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Phosphorus-Sorption Characteristics of Calcareous Soils and Limestone from the Southern Everglades and Adjacent Farmlands

Tropical Research & Education Center, IFAS, University of Florida, 18905 SW 280th Street, Homestead, FL 33031

View larger version (12K): [in a new window]   Fig. 1. Linear P-sorption isotherm of Chekika Soil 9.

View larger version (14K): [in a new window]   Fig. 2. Freundlich and Langmuir P-sorption isotherms and P precipitation of Chekika Soil 9.

View larger version (12K): [in a new window]   Fig. 3. P-sorption isotherm of pineland soil with low in carbonate and high in noncarbonate clay (Soil 17).

View larger version (12K): [in a new window]   Fig. 4. Freundlich P-sorption isotherm of Limestone Bedrock 2.

View larger version (13K): [in a new window]   Fig. 5. P sorption and precipitation of Limestone Bedrock 2.

View larger version (11K): [in a new window]   Fig. 6. Relationship in soils of P-sorption values of the Langmuir Isotherm Smax to those of the one-point isotherm (Psorption).

View larger version (11K): [in a new window]   Fig. 7. Relationship between degree of P saturation (DPS; POlsen/Smax) and P-saturation index (PSI; POlsen/Psorption).