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Cadmium sorption and extractability in tropical soils with variable charge
Marina Colzato1, Luís Reynaldo Ferracciú Alleoni2, Marcos Yassuo Kamogawa2
1University of São Paulo - College of Agriculture Luiz de Queiroz, Av. Pádua Dias, 11, Piracicaba, SP, 13418-900, Brazil. mcolzato@usp.br.
Cadmium (Cd) sorption in tropical soils is influenced by soil properties, with higher sorption capacity linked to more favorable thermodynamic conditions. Cd distribution among soil fractions was consistent across initial concentrations.
Area of Science:
- Environmental Science
- Soil Science
- Geochemistry
Background:
- Cadmium (Cd) availability to plants and environmental impact are governed by its sorption onto soil colloids.
- Understanding Cd sorption and fractionation in soils is key to assessing its affinity with soil components.
Purpose of the Study:
- To evaluate cadmium sorption and desorption dynamics in diverse tropical soils (Oxisols, Mollisol, Entisols).
- To assess the relationship between soil properties and Cd sorption capacity using a thermodynamic approach.
Main Methods:
- Cadmium sorption and desorption experiments were conducted on six different soil types.
- A thermodynamic approach, including Gibbs standard free energy, was used to analyze sorption.
- Chemical fractionation was employed to determine Cd distribution among soil pools.
Main Results:
- Cadmium sorption data fitted the Langmuir model well, with sorption capacities varying from 0.33 to 11.5 mmol kg⁻¹.
- Higher Cd sorption capacity correlated positively with Gibbs standard free energy, indicating more favorable sorption.
- Initial Cd concentration did not significantly affect Cd distribution among soil fractions, with CaCl₂ being the predominant extractant.
Conclusions:
- Soil properties significantly influence cadmium sorption capacity and thermodynamic favorability.
- Cadmium predominantly partitions into the readily extractable fraction (0.1 mol L⁻¹ CaCl₂) regardless of initial concentration.
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