Abstract
The aim of this study was to develop techniques to evaluate soil phosphorus (P) sorption capacity (PSC) and determine critical soil P levels to predict P loss potential for calcareous soils. Seventy-five soils mostly from Northern China were analyzed for soil P using four extraction methods (water, Pw; carbonate, POls; ammonium oxalate, Pox; and Mehlich 3, PM3) as well as PSC derived from single-point (PSC150) and multipoint sorption (S t) isotherms. Strong correlation was found between PSC150 and S t (r (2)=0.89, p<0.001). The sum of αCaM3 and βMgM3 as an index of PSC (PSC(CaM3 + MgM3)) was most closely related to the maximum amount of P sorbed (S max) as given by the sum of S t and soil initial P setting α=0.039 and β=0.462 (r (2)=0.80, p<0.001). The degree of P saturation (DPS) was thereafter calculated from PSC(CaM3 + MgM3) (DPS(CaM3 + MgM3)), to which Olsen P (POls) was significantly correlated (r (2)=0.82, p<0.001). In a split-line regression from Pw against DPS(CaM3 + MgM3) (r (2)=0.87, p<0.05), a change point was identified at 28.1% DPS(CaM3 + MgM3), which was equivalent to 49.2 mg kg(-1) POls and corresponded to a Pw concentration of 8.8 mg kg(-1). After the change point, a sharp increase in Pw was observed. Our results reveal a new approach to approximating DPS from CaM3 and MgM3 for calcareous soils without the need to generate a S max. We conclude that in the absence of an environmental soil test criteria for P, the DPS(CaM3 + MgM3) and POls could be used to predict P loss potential from calcareous soils.
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