Forms of Potassium and Q/I Relationship in the Acidic Brown Hill Soils of Simla
Ankita Negi, Reena Sharma, K. C. Sud, J. S. Grewal
Abstract
Ankita Negi, Reena Sharma, K. C. Sud, J. S. Grewal
Abstract
NH4OAc extractable soil K in 39 surface samples of acidic brown hill soils of Simla varied from 53 to 775 ppm, with an average value of 206 ppm. The mean values of fixed ana HCl soluble K were 0.23 and 0.715 per cent, respectively. NH4OAc extractable K was positively correlated with organic carbon, silt, clay and cation exchange capacity but negatively with the sand fraction of soils Fixed and HCl soluble K were positively correlated with sand and negatively with silt and day fraction. Fixed and HCl soluble K were highly correlated with each other but poorly with NH4OAc−K. Q/I relationships showed a low capacity as well as low potential buffering capacity of soils and it underlined the importance of K fertilization.
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NH4OAc extractable soil K in 39 surface samples of acidic brown hill soils of Simla varied from 53 to 775 ppm, with an average value of 206 ppm. The mean values of fixed ana HCl soluble K were 0.23 and 0.715 per cent, respectively. NH4OAc extractable K was positively correlated with organic carbon, silt, clay and cation exchange capacity but negatively with the sand fraction of soils Fixed and HCl soluble K were positively correlated with sand and negatively with silt and day fraction. Fixed and HCl soluble K were highly correlated with each other but poorly with NH4OAc−K. Q/I relationships showed a low capacity as well as low potential buffering capacity of soils and it underlined the importance of K fertilization.
Key concepts: Silt, Soil water, Cation-exchange capacity, Potassium, Chemistry, Animal science, Total organic carbon, Environmental chemistry