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Understanding how nutrient distribution relates to soil depth is essential for improving fertilization practices for grasslands. This study evaluated the distribution of P, other elements, and selected soil properties at 0- to 5-cm and 5- to 15-cm layers in a grass sward following several years of N and P fertilization. Soil samples were collected in the spring of 2010 from a timothy grass sward (Phleum pratense L.) established in 1998 on a gravely-sandy loam soil. Sixteen combinations of P (0, 15, 30, and 45 kg ha−1) as triple superphosphate and N (0, 60, 120, and 180 kg ha−1) as calcic ammonium nitrate were broadcast annually from 1999 to 2006 in a split-plot design with P as main plots and N as subplots. Concentration of three soil P indicators [water (CP), Mehlich-3 (PM3), and acid oxalate (POx) extractable P] and total phosphorus (PT) were greater in the 0- to 5-cm than in the 5- to 15-cm layer. Differences in concentration of CP, PM3, POx, and PT between the two soil layers increased with increasing P applications. The NH4OAc extractable Ca and Mg concentrations were significantly greater in the 0- to 5-cm soil layer compared with the 5- to 15-cm soil layer. The NH4OAc extractable K was significantly decreased by N application being greater in the 5- to 15-cm soil layer than in the 0- to 5-cm soil layer. Soil pH decreased and the concentration of Mehlich-3 Al increased with increasing N applications only in the 0- to 5-cm layer. This study demonstrated that several years of P fertilizer in grasslands could increase soil available P in the 0- to 5-cm layer, possibly due to lack of mixing and the low mobility of P. Our results also suggest that changes in soil chemical properties induced by N fertilizer in grasslands could be heightened at the 0- to 5-cm layer.
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Messiga et al. (2013) studied this question.
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