Fate of phosphorus applied in slurry and mineral fertilizer: accumulation in soil and release into surface runoff water

Phosphorus (P) accumulation on the soil surface and its effect on the concentration of dissolved orthophosphate P (PO4-P) in surface runoff water were studied after three years of surface application of slurry and mineral fertilizer to grass ley on a sandy soil, poor in P. The total amount of P applied was 107-143 kg ha(-1), of which 72-119 kg ha(-1) was applied on the soil surface during two or three years without incorporation or mixing. The addition of slurry and mineral fertilizer resulted in an increase in inorganic P in the 0-5 cm but not the 5-25 cm soil layer, but organic P was not affected. The measured changes in inorganic P deviated only by 4-6 kg ha(-1) from the values derived from inputs and outputs of P (crop uptake + losses in surface runoff and drainage water). The increase in inorganic-P was accompanied by increases in the degree of P saturation (DPS) and in P extracted with acid am monium acetate (P-Ac ), sodium bicarbonate (P-Olsen) and anion-exchange resin (P-Resin). In surface runoff, 10-18 months after the last surface application of P, the mean flow-weighted concentration of PO4-P was linearly increased with the values of DPS, P-Ac, P-Olson and P-Resin in the 0-5 cm soil layer. PO4-P was lowest (0.033 mg l(-1) ) in the control plots and highest (0.62 mg l(-1)) in the plot where 143 kg ha(-1) P had been applied in slurry and fertilizer. On that plot, the corresponding values of DPS, P-Ac, P-Olson and P-Resin were 16%, 13 mg kg(-1), 85 mg kg(-1) and 71 mg kg(-)1, respectively. The results showed that on a low P soil, surface applications of slurry and mineral fertilizers may considerably increase the P status at the soil surface , even within a few years, and multiply the P loading to surface runoff from the site. A very shallow soil sampling (< 5 cm) is needed to assess P loading potential in a soil where P has been surface-applied.