The transport of bioavailable phosphorus (BAP, i.e., algal available) in agricultural runoff can accelerate freshwater eutrophication. As procedural and theoretical limitations have restricted BAP estimation in agricultural soils and runoff, a routine method was developed using iron oxide-impregnated paper strips (Fe-oxide strips) as a sink for BAR Fe-oxide strips were used to investigate the amounts and seasonal dynamics of BAP in 12 Oklahoma soils over 2 years and the effect of agricultural management on BAP loss in runoff from these 12 and 8 additional sites over 4 years. The sites involved native grass, wheat ( Triticum aestivum L.), sorghum [ Sorghum bicolor (L.) Moench.], and peanut ( Arachis hypogaea L.). The strip P content of unfertilized soils was higher in winter (October–March; 10–19 mg kg −1) than spring months (May–June; 3–6 mg kg −1). For the P-fertilized soils, the strip P content increased from 8–17 mg kg −1 prior to P application (20–25 kg ha −1 yr −1 to 33–42 mg kg −1 immediately following application. Seasonal dynamics of strip and organic (OP) and inorganic P (IP) fractions indicated mineralization of moderately labile OP, as a function of phosphatase enzyme activity, and release of moderately labile IP and fertilizer P, as a function of P sorption capacity; these are the major processes controlling the strip P content of unfertilized and fertilized soil, respectively. Dissolved organic P did not reduce the efficiency of IP sorption by the Fe-oxide strips and removal of P from the strips by NaOH rather than H 2S0 4 minimized hydrolysis of OP sorbed on the strip. The loss of BAP in runoff was a function of watershed management. Over the 4-yr study, BAP losses increased in the order reduced till (98 g ha −1 yr −1), native grass (160 g ha −1 yr −1), no till (382 g ha −1 yr −1), and conventional till (678 g ha −1 yr −1). Although the total P loss was 93% lower from no till than conventional till, 73% was bioavailable for no till compared to only 28% for conventional till. Clearly, strip P is a dynamic soil property, which, along with watershed management, can influence the bioavailability of P loss in runoff. Thus, the BAP content of runoff in conjunction with runoff and erosion potential may provide a more reliable index of the trophic response of receiving water bodies than dissolved or total P.
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