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Soil Characteristics and Management Effects on Phosphorus Sorption by Highland Plateau Soils of Ethiopia

Miressa Dufferaa and Wayne P. Robargea

a Dep. of Soil Science, North Carolina State Univ., Box 7619, Raleigh, NC 27695-7619 USA



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Fig. 1 Solution P concentration as a function of P applied for surface soil samples (0–15 cm) from the highland plateau areas of Ethiopia. (Standard errors are calculated on the basis of duplicate samples analyzed)

 


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Fig. 2 Phosphorus sorption isotherms for applied P sorbed expressed per unit mass of soil for surface soil samples (0–15 cm) from the highland plateau areas of Ethiopia. (Standard errors are calculated on the basis of duplicate samples analyzed)

 


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Fig. 3 Phosphorus sorption isotherms for applied P sorbed expressed per unit surface area for surface soil samples (0–15 cm) from the highland plateau areas of Ethiopia. (Standard errors are calculated on the basis of duplicate samples analyzed)

 


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Fig. 4 Phosphorus sorption isotherms considering the resin-P as initially sorbed P for surface soil samples (0–15 cm) from the highland plateau areas of Ethiopia. (Standard errors are calculated on the basis of duplicate samples analyzed)

 


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Fig. 5 Phosphorus sorption isotherms considering the sum of resin, NaHCO3 Pi, and NaOH Pi as initially sorbed P for surface soil samples (0–15 cm) from the highland plateau areas of Ethiopia. (Standard errors are calculated on the basis of duplicate samples analyzed)

 





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