Abstract

Abstract Field experiments were conducted on Black Chernozem and Gray Luvisol soils in Alberta to determine the downward movement of long‐term applications of surface‐broadcast P fertilizer on established forage grass or alfalfa stands. The majority of fertilizer P recovered in soil as extractable P remained in the top 5 cm layer. The amount and depth of movement of applied P increased with P rate, but little or none was recovered below 15 cm.

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