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Soil Science Society of America Journal 64:1090-1099 (2000)
© 2000 Soil Science Society of America

DIVISION S-8-NUTRIENT MANAGEMENT & SOIL & PLANT ANALYSIS

Phosphorus Forms and Concentrations in Leachate under Four Grassland Soil Types

Benjamin L. Turner and Philip M. Haygarth

Dep. of Geography, Royal Holloway, Univ. of London, Egham, Surrey, UK TW20 0EX

phil.haygarth{at}bbsrc.ac.uk

The transfer of P in water draining from agricultural land can contribute to eutrophication and the growth of toxic algae. Traditionally, research has focused on particulate P transfer in surface pathways, with transfer by subsurface pathways perceived as negligible. We investigated this by monitoring P in leachate draining through large-scale monolith lysimeters (135 cm deep, 80 cm diam.) installed in a field site in southwest England. The lysimeters were taken from four grassland soil types with a range of textures (silty clay–sand) and extractable-P contents (15–75 mg kg-1 NaHCO3 extractable P) and leachate was sampled over two drainage seasons. Export of total P was <0.5 kg ha-1 yr-1 for all soil types. Concentrations of total P in the leachate routinely exceeded 100 µg L-1 and remained relatively stable throughout the drainage season, except during the late spring period when maximum concentrations >200 µg L-1 were detected from all soil types. Physically, most of the leachate P was dissolved (<0.45 µm), although 21 to 46% occurred in the particulate (>0.45 µm) size fraction, most notably from the sandy-textured soils. Chemically, the leachate was dominated by reactive (inorganic) P from all soil types (62–71%), although a large proportion was in unreactive (organic) P forms (29–38%). Reactive P occurred mainly in the <0.45 µm fraction, while unreactive P was predominantly in the >0.45 fraction. Unreactive P in the <0.45 µm fraction was greatest during the springtime (April–May), probably reflecting microbiological turnover and release of P in the soil. Our results indicate that (i) subsurface P transfer from soil to surface water can occur at concentrations that could cause eutrophication and (ii) unreactive and >0.45 µm P forms are important in subsurface P transfer.

Abbreviations: RP, reactive phosphorus • RP (<0.45), reactive phosphorus <0.45 µm • RP (>0.45), reactive phosphorus >0.45 µm • TP, total phosphorus • TP (<0.45), total phosphorus <0.45 µm • TP (>0.45), total phosphorus >0.45 µm • UP, unreactive phosphorus • UP (<0.45), unreactive phosphorus <0.45 µm • UP (>0.45), unreactive phosphorus >0.45 µm




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