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首页> 外文期刊>International journal of soil science >Effect of Different Factors on Diffusion Characteristics of Potassium in Alluvial Soils of Eastern Indo Gangetic Plain
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Effect of Different Factors on Diffusion Characteristics of Potassium in Alluvial Soils of Eastern Indo Gangetic Plain

机译:不同因素对印度东部恒河平原冲积土壤钾素扩散特征的影响

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摘要

To understand the transport behaviour of potassium as influenced by different factors, the tracer diffusion (D_a) and porous diffusion (D_p) coefficients of potassium were studied in three alluvial soils of varying potassium content and mineralogicalcomposition. Diffusion coefficients were increased with increase in moisture content (8), temperature (T), bulk density (d) and tracer:bckground ratio (R). The D_a and D_p values were significantly higher when NaCl was taken as background electrolyte than for CaCl_2. Soil with higher exchangeable K and illite content recorded higher D_a and D_p values. The energy of activation (E_a) decreased significantly with increase in bulk density and the Arrhenius frequency factor (A) and entropy factor of diffusion (o) were found to significantly decrease with increasing tracer component. Exchangeable K, nonexchangeable K and illitic fraction of the clay minerals was found most relevant factor predicting the diffusion coefficients of potassium in the alluvial soils.
机译:为了了解不同因素对钾的迁移行为的影响,研究了三种不同钾含量和矿物组成的冲积土壤中钾的示踪扩散系数(D_a)和多孔扩散系数(D_p)。扩散系数随着水分含量(8),温度(T),堆积密度(d)和示踪剂:背景比率(R)的增加而增加。当以NaCl为背景电解质时,D_a和D_p值明显高于CaCl_2。交换钾和伊利石含量较高的土壤记录的D_a和D_p值较高。活化能(E_a)随着堆积密度的增加而显着降低,并且发现Arrhenius频率因子(A)和扩散的熵因子(o)随着示踪剂组分的增加而显着降低。发现粘土矿物中可交换的钾,不可交换的钾和硅质分数是预测钾在冲积土壤中扩散系数的最相关因素。

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