Journal of Plant Nutrition and Soil Science · 2003 · 12 citations · 9 references
AgricultureAgronomySoil SciencesSoil BiogeochemistrySoil ChemistrySoil ScienceNutrient AvailabilitySoil Chemical PropertiesSoil Fertility EvaluationSoil Nutrient AvailabilitySoil PhSoil Phosphorus ChemistryAmmonium Acetate ExtractionAvailable Soil PhosphorusExtractionsP-valuesPhosphate Availability In SoilSoil Ph MeasurementSoil Phosphorus AvailabilitySoil Phosphorus Speciation
Abstract The P status of the soils of Geneva is routinely determined by two independent chemical extractions. The P amounts extracted independently by an aqueous solution of ammonium acetate 0.5 M + EDTA 0.02 M (pH 4.65) (1:10 solid weight : solution volume, 60 minutes) and by H 2 O (1 : 10 solid weight : solution volume, 60 minutes) were assumed to represent mobilizable and mobile phosphorus pools. The best correlations with the data from 1023 crop field soil samples in Geneva canton during the years 1994 to 2000 were obtained by power functions if the data were grouped in two distinct pH ranges: pH 4.6–6.5: (P‐AAE) = 16.436 (P‐H 2 O) 0.6083 ; R 2 = 0.625; n = 166, pH 6.6–8.6: (P‐AAE) = 25.582 (P‐H 2 O) 0.6518 ; R 2 = 0.47; n = 857. The derivatives of these functions are representative of apparent P‐buffering power. Environmentally sound threshold values for P‐H 2 O and P‐AAE are estimated by calculating the change points first of these P‐AAE (quantity) against P‐H 2 O (intensity) curves and second P‐buffering power against P‐H 2 O or P‐AAE curves. The change points obtained from the smoothed quantity‐intensity data were: pH 4.6–6.5: P‐H 2 O = 3.8 mg kg –1 and P‐AAE = 16.436 (3.8) 0.6083 = 37.0 mg kg –1 ; n = 166, pH 6.6–8.6: P‐H 2 O = 2.5 mg kg –1 and P‐AAE = 25.582 (2.5) 0.6518 = 46.5 mg kg –1 ; n = 857. The change‐points for P‐buffering power curves occurred at pH 4.6–6.5: P‐H 2 O = 1.3 mg kg –1 ; P‐AAE = 19.7 mg kg –1 ; n = 166, pH 6.6–8.6: P‐H 2 O = 1.3 mg kg –1 ; P‐AAE = 20.6 mg kg –1 ; n = 857. The threshold buffering powers were: pH 4.6–6.5: d(P‐AAE)/d(P‐H 2 O) = 9.998 (P‐H 2 O) –0.3917 = 9.0, pH 6.6–8.6: d(P‐AAE)/d(P‐H 2 O) = 16.674 (P‐H 2 O) –0.3482 = 15.2. These results show that presently only about 25 % of the crop soils of Geneva canton were within these safe limits. The possibility of applying values of this magnitude which are significantly lower than officially recommended reference levels for phosphorus fertilizer recommendations is supported by recent agronomic investigations.
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A PHOSPHATE SORPTION INDEX FOR SOILS
Bryon W. Bache, E. G. Williams · Journal of Soil Science · 1971 · 537 citations
Determining environmentally sound soil phosphorus levels
Andrew N. Sharpley, T. C. Daniel, J. T. Sims et al. · Journal of Soil and Water Conservation · 1996 · 473 citations