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Updated: May 8, 2025

Interfacial Molecular-level Structures of Polymers and Biomacromolecules Revealed via Sum Frequency Generation Vibrational Spectroscopy
Published on: August 13, 2019
Elucidating how trace gases interact with ice surfaces utilizing sum frequency generation spectroscopy.
Gurivi Reddy Yettapu1, Luca B Manning1, Jenée D Cyran1
1Boise State University, Department of Chemistry and Biochemistry, 1910 University Drive, Boise, Idaho, 83702, USA. jeneecyran@boisestate.edu.
Investigating ice surfaces with sum frequency generation (SFG) spectroscopy reveals how acetone and methanol interact differently with water molecules. These interactions impact atmospheric chemistry, affecting ozone depletion and aerosol formation.
Area of Science:
- Atmospheric Chemistry
- Surface Science
- Spectroscopy
Background:
- Trace gas interactions with ice surfaces are critical for atmospheric chemistry, influencing ozone depletion and aerosol formation.
- Understanding molecular adsorption on ice is key to comprehending the impact of hosted molecules and subsequent chemical reactions.
Purpose of the Study:
- To gain a molecular-level understanding of ice-trace gas interactions using surface-selective techniques.
- To probe ice surfaces and observe the adsorption of small organic molecules like acetone and methanol.
Main Methods:
- Utilizing sum frequency generation (SFG) spectroscopy, a surface-selective technique.
- Analyzing the structure of water molecules at ice and water interfaces with and without adsorbed molecules.
Main Results:
- Observed significant differences in water molecule structure at ice/water interfaces upon addition of acetone and methanol.
- Methanol-ice interface showed a blue shift (~80 cm⁻¹) indicating weakened hydrogen bonds, contrasting with acetone-ice interface's red shift (~10 cm⁻¹).
Conclusions:
- The distinct behaviors of water molecules and organic compounds at interfaces are linked to varying reactivity and photochemical reaction rates.
- Observed frequency shifts at interfaces can impact atmospheric models, particularly concerning overtone pumping reactions.
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