4.6 Article

Competitive Carboxylate-Silicate Binding at Iron Oxyhydroxide Surfaces

Journal

LANGMUIR
Volume 37, Issue 44, Pages 13107-13115

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acs.langmuir.1c02261

Keywords

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Funding

  1. Swedish Research Council [2020-04853]
  2. CNRS
  3. China Scholarship Council
  4. Rennes Metropole (France)
  5. Institut Universitaire de France (IUF)
  6. Swedish Research Council [2020-04853] Funding Source: Swedish Research Council

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This study investigated the competitive adsorption of dissolved silicate and organic contaminants on goethite surfaces, revealing that high silicate concentrations can displace pre-bound organic molecules. The competition process involves interactions between species and their impact on the goethite surface properties.
Dissolved silicate ions in wet and dry soils can determine the fate of organic contaminants via competitive binding. While fundamental surface science studies have advanced knowledge of binding in competitive systems, little is still known about the ranges of solution conditions, the time dependence, and the molecular processes controlling competitive silicate-organic binding on minerals. Here we address these issues by describing the competitive adsorption of dissolved silicate and of phthalic acid (PA), a model carboxylate-bearing organic contaminant, onto goethite, a representative natural iron oxyhydroxide nanomineral. Using surface complexation thermodynamic modeling of batch adsorption data and chemometric analyses of vibrational spectra, we find that silicate concentrations representative of natural waters (50-1000 mu M) can displace PA bound at goethite surfaces. Below pH similar to 8, where PA binds, every bound Si atom removes similar to 0.3 PA molecule by competing with reactive singly coordinated hydroxo groups (-OH) on goethite. Long-term (30 days) reaction time and a high silicate concentration (1000 mu M) favored silicate polymer formation, and increased silicate while decreasing PA loadings. The multisite complexation model predicted PA and silicate binding in terms of the competition for -OH groups without involving PA/silicate interactions, and in terms of a lowering of outer-Helmholtz potentials of the goethite surface by these anions. The model predicted that silicate binding lowered loadings of PA species, and whose two carboxylate groups are hydrogen- (HB) and metal-bonded (MB) with goethite. Vibrational spectra of dried samples revealed that the loss of water favored greater proportions of MB over HB species, and these coexisted with predominantly monomeric silicate species. These findings underscored the need to develop models for a wider range of organic contaminants in soils exposed to silicate species and undergoing wet-dry cycles.

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