Effects of Salinity of Magnetized Water on Water-Salt Transport and Infiltration Characteristics of Soil Under Drip Irrigation

被引:0
|
作者
Wang, Dongwang [1 ,2 ,3 ,4 ]
Wang, Zhenhua [2 ,3 ]
Zhang, Jinzhu [2 ,3 ]
Zhang, Yushun [1 ,4 ]
Chen, Pengpeng [2 ,3 ]
机构
[1] Water Resources & Water Environm Res Inst, Henan Water Conservancy Technol Applicat Ctr, Zhengzhou 450000, Peoples R China
[2] Shihezi Univ, Coll Water Conservancy & Architectural Engn, Shihezi 832000, Peoples R China
[3] Shihezi Univ, Key Lab Modern Water Saving Irrigat, Xinjiang Prod & Construct Grp, Shihezi 832000, Peoples R China
[4] Henan Irrigat Expt Ctr Stn, Zhengzhou 450000, Peoples R China
来源
AGRONOMY-BASEL | 2024年 / 14卷 / 12期
基金
中国国家自然科学基金;
关键词
magnetized brackish water; water-salt distribution; cumulative infiltration; infiltration model parameters; LIQUID WATER; FIELD;
D O I
10.3390/agronomy14122873
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The shortage of fresh water resources and soil salinization restrict the sustainable development of oasis agriculture in Xinjiang, China. Magnetically treated brackish water can physically improve the quality of water used for irrigation, and this technology is being gradually applied in agricultural production. However, the infiltration characteristics of magnetized brackish water and its response to the distribution of soil water and salt are still unknown. We conducted infiltration tests using a one-dimensional soil column system, employing magnetized water at concentrations of 0.2, 1, 3, and 5 g<middle dot>L(-)1, with a magnetization strength of 3000 gauss (GS), and explored the effects of salinity of magnetized water on water-salt transport and infiltration characteristics of soil under drip irrigation. The migration rate of the wetting front of magnetized water infiltration slowed, and the cumulative infiltration content increased. Specifically, compared to the unmagnetized control, the infiltration time at a depth of 40 cm for magnetized water concentrations of 0.2, 1, 3, and 5 g<middle dot>L-1 increased by 17.42%, 42.16%, 47.02%, and 39.19%, respectively. Correspondingly, the cumulative infiltration volume increased by 7.88%, 8.09%, 10.60%, and 5.38%. Further, the infiltration of magnetized brackish water increased the water retention capacity of soil, effectively reduced the salt content of soil layers, and had a remarkable desalting effect. Salinity of the soil profile showed an L-shaped trend of salt accumulation in the lower layer and desalting in the upper layer. For water salinity of 3 g<middle dot>L-1, soil desalting intensity was greatest. In addition, KShf, suction rate, empirical coefficient a, initial infiltration rate, and stable infiltration rate all decreased under magnetization treatment with the same salinity. Thus, this study provides a new way to alleviate the shortage of fresh water resources in arid areas, a guideline for safely using brackish water and also increasing productivity of saline-alkali land.
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页数:16
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