Available Phosphorus by Five Different Soil Testing Methods in Sandy Soils of Southwest Florida, USA

Phosphorus (P) fertilization is critical for improved vegetable production on Florida sandy soils. Mehlich 1 (M1) is the standard soil P testing solution for P fertilization recommendation in acidic soils with low cation exchange capacity. However, its suitability for calcareous and/or alkaline soils needs to be evaluated, therefore compared with that of other soil P testing methods (Mehlich 3, Bray, Olsen, and AB-DTPA) in this study. Soil samples collected from vegetable farms were characterized as alkaline/non-calcareous and calcareous soils. M1-P was well correlated with M3-, Bray-, and Olsen-P, respectively, for both soils. M1-, M3-, and Bray-P were greater from calcareous soil than non-calcareous soil for given labile P, which indicated an overestimation from calcareous soil. Olsen-P for given labile P was similar for both soils, thus well represented available P from both soils. Appropriate soil P testing methods need to be developed in calcareous and/or alkaline soils in southern Florida for improved P fertilization recommendations.

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Publication Details

Published
2024-08-01
DOI
https://doi.org/10.70222/hres27
Primary Topic
Soil and Water Nutrient Dynamics
Type
article
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article

Available Phosphorus by Five Different Soil Testing Methods in Sandy Soils of Southwest Florida, USA

Kelly T. Morgan, Shinjiro Sato
Soil and Water Nutrient Dynamics
article

Available Phosphorus by Five Different Soil Testing Methods in Sandy Soils of Southwest Florida, USA

Kelly T. Morgan, Shinjiro Sato
article en

Abstract

Phosphorus (P) fertilization is critical for improved vegetable production on Florida sandy soils. Mehlich 1 (M1) is the standard soil P testing solution for P fertilization recommendation in acidic soils with low cation exchange capacity. However, its suitability for calcareous and/or alkaline soils needs to be evaluated, therefore compared with that of other soil P testing methods (Mehlich 3, Bray, Olsen, and AB-DTPA) in this study. Soil samples collected from vegetable farms were characterized as alkaline/non-calcareous and calcareous soils. M1-P was well correlated with M3-, Bray-, and Olsen-P, respectively, for both soils. M1-, M3-, and Bray-P were greater from calcareous soil than non-calcareous soil for given labile P, which indicated an overestimation from calcareous soil. Olsen-P for given labile P was similar for both soils, thus well represented available P from both soils. Appropriate soil P testing methods need to be developed in calcareous and/or alkaline soils in southern Florida for improved P fertilization recommendations.

Vol. 1(5)
Life in Land
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Soil and Water Nutrient Dynamics
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Available Phosphorus by Five Different Soil Testing Methods in Sandy Soils of Southwest Florida, USA — Kelly T. Morgan, Shinjiro Sato · (2024) | TGRS Research Map | TGRS