation before freezing is short,especially in the shallow layer,it is even difficult to maintain until the freezing period.Therefore,moderately delaying autumn irrigation is more conducive to water saving and salt control.With the advance of non-growth period,the influence depth of air temperature on soil temperature and water on salt gradually weakened,and the interaction effect decreased.The correlation between soil temperature and salinity is enhanced,and the effect of soil temperature on water content during freezing period is particularly significant.

       

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