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磁化微咸水礦化度對(duì)土壤水鹽運(yùn)移的影響
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國(guó)家自然科學(xué)基金面上項(xiàng)目(5167090151)和國(guó)家重點(diǎn)研發(fā)計(jì)劃項(xiàng)目(2016YFC0501405-4)


Effect of Salinity of Magnetized Brackish Water on Salt and Water Movement
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    摘要:

    采用300mT磁感應(yīng)強(qiáng)度恒定磁水器對(duì)不同礦化度微咸水(0.14、2、3、4、5g/L)進(jìn)行磁化處理,并進(jìn)行一維垂直土柱入滲試驗(yàn),研究磁化微咸水礦化度對(duì)土壤水鹽運(yùn)移的影響。結(jié)果表明:微咸水磁化處理后,土壤入滲速率及濕潤(rùn)鋒遷移速率顯著降低,濕潤(rùn)體含水率顯著提高;微咸水礦化度對(duì)磁化效果具有顯著影響,磁化微咸水礦化度為3g/L時(shí),相同入滲時(shí)間累積入滲量和濕潤(rùn)鋒深度相對(duì)減少量最大,濕潤(rùn)體含水率相對(duì)增加量最多。磁化微咸水入滲對(duì)Philip和Green-Ampt入滲公式參數(shù)有顯著影響,相同礦化度的磁化微咸水土壤吸滲率S、飽和導(dǎo)水率Ks及濕潤(rùn)鋒處吸力hf均小于未磁化微咸水;磁化與未磁化微咸水相對(duì)吸滲率ΔS及相對(duì)飽和導(dǎo)水率ΔKs與礦化度之間均呈現(xiàn)較好的二次多項(xiàng)式關(guān)系,在礦化度為3g/L時(shí),相對(duì)吸滲率ΔS及相對(duì)飽和導(dǎo)水率ΔKs均達(dá)到最大。磁化微咸水能夠提高土壤持水能力,相同土層深度的土壤含水率顯著增加;微咸水磁化處理后,脫鹽率顯著提高,土層深度0~20cm磁化微咸水脫鹽率均大于未磁化微咸水,礦化度為3g/L的磁化微咸水磁化脫鹽強(qiáng)度最大,相對(duì)脫鹽效果更好。

    Abstract:

    The physical and chemical properties of magnetized brackish water changed significantly, so irrigation with such water is likely to influence the characteristics of soil water and salt movement. The constant magnetic water device with magnetization intensity of 300mT was used to magnetize brackish water with different salinities (0.14g/L,2g/L,3g/L,4g/L and 5g/L), and one-dimension vertical water infiltration experiment was conducted to reveal the effects of salinity of magnetized brackish water on water and salt movement in soil. Results showed that the soil infiltration rate and wetting front migration rate were decreased significantly with irrigation by magnetized brackish water, whereas the moisture content of the wetted zone was increased significantly. The salinity of brackish water had significant impact on the magnetic effect. When the salinity of brackish water was 3g/L, the relative reductions of cumulative infiltration and wetting front depth reached the maximum, and the relative increase of moisture content of wetted zone reached the maximum at the same infiltration time. Magnetized brackish water had significant impact on the parameters of Philip and Green-Ampt formulas. The soil sorptivity S, the saturated hydraulic conductivity Ks and the wetting front suction of magnetized brackish water were all less than those of the non-magnetized brackish water. There was significantly quadratic polynomial relationship among the relative sorptivity ΔS, the relative saturated hydraulic conductivity ΔKs and the salinity of brackish water. When the salinity of brackish water was 3g/L, the relative sorptivity ΔS and the relative saturated hydraulic conductivity ΔKs reached the peak value. Moreover, magnetized brackish water could enhance soil water retention capacity, thus the soil moisture content was increased significantly in the same soil depth. Magnetized brackish water could improve the desalination efficiency. In the soil depth of 0~20cm, the desalination efficiency of brackish water was greater than that of the non-magnetized brackish water, and when salinity of brackish water was 3g/L, the magnetic salinity intensity was the strongest, and the relative desalination effect turned out to be better.

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王全九,許紫月,單魚洋,張繼紅.磁化微咸水礦化度對(duì)土壤水鹽運(yùn)移的影響[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2017,48(7):198-206. ANG Quanjiu, XU Ziyue, SHAN Yuyang, ZHANG Jihong. Effect of Salinity of Magnetized Brackish Water on Salt and Water Movement[J]. Transactions of the Chinese Society for Agricultural Machinery,2017,48(7):198-206.

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  • 收稿日期:2017-03-29
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  • 在線發(fā)布日期: 2017-07-10
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