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磁場強度對磁化水入滲和土壤水鹽運移特征的影響
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國家自然科學(xué)基金面上項目(51679190)、國家自然科學(xué)基金重點項目(41830754)、國家重點研發(fā)計劃項目(2016YFC0501405-04)〖JP〗和新疆維吾爾自治區(qū)重大科技專項(2016A03008)


Effects of Magnetic Field Strength on Magnetized Water Infiltration and Soil Water and Salt Movement
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    摘要:

    為探明不同磁場強度對磁化水土壤水鹽運移規(guī)律的影響,揭示磁化水淋鹽增效機理,進行了室內(nèi)一維垂直土柱入滲試驗,研究了0、01、02、03、05T磁場強度磁化水對土壤水鹽運移特征的影響。結(jié)果表明:經(jīng)磁化處理后,土壤水分入滲速率與濕潤鋒運移速率均有所降低,而上層土壤濕潤體水分含量增加;隨著磁場強度的增加,累積入滲量呈現(xiàn)先減后增的變化趨勢,在磁場強度為0.3T時,累積入滲量減少幅度最大。磁場強度對磁化水土壤入滲參數(shù)具有顯著影響,入滲模型吸滲率和飽和導(dǎo)水率與磁場強度之間存在較好的二次多項式關(guān)系,在磁場強度為0.28T時,吸滲率和飽和導(dǎo)水率均達到最小值。磁化水入滲能夠提高水分在上層土壤中的滯留時間,提高上層土壤含水率,降低深層土壤水分入滲量;經(jīng)磁化處理后,單位水體鹽分淋洗量增加,脫鹽率和脫鹽強度顯著提高,在磁場強度為0.3T時磁化水鹽分淋洗效果最好。研究表明,磁場強度顯著影響磁化水入滲和土壤水鹽運移特征。

    Abstract:

    Magnetized water may improve the soil salt leaching efficiency. It is the basis for revealing the mechanism of salt leaching by magnetized water to explore the influence of magnetized water under different magnetic field intensity on the movement of soil water and salt. The effects of magnetized water with 0T, 01T, 02T, 03T and 05T magnetic field intensity on the characteristics of soil water and salt transport were studied through onedimensional vertical soil column infiltration test in the laboratory. The results showed that the soil water infiltration rate and the wetting front migration rate were decreased with irrigation by magnetized water, while the moisture content of the upper soil wetted zone was increased. With the increase of magnetic field intensity, the cumulative infiltration amount showed decreasing trend initially and then increasing. The cumulative infiltration amount was decreased the most when the magnetic field intensity was 03T. Moreover, the magnetic field intensity had a significant influence on the soil water infiltration parameters under the condition of magnetized water infiltration. The soil sorptivity S and saturated hydraulic conductivity Ks of the infiltration model showed the quadratic polynomial relationship with the magnetic field intensity, respectively. When the magnetic field intensity was 028T, both the soil sorptivity S and the saturated hydraulic conductivity Ks were minimized. In addition, magnetized water infiltration could increase the retention time of water in the upper soil, increase the water content of the upper layer soil, and reduce the water infiltration of deep soil. After the magnetization treatment, the salt leaching amount in unit volume of water was increased, and the desalination rate and magnetization desalination intensity were significantly improved. The magnetized water had the best effect on salt leaching when the magnetic field intensity was 03T. The results showed that the magnetic field intensity could significantly affect the characteristics of magnetized water infiltration and soil water and salt transport, which provided theoretical support and guidance for rational use of magnetized water in agricultural irrigation.

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王全九,解江博,張繼紅,韋開,孫燕,李宗昱.磁場強度對磁化水入滲和土壤水鹽運移特征的影響[J].農(nóng)業(yè)機械學(xué)報,2020,51(2):292-298. WANG Quanjiu, XIE Jiangbo, ZHANG Jihong, WEI Kai, SUN Yan, LI Zongyu. Effects of Magnetic Field Strength on Magnetized Water Infiltration and Soil Water and Salt Movement[J]. Transactions of the Chinese Society for Agricultural Machinery,2020,51(2):292-298.

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  • 收稿日期:2019-09-19
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  • 在線發(fā)布日期: 2020-02-10
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