首页> 外文期刊>Indian Agriculturist >Distribution of available boron and sorption desorption behaviour of boron in some soils of Cooch Behar district of West Bengal: Part II - Sorption and desorption of boron.
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Distribution of available boron and sorption desorption behaviour of boron in some soils of Cooch Behar district of West Bengal: Part II - Sorption and desorption of boron.

机译:西孟加拉邦Cooch Behar区某些土壤中有效硼的分布和硼的吸附脱附行为:第二部分-硼的吸附和脱附。

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摘要

Twenty four soil samples collected from different places of Cooch Behar district of West Bengal were used to estimate the adoption/desorption of applied boron. The sorption/desorption findings were fitted to the standard adsorption isotherms namely, Freundlich and Langmuri adsorption isotherms. The soils had the lower capacity of boron sorption. The Freundlich k value was higher during desorption run that in sorption run indicating greater affinity of sorbed boron for the soil surface, thereby leading to low desirability of once-sorbed boron. Similar trend was also found in the Langmuir adsorption maxima. The Freundlich equation gave a better fit than the Langmuir equation representing greater R2 values. Freundlich k had positive correlation with CEC clay and organic matter content of the soils. Similar trend was also observed in case of Langmuir adsorption isotherm indicating that the soils having higher clay and organic matter content have the greater adsorption sites for boron adsorption. The changes in Gibbs free energy for B adsorption on all the 24 soils were found to be positive indicating that B adsorption was not a spontaneous process and leachability of B was higher for these soils resulting in boron deficiency.
机译:从西孟加拉邦Cooch Behar地区的不同地方收集的24个土壤样品用于估算施用的硼的吸收/解吸。吸附/解吸结果符合标准吸附等温线,即Freundlich和Langmuri吸附等温线。土壤的硼吸附能力较低。解吸过程中的Freundlich k值高于吸附过程中的Freundlich k值,表明被吸附的硼对土壤表面的亲和力更大,从而导致一次被吸附的硼的需求较低。在Langmuir吸附最大值中也发现了类似的趋势。与代表更大的R 2 值的Langmuir方程相比,Freundlich方程具有更好的拟合度。 Freundlich k与CEC黏土和土壤有机质含量呈正相关。在Langmuir吸附等温线的情况下也观察到类似的趋势,这表明粘土和有机质含量较高的土壤对硼的吸附位置更大。发现所有24种土壤上的B吸附的吉布斯自由能的变化都是正的,这表明B吸附不是自发过程,并且这些土壤的B浸出率较高,导致硼缺乏。

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