期刊
ENVIRONMENTAL SCIENCE-NANO
卷 8, 期 2, 页码 -出版社
ROYAL SOC CHEMISTRY
DOI: 10.1039/d0en00971g
关键词
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资金
- U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences, and Biosciences Division [21-015452]
- U.S. Department of Energy's National Nuclear Security Administration [DE-NA-0003525]
A quarter of Earth's land surface is covered by porous sedimentary silicate rocks, making silica-water interfaces critical for global-scale fate and transport of chemical species. The properties of these interfaces become unpredictable when confined in nanometer-scale pores within sedimentary rocks. The free energy of hydration of trivalent lanthanide ions is a descriptor that can predict how nanoconfinement will change the thermodynamics and products of interfacial reactions.
A quarter of Earth's land surface is covered by porous sedimentary silicate rocks, so silica-water interfaces are critical to the fate and transport of chemical species on a global-scale. However, while the physiochemical properties of unconfined silica-water interfaces are understood reasonably well, these properties have proven to be unpredictable when the interface is confined in nanometer-scale pores within sedimentary rocks. For example, the existing theories struggle to quantitatively predict how the energetics of adsorption reactions and the coordination environment of adsorbed species shift due to nanoconfinement of an interface. Here, we utilized gradual and known variations in the properties of trivalent lanthanide ions to decipher the chemical interactions that cause the nanoconfinement effects on chemistry at the silica-water interfaces. We discovered that the lanthanide's free energy of hydration (Delta G(hydr)) is a descriptor that can be used to predict the extent to which nanoconfinement will change the thermodynamics and products of interfacial reactions. We show that nanoconfinement promotes inner-sphere complexation between lanthanides and silica surface, as well as the formation of polymeric surface species. In nanoconfined domains lanthanide's Delta G(hydr) becomes less negative, reducing the energy required to dehydrate the ion during the formation of an inner-sphere surface complex. These nanoconfinement effects on chemistry become more pronounced for ions with lower hydration free energies.
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