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Updated: Feb 9, 2026

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Integrated Field Lysimetry and Porewater Sampling for Evaluation of Chemical Mobility in Soils and Established Vegetation
Published on: July 4, 2014
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Using Qmsax* to evaluate the reasonable As(V) adsorption on soils with different pH
Guannan Lu1, Haixia Tian1, Yanju Liu2
1College of Natural Resources and Environment, Northwest A&F University, Key Laboratory of Plant Nutrition and Agro-environment in Northwest China, Ministry of Agriculture, Yangling 712100, Shaanxi, China.
Ecotoxicology and Environmental Safety
|June 2, 2018
Summary
This study introduces a new parameter, Qmax*, to better assess arsenic adsorption in soils, finding it
Area of Science:
- Environmental Science
- Soil Science
- Geochemistry
Background:
- Arsenic (As) contamination in soil and water poses significant environmental and health risks due to human activities.
- Arsenic bioavailability is critically dependent on its adsorption-desorption dynamics within the soil matrix.
- Traditional adsorption capacity parameters (e.g., Qmax from Langmuir equation) may oversimplify complex soil systems.
Purpose of the Study:
- To develop a more accurate parameter (Qmax*) for evaluating soil's arsenic adsorption capacity, accounting for non-electrostatic interactions.
- To investigate the influence of soil properties, particularly pH, iron oxides (Feox), and clay content, on arsenic adsorption.
- To assess the potential for secondary arsenic pollution through desorption processes.
Main Methods:
- Conducted adsorption-desorption experiments using eighteen Chinese soil samples with varying pH.
- Calculated maximum adsorption capacity (Qmax) using the Langmuir equation.
- Determined the maximum non-electrostatic adsorption capacity (Qmax*) by analyzing the difference between adsorption and desorption.
- Utilized multiple linear regression to identify key soil factors influencing Qmax*.
Main Results:
- Maximum As(V) adsorption capacities (Qmax) ranged from 50.25 to 312.50 mg/kg, strongly correlating with soil pH.
- The new parameter, Qmax*, was significantly higher in acidic/neutral soils (162.18 mg/kg) compared to alkaline soils (79.52 mg/kg).
- Qmax* was primarily influenced by soil Feox and clay content.
- Hysteresis index (HI) values indicated a notable risk of secondary arsenic pollution from desorption.
Conclusions:
- The parameter Qmax* provides a more realistic measure of arsenic adsorption capacity in diverse soil environments.
- Soil pH, Feox, and clay content are critical factors governing arsenic adsorption.
- The desorption process poses a significant risk of secondary arsenic contamination, necessitating careful environmental management.
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