魏建涛, 张建新, 范文波, 许忠宇, 董倩倩, 李长晓, 王雅琴. 犁底层深度对膜下滴灌土壤水盐运移影响的模拟研究[J]. 土壤通报, 2021, 52(4): 845 − 853. DOI: 10.19336/j.cnki.trtb.2020092202
引用本文: 魏建涛, 张建新, 范文波, 许忠宇, 董倩倩, 李长晓, 王雅琴. 犁底层深度对膜下滴灌土壤水盐运移影响的模拟研究[J]. 土壤通报, 2021, 52(4): 845 − 853. DOI: 10.19336/j.cnki.trtb.2020092202
WEI Jian-tao, ZHANG Jian-xin, FAN Wen-bo, XU Zhong-yu, DONG Qian-qian, LI Chang-xiao, WANG Ya-qin. Effect of the Plough Bottom Depth on the Soil Water and Salt Transport under Mulched Drip Irrigation[J]. Chinese Journal of Soil Science, 2021, 52(4): 845 − 853. DOI: 10.19336/j.cnki.trtb.2020092202
Citation: WEI Jian-tao, ZHANG Jian-xin, FAN Wen-bo, XU Zhong-yu, DONG Qian-qian, LI Chang-xiao, WANG Ya-qin. Effect of the Plough Bottom Depth on the Soil Water and Salt Transport under Mulched Drip Irrigation[J]. Chinese Journal of Soil Science, 2021, 52(4): 845 − 853. DOI: 10.19336/j.cnki.trtb.2020092202

犁底层深度对膜下滴灌土壤水盐运移影响的模拟研究

Effect of the Plough Bottom Depth on the Soil Water and Salt Transport under Mulched Drip Irrigation

  • 摘要: 为了探寻膜下滴灌条件下犁底层深度对土壤水盐运移的影响规律,采用室内土柱模拟试验与数值模拟相结合的方法,对不同犁底层深度(无犁底层,CK;25 cm深度,PB25;30 cm深度,PB30;35 cm深度,PB35;40 cm深度,PB40;45 cm深度,PB45)下土壤水盐运移规律进行了研究,结果表明:犁底层可以阻碍水分运移,降低水分入渗速率且有一定的阻水性,蒸发结束后PB处理表层10 ~ 20 cm土壤含水率比CK处理大;犁底层有一定的抑盐作用,CK处理上部10 ~ 20 cm土层的“洗盐”效果比PB处理好,蒸发结束后上部10 ~ 20 cm土层盐分最大的是PB30处理,最小的是PB45处理;利用HYDRUS-1D模型对膜下滴灌条件下犁底层对土壤水盐运移的变化规律进行模拟,经过实测数据验证,模拟效果较好。在现行以旋耕为主的传统耕作模式下,可根据不同作物根系吸水和耐盐的特点适度深耕打破犁底层,为作物生长创造适宜的水盐环境。研究结果可为新疆地区盐碱地改良、农业生产可持续发展提供参考。

     

    Abstract: In order to explore the influence of the depth of plough bottom on soil water and salt transport under mulched drip irrigation, the soil column test and simulation method were used to investigate the soil water and salt transport law under different plough bottom depths (no plough bottom, CK; 25 cm depth, PB 25; 30 cm depth, PB 30; 35 cm depth, PB 35; 40 cm depth, PB 40; 45 cm depth, PB 45). The results showed that plough bottom could hinder water movement, reduce water infiltration rate, with a certain water holding capacity. After evaporation, the soil moisture contents of the 10-20 cm soil layer with PB treatments were higher than that of CK treatment. The effect of “salt washing” above 10-20 cm soil layer with CK treatment was better than that of PB treatments. With the increase of plough bottom depth, the phenomenon of surface soil salt returning was gradually aggravated. Under the condition of mulched drip irrigation, the HYDRUS-2D model was used to simulate the law of soil water and salt movement, showing a good effect the verification of measured data. According to the characteristics of water absorption and salt tolerance in the different crops, the moderately deep ploughing should be carried out to break the plough bottom and create a suitable water and salt environment for crop growth. The results could provide a reference for the improvement of saline alkali land and sustainable development of agricultural production in Xinjiang.

     

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