Arsenate and arsenite adsorption in relation with chemical properties of alluvial and loess soils

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Shah Rukh
Mohammad Saleem Akhtar
Ayaz Mehmood
Sayed Hassan
Khalid S. Khan
Syed M.S. Naqvi
Muhammad Imran

Abstract

Arsenic is one of the most toxic elements in the soil environment. Understanding of the arsenic adsorption chemistry is essential for evolving the extent of soil and groundwater contaminations. This research was conducted to determine the variation in adsorption behaviour of arsenite and arsenate with depth in different lithology soils. We sampled two parent materials at genetic horizons, and within a parent material, we selected two soils. Besides basic soil characterizations, a laboratory batch experiments were carried out to study the adsorption of arsenate and arsenite. Freundlich adsorption approaches were employed to investigate the adsorption of arsenate and arsenite in the soils. Freundlich isotherms fit arsenate and arsenite sorption data well with r2 values of 0.88–0.98 in most soils. Arsenate and arsenite adsorption varied with the soil properties, especially in clay composition and in the oxides of iron and alu­minum. Arsenic adsorption parameters also varied with depth in parent mat­erials, and loess derived soils had greater adsorption capacity as compared to alluvial soils in most of the adsorption parameters. This research concludes that the loess soils had higher arsenic adsorption capacity than the alluvial soils. 

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How to Cite
[1]
S. Rukh, “Arsenate and arsenite adsorption in relation with chemical properties of alluvial and loess soils”, J. Serb. Chem. Soc., vol. 82, no. 7-8, pp. 943–954, Aug. 2017.
Section
Environmental Chemistry

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