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Related Experiment Video

Updated: Jun 25, 2026

Integrated Field Lysimetry and Porewater Sampling for Evaluation of Chemical Mobility in Soils and Established Vegetation
10:05

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Published on: July 4, 2014

Arsenic mobility and stabilization in topsoils.

Konstantina Tyrovola1, Nikolaos P Nikolaidis

  • 1Department of Environmental Engineering, Technical University of Crete, University Campus, 73100 Chania, Crete, Greece. konstantina.tyrovola@enveng.tuc.gr

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|February 10, 2009
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Summary

This study shows that zero valent iron (ZVI) can stabilize arsenic in agricultural topsoils. The research developed a model to predict arsenic stabilization efficiency based on iron concentration and soil conditions.

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Published on: December 19, 2017

Area of Science:

  • Environmental Science
  • Soil Science
  • Geochemistry

Background:

  • Agricultural topsoils are susceptible to arsenic pollution from geothermal water irrigation.
  • Arsenic contamination poses risks to soil health and potentially food safety.

Purpose of the Study:

  • To evaluate arsenic mobility in topsoils.
  • To assess the effectiveness of zero valent iron (ZVI) for arsenic stabilization.
  • To develop a predictive empirical model for arsenic stabilization.

Main Methods:

  • Short-term laboratory experiments were conducted to study arsenic stabilization.
  • An empirical model was developed correlating dissolved iron concentration with remaining arsenic in solution.
  • Experiments varied pH, ZVI/solution ratios, and temperature to assess arsenic release and adsorption.

Main Results:

  • Arsenic stabilization efficiency is influenced by reaction time and the ZVI/soil ratio.
  • The developed empirical model predicts arsenic release based on dissolved iron.
  • Arsenate desorption from soil increases with rising temperatures.

Conclusions:

  • Zero valent iron (ZVI) shows potential for stabilizing arsenic in contaminated agricultural topsoils.
  • The empirical model provides a tool for predicting stabilization outcomes.
  • Temperature is a critical factor influencing arsenic desorption from soils.