Cited by 147Electrostatics and Colloid InteractionsClay minerals and soil interactionsChemical and Physical Studies

Hydrated Cation Speciation at the Muscovite (001)−Water Interface

Lee, Sang Soo, Fenter, Paul, Park, Changyong, Sturchio, Neil C., Nagy, Kathryn L.·2010·Langmuir

Abstract

Charged materials in aqueous systems interact according to their interfacial properties, typically described by the electrical double layer (EDL). Distributions of divalent metal cations at the muscovite (001)-solution interface observed using resonant anomalous X-ray reflectivity demonstrate an unexpected complexity with respect to the EDL structure. Three forms of adsorbed cations can coexist: the classical inner-sphere and outer-sphere complexes and a third "extended" outer-sphere complex located farther from the surface. Their relative proportions are controlled by the energy balance among cation hydration, interface hydration, and electrostatic attraction. Systematic trends in coverage and position establish the defining role of cation hydration in stabilizing the multiple coexisting species.

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Crossref · 10.1021/la1032866

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1 of 1 references verified0 citation errors · 0 not checkable

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  • Lee et al. found three forms of sorbed cations: classical outer-sphere, inner-sphere, and extended outer-sphere located above the surface hydration layer or maintaining intact higher-order hydration shell.

    “Recently, Lee et al. [4], by using in situ resonant anomalous X-ray reflectivity, found three forms of sorbed cations: the classical outer-sphere and inner-sphere complexes and an B extended ^ outer-sphere complex located above the surface hydration layer or maintaining intact higherorder hydration shell (Fig. 1).”
  • For less strongly hydrated cations, the presence of fulvic acid increased metal sorption in the order Ba ≈ Sr < Pb < Hg, in order of increasing cation affinity for FA.

    “For less strongly hydrated cations, the presence of FA increased metal sorption in the order Ba ≈ Sr&lt;Pb&lt;Hg, in order of increasing cation affinity for FA.”
  • The binding of strongly hydrated metals, such as Cu and Zn, onto the surfaces of muscovite was not altered by FA.

    “Finally, the binding of strongly hydrated metals, such as Cu and Zn, onto the surfaces of muscovite was not altered by FA.”

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Authors
Lee, S. S., Fenter, P., Park, C., Sturchio, N. C., & Nagy, K. L.
Affiliations
  • Argonne National Laboratory (US)
  • University of Illinois Chicago (US)
Corresponding author
Lee, Sang Soo
Venue
Langmuir
Published
2010-10-08
Volume
26
Issue
22
Pages
16647-16651
ISSN
  • 0743-7463 (ISSN-L)
  • 1520-5827
OpenAlex
W2033251150
Cited by
147
References
1
Citations by year
2026: 6 · 2025: 2 · 2024: 11 · 2023: 7 · 2022: 9 · 2021: 10 · 2020: 4 · 2019: 11 · 2018: 11 · 2017: 12 · 2016: 13 · 2015: 11 · 2014: 7 · 2013: 11 · 2012: 12
FWCI
7.01
Type
journal article
Language
en
Open access
closed
Locations
  • Langmuir (publishedVersion)
  • PubMed (publishedVersion)
Topics
  • Physical Sciences › Chemistry › Physical and Theoretical Chemistry › Electrostatics and Colloid Interactions
  • Physical Sciences › Materials Science › Biomaterials › Clay minerals and soil interactions
  • Life Sciences › Biochemistry, Genetics and Molecular Biology › Biophysics › Chemical and Physical Studies
Keywords
muscovite, clay-water interface, electric double layer, divalent cation adsorption, cation hydration, inner-sphere complexes, outer-sphere complexes, electrostatic attraction

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