汪思佳, 王春霞, 吴晨涛. 北疆膜下滴灌棉田单个灌水周期内土壤水热盐迁移规律研究[J]. 土壤通报, 2024, 55(3): 651 − 660. DOI: 10.19336/j.cnki.trtb.2022111804
引用本文: 汪思佳, 王春霞, 吴晨涛. 北疆膜下滴灌棉田单个灌水周期内土壤水热盐迁移规律研究[J]. 土壤通报, 2024, 55(3): 651 − 660. DOI: 10.19336/j.cnki.trtb.2022111804
WANG Si-jia, WANG Chun-xia, WU Chen-tao. Experimental Study on Soil Hydrothermal Salt Migration Law in a Single Irrigation Cycle in Submembrane Drip Irrigation Cotton Field in Northern Xinjiang[J]. Chinese Journal of Soil Science, 2024, 55(3): 651 − 660. DOI: 10.19336/j.cnki.trtb.2022111804
Citation: WANG Si-jia, WANG Chun-xia, WU Chen-tao. Experimental Study on Soil Hydrothermal Salt Migration Law in a Single Irrigation Cycle in Submembrane Drip Irrigation Cotton Field in Northern Xinjiang[J]. Chinese Journal of Soil Science, 2024, 55(3): 651 − 660. DOI: 10.19336/j.cnki.trtb.2022111804

北疆膜下滴灌棉田单个灌水周期内土壤水热盐迁移规律研究

Experimental Study on Soil Hydrothermal Salt Migration Law in a Single Irrigation Cycle in Submembrane Drip Irrigation Cotton Field in Northern Xinjiang

  • 摘要:
    目的 通过连续监测膜下滴灌棉田单个灌水周期内土壤水热盐状况,掌握其在土体内随时间变化的运移规律,并探究三者之间存在的相互作用关系。
    方法 利用Trime-T3测得各层土壤含水量与含盐量,同时利用八路报警温度记录仪同步检测土壤温度。
    结果 ①土层含水量随时间变化趋势基本一致,灌后土壤水分聚集在棉行下方根系附近。滴头下方土壤盐分变幅最为显著,单个灌水周期结束,滴头下方土壤呈现脱盐现象,而膜间与棉行下方土壤则呈现积盐现象。灌溉水对土壤温度影响显著,单个灌水周期结束后,滴头下方土壤温度呈现先大幅下降后缓慢上升趋势,而土壤盐分对温度影响并不显著。土壤含水量、含盐量与时间的幂指数相关系数随土层深度增加呈先增加后降低的趋势。
    结论 北疆滴灌棉田单个灌水周期内各土层含水量、温度和含盐量存在差异,随灌水结束后时间的延长,北疆滴灌棉田单个灌水周期内各土层含水量、温度和含盐量变化明显,但水分调控水、温、盐的主导作用越发明显;土壤含水量与同一土层的土壤温度、与10 cm以下各土层含盐量呈显著负相关关系,这一水盐空间变化特征可用于当地棉田灌溉灌水周期内土壤墒情变化预测,为棉花精细灌溉制度的制订提供参考。

     

    Abstract:
    Objective Through continuous monitoring of soil water, heat and salt quantities in a single irrigation cycle of a drip-irrigated cotton field under the membrane, the aims were to grasp the transport law of their changes in the soil body over time, and to explore the interaction relationships among them.
    Methods The soil water content and salt content of each layer were measured by using Time-T3, while the soil temperature was detected synchronously by using an eight-channel alarm temperature recorder.
    Results The water content of each soil layer with the time change trend was basically the same. After irrigation, soil water gathered in the cotton row below the root system near. The salinity of the soil below the drip head was the most significant. The end of a single irrigation cycle, the soil below the drip head presented desalination phenomenon, while the soil between the membrane and the cotton row presented salination phenomenon. The irrigation water had a significant impact on soil temperature. After a single irrigation cycle, the soil temperature below the drip head showed a significant drop first and then slow down. ④The temperature of soil below the drip head showed a significant drop first and then slow down. After a single irrigation cycle, the soil temperature showed a significant decrease and then a slow increase, while the soil salinity did not significantly affect the temperature. The power index correlation coefficient of soil water content, salinity and time showed an increase and then a decrease in the depth of the soil layer.
    Conclusion There are differences in the quantity of water, heat and salt in each soil layer in a single irrigation cycle. With the extension of the end time of irrigation, water plays a dominant role in checking and balancing, and its spatial and temporal distribution is significantly affected by the crop root system. So its spatial change characteristics can be utilized to predict the soil moisture content in an arbitrary irrigation cycle in the same case, and to provide a fine irrigation system.

     

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