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a Institute of Geography and Natural Resources, Chinese Academy of Sciences, Beijing 100101, China
b Soil and Water Science Dept., University of Florida, Gainesville, FL 32611-0290
* Corresponding author (mchen{at}gnv.ifas.ufl.edu)
Taxonomic and geographic distributions of background P concentrations are important in assessing whether a soil P level is influenced by anthropogenic activities. This study was conducted to establish an upper baseline concentration (UBC) of soil P, which is defined as 97.5% of the background concentration, using 448 geographically and pedogenically representative Florida surface soils (genetic horizon A, A1, Ap, O, O1 or Op) using total P as determined by the USEPA Method 3052 (HClHNO3HF digestion). A significant difference existed in total P concentrations between disturbed (126 mg kg-1, n = 180) and undisturbed (60 mg kg-1, n = 268) soils. Geometric mean (GM) concentration of total P in the undisturbed soils decreased in the order of Histosols (350 mg kg-1) > Mollisols (171 mg kg-1), Inceptisols (140 mg kg-1) > Ultisols (88 mg kg-1) > Alfisols (54 mg kg-1), Entisols (53 mg kg-1) > Spodosols (24 mg kg-1). Aquic suborders tended to have greater P contents than the dry suborders, e.g., Aquents (92 mg kg-1) > Psamments (47 mg kg-1) and Aquods (27 mg kg-1) > Orthods (14 mg kg-1). Total P estimation based on digitized taxonomic soil maps suggested that native soil properties were primary factors in controlling total P in soils. The wide occurrence of P bearing parent materials resulted in many soils having high P concentrations. Twenty-four P-elevated samples from the disturbed soils were identified using the UBC of P for the undisturbed soils at suborder level as reference criterion. Anthropogenic P inputs were related to commercial PO4fertilizer application and population growth as nonpoint sources.
Abbreviations: GM, geometric mean GSD, geometric standard deviation muid, map unit identifier STATSGO, state soil geographic database UBC, upper baseline concentration
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