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

T. Debnath, S. Majumder, D. Saha
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引用次数: 1

Abstract

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.
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连续浸没石灰土和相应的无石灰土在一个和两个干燥周期下的k动力学
通过室内试验,研究了在施氮、施钾和不施氮、不施钾的情况下,不同干燥阶段对浸没石灰土和相应的无底土中不同组分钾转化的影响。监测不同组分K随时间的变化。结果表明,无论处理方式如何,石灰土的速效钾在整个孵育期间都有所增加。而非交换性钾表现出完全相反的结果趋势,特别是在石灰条件下,这表明土壤中这些形式的钾之间存在动态平衡。然而,在无限情况下,可交换形式和不可交换形式的结果趋势是完全不同的。在石灰土中,经过单一干燥阶段,1N沸腾HNO3可萃取K的下降幅度较大。在不同的处理组合下,晶格和总钾没有明显的变化。结果表明,维持干燥期对土壤晶格和全钾的影响不大。
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