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a Dep. of Chemistry and Biochemistry, South Dakota State University, Brookings, SD 57007 USA
mlthomps{at}iastate.edu
Information about soil P fractions is useful to predict the bioavailability of P in soil as well as to predict the likelihood of its transport. In this study, we used a sequential fractionation procedure to investigate the forms of P in a Mollisol amended at the soil surface with biosolids (i.e., anaerobically digested sewage sludge). Soil samples from three depths (05, 520, and 2035 cm) were collected from a Cumulic Vertic Endoaquoll in a field experiment with three biosolid application rates, two vegetation treatments [hybrid poplarcottonwood trees (Populus x euramericana clone NC-5326) and switchgrass (Panicum virgatum L.)], and four replications per treatment. The Hedley fractionation scheme (dividing soil P into six empirical fractions [water-soluble, NaHCO3-soluble inorganic and organic P; NaOH-soluble inorganic and organic P; HCl-soluble P, and residual P)] was employed. After 6 yr of continuous application of biosolids to poplar plots, the absolute concentrations of all P fractions at the 0- to 5-cm depth increased significantly (P < 0.05). Some P fractions at the 5- to 20-cm depth increased significantly, whereas at the 20- to 35-cm depth, none of the fractions was affected by biosolids amendment. At the 0- to 5-cm depth of both poplar tree and switchgrass plots, the relative concentrations of some of the P fractions (e.g., HClP, NaOHOP, and residual P) decreased rather than increased. Because NaHCO3IP and H2OP increased in the biosolids-amended soil at rates disproportionate to their concentrations in the biosolids, we conclude that HClP applied with biosolids was transformed to more labile forms.
Abbreviations: IP, inorganic P OP, organic P
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