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2017
DOI: 10.9734/ijpss/2017/30445
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Influence of Organic Manure on Phosphorus and Potassium Fractions in Soil Planted with Soybean

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Cited by 7 publications
(5 citation statements)
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“…The increase in total K in soils treated with manures could be attributed to the increase in available K and non-exchangeable K and due to the fixation of added soluble K through manures by clay minerals. The increase in total K with the addition of manures has also been reported by Kaur and Benipal [42], and Soremi et al [43].…”
Section: Total Macronutrients (N P and K)supporting
confidence: 78%
“…The increase in total K in soils treated with manures could be attributed to the increase in available K and non-exchangeable K and due to the fixation of added soluble K through manures by clay minerals. The increase in total K with the addition of manures has also been reported by Kaur and Benipal [42], and Soremi et al [43].…”
Section: Total Macronutrients (N P and K)supporting
confidence: 78%
“…Besides, it could be also due to the prevention of leaching loss due to retention of more potassium by organic components while inorganic fertilizers could have released potassium at a faster rate. These result confirms the findings of [35]; [29]; [36] and [37]. Organic manures had a good effect on reducing potassium fixation by interacting with potassium clay to release potassium from the non-exchangeable fraction into the accessible pool [38].…”
Section: Available Potassiumsupporting
confidence: 91%
“…The lowest concentration of water soluble K in present investigation might be attributed to the fact that the K in the soil solution is more easily utilized by the crop [17]. Sawarkar et al [18] discussed the contributions of various potassium (K) fractions in soil, ranking them as follows: lattice-K > non-exchangeable-K > exchangeable-K > water-soluble-K. A similar trend in the abundance of K fractions in soils was also observed by Soremi et al [19]. In a recent study, Jadhao et al [20] reported the sequential dominance of K fractions in Vertisols of Akola as follows: lattice K > non-exchangeable K > exchangeable K > available K > water-soluble K. Earlier, Prakash and Singh [21] found the water-soluble K fraction to range from 8 to 50 mg kg -1 with a mean value of 18.25 for surface soil and 16.45 mg kg -1 for sub-surface soil.…”
Section: Soil K Fraction Under Different Inm Modulessupporting
confidence: 80%