Abstract

The transformation of landscapes from nonurban to urban land use has potential to greatly modify soil phosphorus (P) pools. There is minimal information on variation of P pools along urbanization gradients. Soils in five zones along an urban-rural land use gradient in Hangzhou city, southeast China, were analyzed for total P, Olsen-P and P fractions. Along the urban–rural land use gradient, soil P concentration and storages varied significantly. The urban and suburban areas had significantly higher soil P than the rural area. The results suggest that physical disturbances and inputs of various materials by humans can alter P pools in the soils. The urban and suburban soils were enriched with P varying from 1.1 to 12.0 times for total P (TP) and 1.6–32.9 times for Olsen-P as compared with the rural soils. The relative abundance of the various P fractions in the urban and suburban soils decreased in the order of HCl-P > organic P > residual P > NaOH-IP > NaHCO3-IP > H2O-P. The HCl-P was the dominant fraction and accounted for 42.3–81.0% of TP. Compared with the rural soils, the old urban and new suburban vegetable soils had a higher TP/C ratio, and the new urban and old suburban vegetable soils had a lower TP/C ratio. In old urban zone, the maximum P soil layer appeared as buried under different depth whereas in other soils as surface.

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