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Ion exchange selectivity in clay is controlled by nanoscale chemical–mechanical coupling
by
Whittaker, Michael L.
, Lammers, Laura N.
, Carrero, Sergio
, Banfield, Jillian F.
, Gilbert, Benjamin
in
Binding
/ Cation exchange
/ Cation exchanging
/ Clay
/ Clay minerals
/ Clay soils
/ Collapse
/ Conformation
/ Contaminants
/ Coupling (molecular)
/ cryo-TEM
/ dynamic equilibrium
/ Earth, Atmospheric, and Planetary Sciences
/ Hydration
/ Image resolution
/ Image transmission
/ INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY
/ Interlayers
/ Ion exchange
/ Macromolecules
/ Mechanical properties
/ Montmorillonite
/ Nutrient transport
/ Organic chemistry
/ Physical Sciences
/ Sediments
/ Selectivity
/ Soil contamination
/ Transmission electron microscopy
/ Water pollution
2019
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Ion exchange selectivity in clay is controlled by nanoscale chemical–mechanical coupling
by
Whittaker, Michael L.
, Lammers, Laura N.
, Carrero, Sergio
, Banfield, Jillian F.
, Gilbert, Benjamin
in
Binding
/ Cation exchange
/ Cation exchanging
/ Clay
/ Clay minerals
/ Clay soils
/ Collapse
/ Conformation
/ Contaminants
/ Coupling (molecular)
/ cryo-TEM
/ dynamic equilibrium
/ Earth, Atmospheric, and Planetary Sciences
/ Hydration
/ Image resolution
/ Image transmission
/ INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY
/ Interlayers
/ Ion exchange
/ Macromolecules
/ Mechanical properties
/ Montmorillonite
/ Nutrient transport
/ Organic chemistry
/ Physical Sciences
/ Sediments
/ Selectivity
/ Soil contamination
/ Transmission electron microscopy
/ Water pollution
2019
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Ion exchange selectivity in clay is controlled by nanoscale chemical–mechanical coupling
by
Whittaker, Michael L.
, Lammers, Laura N.
, Carrero, Sergio
, Banfield, Jillian F.
, Gilbert, Benjamin
in
Binding
/ Cation exchange
/ Cation exchanging
/ Clay
/ Clay minerals
/ Clay soils
/ Collapse
/ Conformation
/ Contaminants
/ Coupling (molecular)
/ cryo-TEM
/ dynamic equilibrium
/ Earth, Atmospheric, and Planetary Sciences
/ Hydration
/ Image resolution
/ Image transmission
/ INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY
/ Interlayers
/ Ion exchange
/ Macromolecules
/ Mechanical properties
/ Montmorillonite
/ Nutrient transport
/ Organic chemistry
/ Physical Sciences
/ Sediments
/ Selectivity
/ Soil contamination
/ Transmission electron microscopy
/ Water pollution
2019
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Ion exchange selectivity in clay is controlled by nanoscale chemical–mechanical coupling
Journal Article
Ion exchange selectivity in clay is controlled by nanoscale chemical–mechanical coupling
2019
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Overview
Ion exchange in nanoporous clay-rich media plays an integral role in water, nutrient, and contaminant storage and transport. In montmorillonite (MMT), a common clay mineral in soils, sediments, and muds, the swelling and collapse of clay particles through the addition or removal of discrete molecular layers of water alters cation exchange selectivities in a poorly understood way. Here, we show that ion exchange is coupled to the dynamic delamination and restacking of clay layers, which creates a feedback between the hydration state of the exchanging cation and the composition of the clay interlayer. Particles with different hydration states are distinct phases with unique binding selectivities. Surprisingly, equilibrium achieved through thermal fluctuations in cation concentration and hydration state leads to the exchange of both ions and individual MMT layers between particles, a process we image directly with high-resolution transmission electron microscopy at cryogenic conditions (cryo-TEM). We introduce an exchange model that accounts for the binding selectivities of different phases, which is likely applicable to many charged colloidal or macromolecular systems in which the structural conformation is correlated with the activities of water and counterions within spatially confined compartments.
Publisher
National Academy of Sciences
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