The maximum phosphorus adsorption (S
max) and Phosphorous saturation index (P
sat) of a soil provide information for the proper management of the P fertilizer of the soil. The objective of this investigation was to determine S
max and develop a P
sat for 14 rice soils. Soil samples were analyzed for pH, clay content, dithionite extractable Fe (Fe
D), Mehlich-3 (M3) extractable P (PM3), and Fe (FeM3). The S
max value and P
sat based on M3 extractions were determined. The S
max value ranged from 110 to 625 mg kg
-1, and correlated with sand (r =-0.70, P>0.01), silt (r =0.70, P>0.01), clay (r =0.59, P>0.05) and Fe
D (r =0.71, P>0.01). Soil pH
H2O and organic carbon content were not correlated (P>0.05) with S
max, while pH
KCl was negatively correlated (r =-0.64, P>0.05) with S
max. Multiple regression found that the combination of pH
KCl and Fe
D were the two most important soil properties related to the S
max of the soils studied. Conventional adsorption equations, such as the Langmuir, Freundlich and Temkin equations, satisfactorily described the P sorption of the soils. The P sorption capacity of the studied soils varied from 80 to 316 mg kg
-1. The calculated energy of adsorption of the soils ranged from 0.18 to 1.56 mg L
-1, and there was apparently a negative correlation between the energy of adsorption (k) and the observed S
max values. Buffering capacity ranged from 14 to 69. Phosphorus saturation indices (P
sat) of the tested soils varied from 1.82 to 28.21%, and were correlated with sand (r =0.56, P>0.05) and silt (r =-0.59, P>0.05), but not with the other soil properties we studied.
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