Abstract
The presence of mercury in soils, like other heavy metals, is associated with organic matter and minerals. Mercury deposited in soils is mainly in its oxidized form Hg2+. The adsorption of Hg (II) from aqueous solution into Ca-bentonite was studied. Adsorption percentage was determined as a function of shaking time and temperature to study the thermodynamics and kinetics of Hg (II) adsorption on Ca-bentonite, which was simulated using the MINSQ and GAUSSIAN 09 programs.
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Robles, I., Bandala, Y., Manríquez, J., & Bustos, E. (2018). Modeling of Hg (II) adsorption onto Ca-bentonite. Journal of the Mexican Chemical Society, 62(2 Special Issue). https://doi.org/10.29356/jmcs.v62i2.396
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