Abstract

This study investigates the sorption of arsenate from water using zero-valent iron ZVI as sorbent. Batch experiments were carried out to study the sorption kinetics of arsenate under different concentrations of arsenate varies from 0.5 to 200 mg/l. A kinetic model was considered to describe the arsenates sorption on ZVI material. The kinetics of the arsenate sorption processes were described by the Langmuir kinetic model. The sorption capacity increases with high initial concentration which obtained the maximum sorption 2.1 mg/g at 200 mg/l of arsenate initial concentration. The results show that the rapid initial sorption rates of arsenate were occurred at the beginning of experiments running time, followed by a slower removal that gradually approaches an equilibrium condition. The data from laboratory batch experiments were used to verify the simulation results of the kinetic model resulting in good agreement between measured and modeled results. The results indicate that ZVI could be employed as sorbent materials to enhance the sorption processes and increase the removal rate of arsenate from water.

Highlights

  • Arsenic contamination of drinking water is an issue of great concern

  • We propose a modeling approach that attempts to describe the sorption kinetic rate of arsenate onto Zero valent iron (ZVI)

  • The sorption kinetic of arsenate model describes the rate at which chemical reactions occur in As/ZVI/H2O system

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Summary

Introduction

Arsenic contamination of drinking water is an issue of great concern. Due to its high toxicity to humans, theWorld Health Organization (WHO) has set a maximum concentration limit 10 μg/l for arsenic in drinking water [1].Natural occurrence of arsenic in groundwater is associated with sedimentary deposits, volcanic deposits, geothermal fields, neotectonic active fault areas and regions near lacustrine or marine deposits [2]. Arsenic contamination of drinking water is an issue of great concern. Due to its high toxicity to humans, the. World Health Organization (WHO) has set a maximum concentration limit 10 μg/l for arsenic in drinking water [1]. Natural occurrence of arsenic in groundwater is associated with sedimentary deposits, volcanic deposits, geothermal fields, neotectonic active fault areas and regions near lacustrine or marine deposits [2]. A sizeable amount of them occur due to irresponsible human activity, such as agricultural activities, where arsenic is used for the production of insecticides and herbicides. Areas, which are close to mining activities, have been found to contain elevated arsenic concentrations. Arsenic is present mainly in inorganic forms in natural waters. Inorganic arsenic species are predominantly in molecular form of H3AsO30 and the negatively charged

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