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Effect of NaCl-induced saline sodicity on the interpretation of soil potassium dynamics

机译:NaCl盐溶液对土壤钾动力学解释的影响

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Excess of exchangeable sodium (Na) in salt-affected soils causes ion toxicity and decrease in nutrient uptake by plants, particularly potassium (K). A number of studies have been conducted to investigate the effect of K-fertilization on plant growth under sodic and saline-sodic conditions but the results are much diverse to process for concrete recommendations. To explore the possible reasons, it was hypothesized that Na applied as NaCl to produce salinity/sodicity in the soil may release non-exchangeable K, minimizing the effect of K-fertilization. Incubation studies were conducted for 2, 4 and 6days in the light (sandy loam) and heavy (clay loam) textured soils producing two saline/sodic levels, i.e. 20 and 30 sodium adsorption ratio (SAR) along with control (SAR 3). Potassium fertilizer applied was calculated according to 40 (general recommendations based on soil-nutrient status), 80 and 160kgKha(-1). Interestingly, it was observed that addition of NaCl possibly released non-exchangeable K from the soil minerals and increased the K concentration in soil solution. Total K release was more in heavy textured soil but initial release was more in light textured soil. This release may eliminate the effect of K-fertilization applied under salt stress induced by NaCl. Therefore, it is suggested that while studying Na-K interaction in salt-affected soils, NaCl should be avoided to produce salinity, and naturally occurring saline-sodic soils may be used. Soil Na-K interaction studies including ameliorating effect of K under sodic or saline-sodic conditions should be conducted carefully considering the above-stated argument.
机译:受盐影响的土壤中过量交换的钠(Na)会引起离子毒性,并降低植物特别是钾(K)对养分的吸收。已经进行了许多研究,以研究钾肥在苏打和盐碱条件下对植物生长的影响,但结果对于针对具体建议的过程而言差异很大。为了探究可能的原因,假设将Na用作NaCl在土壤中产生盐度/碱度可能释放出不可交换的K,从而最大程度地降低了K施肥的影响。在轻质(砂壤土)和重质(粘土壤土)质地的土壤中进行孵化研究2、4和6天,产生两种盐/钠水平,即钠和钠的吸收率(SAR)和对照(SAR 3)两种。施用的钾肥根据40(基于土壤养分状况的一般建议),80和160kgKha(-1)进行计算。有趣的是,观察到添加氯化钠可能从土壤矿物中释放出不可交换的钾,并增加了土壤溶液中的钾浓度。重质感土壤中的总钾释放更多,而轻质感土壤中的初始释放更多。这种释放可能消除了在NaCl诱导的盐胁迫下施用钾肥的影响。因此,建议在研究受盐影响的土壤中的Na-K相互作用时,应避免使用NaCl产生盐分,并且可以使用天然存在的盐碱土壤。考虑到上述论点,应仔细进行土壤Na-K相互作用研究,包括在钠盐或盐碱盐条件下改善K的作用。

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