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加氧微咸水溶氧量對土壤水鹽運移特征的影響
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國家自然科學基金項目(41830754)、國家自然科學基金面上項目(2016A03008)和新疆維吾爾自治區(qū)重大科技專項(2016A03008)


Effect of Dissolved Oxygen Content of Oxygenated Brackish Water on Soil Water and Salt Transport
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    摘要:

    利用微納米發(fā)泡器對微咸水進行加氧處理,并對加氧微咸水入滲條件下的土壤水鹽運移特征及對入滲模型參數(shù)影響開展了研究。結(jié)果表明,在微咸水不同溶氧量入滲條件下,入滲時間相同時,累積入滲量和濕潤鋒深度隨溶氧量增加先增加后減小,微咸水溶氧量為14.0mg/L時累積入滲量和濕潤鋒深度最大。相比于其他處理,微咸水溶氧量為14.0mg/L時能加快水分入滲,增加土壤體積含水率。此外,相比于不加氧處理,不同加氧水平入滲均能提高灌溉水脫鹽效率。同時,利用現(xiàn)有入滲模型對入滲過程進行了定量分析,結(jié)果顯示代數(shù)模型和PHILIP模型都能準確描述加氧微咸水入滲過程,而且模型參數(shù)與微咸水溶氧量存在函數(shù)關(guān)系。PHILIP模型中吸滲率隨著微咸水溶氧量的增加呈先增加后減小的趨勢,最大值出現(xiàn)在14.0mg/L,代數(shù)模型中綜合形狀系數(shù)則呈現(xiàn)相反的規(guī)律,最小值出現(xiàn)在14.0mg/L,且代數(shù)模型可較好描述加氧微咸水一維垂直入滲條件下的土壤含水率分布。

    Abstract:

    The distribution of salt and water and the parameters of infiltration model under the condition of oxygenated brackish water were investigated, and micro-nanobubble rapid generation device was used to carry out different oxygenated levels treatment to brackish water. The results showed that under the condition of different dissolved oxygen infiltration in brackish water, when the infiltration time was the same, the cumulative infiltration and the wetting front depth were increased first and then decreased with the dissolved oxygen amount, and when the dissolved oxygen content of brackish water was 14.0mg/L, the cumulative infiltration and the depth of wet front were maximum. Compared with other treatments, infiltration conditions with dissolved oxygen content of 14.0mg/L in brackish water could accelerate water infiltration and increase soil moisture content. In addition, compared with the treatment without the addition of oxygen, infiltration of different oxygen levels could improve the desalination efficiency of irrigation water. The fitting effect of algebraic model was better than that of PHILIP model under the condition of oxygenated brackish water. In the PHILIP model, with the increase of dissolved oxygen in brackish water, the permeation rate was increased first and then decreased, and the maximum appeared at 14.0mg/L. In the algebraic model, the comprehensive shape factor showed the opposite law, and the minimum value appeared at 14.0mg/L, the algebraic model was able to fit the soil moisture content under one-dimensional vertical infiltration conditions of oxygenated brackish water.

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孫燕,朱夢杰,王全九,張繼紅.加氧微咸水溶氧量對土壤水鹽運移特征的影響[J].農(nóng)業(yè)機械學報,2019,50(6):299-305. SUN Yan, ZHU Mengjie, WANG Quanjiu, ZHANG Jihong. Effect of Dissolved Oxygen Content of Oxygenated Brackish Water on Soil Water and Salt Transport[J]. Transactions of the Chinese Society for Agricultural Machinery,2019,50(6):299-305.

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  • 收稿日期:2019-03-15
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  • 在線發(fā)布日期: 2019-06-10
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