THE EFFECT OF EXCESSIVE SODIUM-CONTAINING IRRIGATION WATERS ON SOIL INFILTRATION RATE

I. Tas, Y. E. Yildirim, Zeki Gokalp
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Abstract

Due to increasing demand for limited water resources, the pressure on irrigation water used in agricultural production is also increasing. One of the alternative solutions to meet the irrigation water needed in agricultural production is to use low-quality water resources. However, use of these waters can cause serious problems for the environment, especially for soil and plants, in the short, medium and long term. The sodium concentration of the irrigation water affects the structure of the soil, infiltration rate and hydraulic conductivity properties, as well as negatively affects the nutrient uptake of the plants. In this study, the effect of irrigation water with excess sodium content on the infiltration rate, which is one of the important parameters for the design and operation of irrigation systems and sustainable agricultural production, was researched. The infiltration rate was measured by the double-ring infiltrometer method. In this study, irrigation water with four different Electrical Conductivity (ECi = 0.6 [control], 5, 10 and 15 dS m-1) and Sodium Adsorption Ratio (SAR) (1, 20, 40 and 50) were used. Cumulative infiltration values varied between 360-446 mm, and a 9-19% reduction was determined as compared to the control treatments, depending on the increasing ECi and SAR ratios. The steady-state infiltration rate of the treatments varied between 24.5-36.5 mm h-1 and decreased by 24-34%. In response to increased EC and SAR in irrigation water, the infiltration rates and cumulative infiltration values of soils decreased.
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过量含钠灌溉水对土壤入渗速率的影响
由于对有限水资源的需求不断增加,农业生产中使用的灌溉用水压力也在增加。满足农业生产所需灌溉用水的替代解决方案之一是使用低质量水资源。然而,从短期、中期和长期来看,利用这些水会给环境,特别是土壤和植物造成严重问题。灌溉水钠浓度影响土壤结构、入渗速率和导水性能,并对植物的养分吸收产生负面影响。过量钠灌溉水对土壤入渗速率的影响是灌溉系统设计和运行以及农业可持续生产的重要参数之一,本文研究了过量钠灌溉水对入渗速率的影响。采用双环式渗滤仪测定渗滤速率。本研究采用4种不同电导率(ECi = 0.6[对照]、5、10和15 dS m-1)和钠吸附比(SAR)(1、20、40和50)的灌溉水。累积入渗值在360-446 mm之间变化,与对照处理相比减少了9-19%,这取决于ECi和SAR比的增加。各处理的稳态入渗速率在24.5 ~ 36.5 mm h-1之间变化,下降幅度为24 ~ 34%。灌溉水EC和SAR的增加导致土壤入渗速率和累积入渗值降低。
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