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首页> 外文期刊>Revista Brasileira de Engenharia Agricola e Ambiental >Saturated hydraulic conductivity of an alluvial soil with different exchangeable sodium percentages
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Saturated hydraulic conductivity of an alluvial soil with different exchangeable sodium percentages

机译:不同钠交换率的冲积土的饱和导水率

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> face="Verdana, Arial, Helvetica, sans-serif" size="2"> The effect of different exchangeable sodium percentages (ESP) on the saturated hydraulic conductivity of a soil was studied under laboratory conditions by determining the relationship between the hydraulic conductivity of a normal soil and that measured on soil with different ESP. The results show a great reduction in the saturated hydraulic conductivity with the increase of the exchangeable sodium percentage in the soil, this reduction being as great as 100% on the highly sodified samples when compared with those which did not receive sodium treatment. This fact is explained due to the dispersing effect of the exchangeable sodium on the soil particles.
机译:> face =“ Verdana,Arial,Helvetica,sans-serif” size =“ 2”>在实验室条件下,通过测定土壤中饱和的水导率,研究了不同可交换钠百分比(ESP)对土壤饱和导水率的影响。正常土壤的水力传导率与不同ESP的土壤的水力传导率之间的关系。结果表明,随着土壤中可交换钠含量的增加,饱和导水率大大降低,与未进行钠处理的样品相比,高度酸化的样品的饱和导水率降低幅度高达100%。可以解释这一事实是由于可交换钠在土壤颗粒上的分散作用。

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