Effects of pH and cations on adsorption of glyphosate and phosphate at clay minerals

Although competitive interactions between glyphosate (Gly) and phosphate (PO 4 ) in soils were previously confirmed, systematic investigations of their behavior on homo-ionic phyllosilicate clay minerals remain limited. This study employed adsorption edge experiments at different pH conditions to derive solid/liquid distribution coefficients (K d ) and evaluated Gly and PO 4 species-specific adsorption contributions on potassium- and calcium-saturated homo-ionic kaolinite (K-, Ca-kao) and montmorillonite (K-, Ca-mont), alongside elucidating related adsorption mechanisms. The results identified H 2 Gly − as the dominant Gly species driving adsorption on K-clays. For PO 4 , H 2 PO 4 − governed adsorption on K-kao, while its enhanced uptake on K-mont under alkaline conditions was reflected in the model by PO 4 3− species. In contrast, both Gly and PO 4 exhibited Ca 2+ -bridged co-adsorption mechanisms on Ca-clays, yielding enhanced adsorption capacities compared to K-clays. At alkaline pH, removal of aqueous PO 4 was primarily attributed to Ca 2+ -PO 4 precipitation. Competitive adsorption data, combined with single-system results, resolved the interplay of surface complexation, interlayer adsorption, and hydrogen bonding under co-adsorption conditions. Notably, Ca 2+ played a dual role by promoting Gly release under competition yet enhancing Gly adsorption in single scenarios. The sorption comparison of Gly and PO 4 with Fe/Al oxides revealed preferential PO 4 adsorption at oxides, while Gly showed comparable adsorption affinity, validating previous kinetic competition analyses. This study elucidates the distinct roles of adsorbate speciation, cation type, and mineral structure, thereby providing a conceptual framework essential for advancing predictions of contaminant behavior in complex environmental systems. • Glyphosate/phosphate on K + homo-ionic clays occur distinct sorption-driven species. • Ca 2+ bridging co-sorption mediates glyphosate sorption on Ca 2+ homo-ionic clays. • Phosphate removal on Ca 2+ clays: Ca 2+ -P bridging (acidic), precipitation (basic). • Ca 2+ promotes glyphosate release in competition yet enhances individual sorption. • Clay vs. Fe/Al oxides: equilibrium data validates kinetic competition analysis.

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Publication Details

Journal
Applied Clay Science
Published
2025-12-22
DOI
https://doi.org/10.1016/j.clay.2025.108094
Primary Topic
Soil and Water Nutrient Dynamics
Type
article
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article

Effects of pH and cations on adsorption of glyphosate and phosphate at clay minerals

Stefan B. Haderlein, Mingshuai Wang, Joel Fabregat-Palau
Applied Clay Science
Soil and Water Nutrient Dynamics
article

Effects of pH and cations on adsorption of glyphosate and phosphate at clay minerals

Stefan B. Haderlein, Mingshuai Wang, Joel Fabregat-Palau
article en

Abstract

Although competitive interactions between glyphosate (Gly) and phosphate (PO 4 ) in soils were previously confirmed, systematic investigations of their behavior on homo-ionic phyllosilicate clay minerals remain limited. This study employed adsorption edge experiments at different pH conditions to derive solid/liquid distribution coefficients (K d ) and evaluated Gly and PO 4 species-specific adsorption contributions on potassium- and calcium-saturated homo-ionic kaolinite (K-, Ca-kao) and montmorillonite (K-, Ca-mont), alongside elucidating related adsorption mechanisms. The results identified H 2 Gly − as the dominant Gly species driving adsorption on K-clays. For PO 4 , H 2 PO 4 − governed adsorption on K-kao, while its enhanced uptake on K-mont under alkaline conditions was reflected in the model by PO 4 3− species. In contrast, both Gly and PO 4 exhibited Ca 2+ -bridged co-adsorption mechanisms on Ca-clays, yielding enhanced adsorption capacities compared to K-clays. At alkaline pH, removal of aqueous PO 4 was primarily attributed to Ca 2+ -PO 4 precipitation. Competitive adsorption data, combined with single-system results, resolved the interplay of surface complexation, interlayer adsorption, and hydrogen bonding under co-adsorption conditions. Notably, Ca 2+ played a dual role by promoting Gly release under competition yet enhancing Gly adsorption in single scenarios. The sorption comparison of Gly and PO 4 with Fe/Al oxides revealed preferential PO 4 adsorption at oxides, while Gly showed comparable adsorption affinity, validating previous kinetic competition analyses. This study elucidates the distinct roles of adsorbate speciation, cation type, and mineral structure, thereby providing a conceptual framework essential for advancing predictions of contaminant behavior in complex environmental systems. • Glyphosate/phosphate on K + homo-ionic clays occur distinct sorption-driven species. • Ca 2+ bridging co-sorption mediates glyphosate sorption on Ca 2+ homo-ionic clays. • Phosphate removal on Ca 2+ clays: Ca 2+ -P bridging (acidic), precipitation (basic). • Ca 2+ promotes glyphosate release in competition yet enhances individual sorption. • Clay vs. Fe/Al oxides: equilibrium data validates kinetic competition analysis.

Applied Clay ScienceVol. 282
University of Tübingen (DE)
Life in Land
Openalex Percentile: Top 39%
Soil and Water Nutrient Dynamics
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