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Leaching efficiency, desalinization and desodification processes in highly saline soil reclamation

机译:高盐碱土壤开垦中的淋洗效率,脱盐和脱盐过程

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A comparison was made between the leaching efficiency of continuous ponding and intermittent ponding in terms of desalinization and desodification of a highly saline soil. Intermittent ponding was more efficient than continuous ponding in leaching total soluble salts. However, a reduction in the water soluble ions in the soil was quite different with ion species; Cl~- and SO_4~(2-) as anions, and Na~+ and Mg~(2+) as cations were removed more efficiently in intermittent ponding than in continuous ponding, but the opposite was the case with Ca~(2+). During leaching, desodification and desalinization were found to occur simultaneously, though desodification was achieved to a lesser extent than desalinization in both cases. Intermittent ponding proved to be more efficient than continuous ponding with respect to desodification. The soil exchangeable sodium percentage was calculated based on ion activities and cation selectivity coefficients, instead of using the traditional calculation from the sodium adsorption ratio of soil water.
机译:在高盐度土壤的脱盐和脱盐方面,比较了连续池和间歇池的浸出效率。在浸出总可溶盐方面,间歇灌浆比连续灌浆更有效。但是,土壤中水溶性离子的减少与离子种类有很大的不同。与连续池相比,间歇池中的Cl〜-和SO_4〜(2-)为阴离子,而Na〜+和Mg〜(2+)作为阳离子的去除效率更高,但Ca〜(2+ )。在浸出过程中,发现脱盐和脱盐同时发生,尽管在两种情况下脱盐的程度都比脱盐的程度小。事实证明,断续淤积比连续淤积在脱沙方面更有效。基于离子活度和阳离子选择性系数计算土壤可交换钠百分比,而不是使用传统方法根据土壤水的钠吸附率来计算。

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