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Cadmium background concentrations to establish reference quality values for soils of São Paulo State,Brazil
Authors:Vinicius Henrique de Oliveira  Cleide Aparecida de Abreu  Ricardo Marques Coelho  Leônidas Carrijo Azevedo Melo
Institution:1. Agro-environmental Management, Agronomic Institute (IAC), Av. Bar?o de Itapura, 1481, Campinas, SP, 13022902, Brazil
3. Center of Soils and Environmental Resources, Agronomic Institute (IAC), Campinas, SP, Brazil
2. Department of Soils, Federal University of Vi?osa, Vi?osa, MG, 36570-000, Brazil
Abstract:Proper assessment of soil cadmium (Cd) concentrations is essential to establish legislative limits. The present study aimed to assess background Cd concentrations in soils from the state of São Paulo, Brazil, and to correlate such concentrations with several soil attributes. The topsoil samples (n?=?191) were assessed for total Cd contents and for other metals using the USEPA 3051A method. The background concentration was determined according to the third quartile (75th). Principal component analysis, Spearman correlation, and multiple regressions between Cd contents and other soil attributes (pH, cation exchange capacity (CEC), clay content, sum of bases, organic matter, and total Fe, Al, Zn, and Pb levels) were performed. The mean Cd concentration of all 191 samples was 0.4 mg kg?1, and the background concentration was 0.5 mg kg?1. After the samples were grouped by parent material (rock origin) and soil type, the background Cd content varied, i.e., soils from igneous, metamorphic, and sedimentary rocks harbored 1.5, 0.4, and 0.2 mg kg?1 of Cd, respectively. The background Cd content in Oxisols (0.8 mg kg?1) was higher than in Ultisols (0.3 mg kg?1). Multiple regression demonstrated that Fe was primarily attributed to the natural Cd contents in the soils (R 2?=?0.79). Instead of a single Cd background concentration value representing all São Paulo soils, we propose that the concentrations should be specific for at least Oxisols and Ultisols, which are the primary soil types.
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