Sulfate Adsorption at
the Buried Fluorite–Solution
Interface Revealed by Vibrational Sum Frequency Generation Spectroscopy
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Abstract
Understanding the structure and energetics of adsorbed
ions at
buried mineral/solution interfaces has great importance to the geochemical
and atmospheric chemistry communities. Vibrational spectroscopy is
a powerful tool for the study of mineral/solution interfaces as these
techniques can be applied in situ, are sensitive to surface structures,
and are generally nondestructive. The use of vibrational sum frequency
generation spectroscopy (VSFG), which is inherently interface-specific,
is applied here to study the adsorption of sulfate at the buried fluorite
(CaF<sub>2</sub>)/Na<sub>2</sub>SO<sub>4</sub> solution surface at
pH 7 and 298 K in the presence of an aqueous background electrolyte,
NaCl. The use of VSFG allowed for the resolution of adsorbed sulfate
complexes from sulfate molecules which reside in the interfacial electric
double layer yet remain fully solvated. The sulfate anion is found
to adsorb with a bidentate inner-sphere structure at the fluorite
surface with an average surface free energy of adsorption of −31
± 3 kJ/mol for pH 7 solutions at 298 K