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Dep. Plant and Soil Sci., Univ. of Delaware, Newark, DE 19717-1303
* Corresponding author (rmaguire{at}udel.edu)
The role that soil testing can play in identifying agricultural soils with an increased potential for P loss is an important topic. Our research compared the Mehlich 3 P saturation ratio (M3-PSR) with the ammonium oxalate degree of P saturation (DPSox), and the M3-PSR was then evaluated for predicting agronomic and environmental soil P saturation thresholds. Intact soil columns (15-cm diam, 20 cm deep) and soil samples were collected from five soil series that ranged in soil texture, chemical properties, and Mehlich 3 P. The soils were analyzed for pH, organic matter (OM) and oxalate and Mehlich 3 extractable P, Al, and Fe. Each intact column was leached with the equivalent of 5 mm of rainfall and resulting leachate analyzed for P. Mehlich 3 extractable Al, Fe, and P were closely related to oxalate extractable Al, Fe, and P, although Mehlich 3 extracted only a small amount of Fe compared with oxalate. The M3-PSRs, calculated as the molar ratios of Mehlich 3 extractable P/[Al + Fe] (ratio I) and P/Al (ratio II), were well correlated to each other and to DPSox. All three P saturation measurements showed a threshold or change point above which the concentration of P in column leachate increased rapidly. Both the agronomic optimum M3-PSRs and the environmental limit suggested in the Netherlands for DPSox (25%) were below the observed change point. The M3-PSR measured in a single Mehlich 3 extraction shows excellent promise for identifying soils that represent an increased risk for P leaching losses.
Abbreviations: PM3, AlM3, and FeM3, Mehlich-3 extractable P, Al and Fe M3-PSR, Mehlich 3 P saturation ratio I, P saturation calculated as PM3/[AlM3 + FeM3] Mehlich 3 P saturation ratio II, P saturation calculated as PM3/AlM3 Pox, Alox and Feox, acid ammonium oxalate extractable P, Al and Fe DPSox, degree of P saturation calculated as (Pox,/0.5[Alox + Feox]) x 100 OM, organic matter
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