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K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase

机译:连续浸没石灰和相应的无盐土壤中的K-动力学经历一,两个循环的干燥阶段

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A laboratory experiment was carried out to study the effect of drying phases on transformation of different fractions of K in submerged limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Changes in different fractions of K were monitored with time. Results showed that irrespective of treatments, available K increased in the limed soil throughout the period of incubation. However, non-exchangeable K showed an exactly opposite trend of results particularly in limed situation indicating a dynamic equilibrium between these forms of K in soils. Although, the trend of results of both available and non-exchangeable forms are totally different in unlimed situation. The decrease in 1N boiling HNO3 extractable K is comparatively more in limed soil subjected to single drying phase. No drastic variation in lattice and total K is observed under different treatment combinations. It indicates, maintenance of drying phase has little effect on lattice and total K in soils.
机译:进行了一项室内实验,研究了干燥阶段对存在和不存在氮肥和钾肥的情况下,浸没石灰和相应的未石灰土壤中不同比例的钾的转化的影响。随着时间监测K的不同分数的变化。结果表明,不管处理如何,在整个培养期间,石灰土壤中的有效钾都会增加。但是,不可交换的K表现出完全相反的结果趋势,特别是在石灰状态下,表明土壤中这些形式的K之间存在动态平衡。虽然,在无限制的情况下,可用和不可交换形式的结果趋势完全不同。 1N沸腾的HNO3可萃取K的减少在单干燥阶段的石灰土壤中相对更大。在不同的处理组合下,未观察到晶格和总K的急剧变化。这表明,保持干燥阶段对土壤的晶格和总钾几乎没有影响。

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