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Stepwise Activation of Water by Open-Shell Interactions, Cl(H2O)
Elizabeth G Christensen1, Ryan P Steele1
1Department of Chemistry and Henry Eyring Center for Theoretical Chemistry, University of Utah, 315 South 1400 East, Salt Lake City, Utah 84112, United States.
Computational studies reveal that while increased water hydration stabilizes charge-transfer in chlorine-water clusters, it is insufficient for full charge separation. Further hydration is needed for this transition.
Area of Science:
- Physical Chemistry
- Computational Chemistry
- Chemical Physics
Background:
- Investigates the chemical activation of water by single chlorine atoms.
- Builds upon prior analysis of chlorine radical-water interactions for small clusters (n=1-4).
Purpose of the Study:
- To computationally examine chlorine radical-water clusters (Cl·(H2O)n) near the onset of ion hydration.
- To explore structural, electronic, and vibrational properties of different isomer classes.
Main Methods:
- Computationally surveyed thousands of unique isomers for chlorine-water clusters.
- Analyzed electronic structures and harmonic vibrational frequencies.
- Investigated three main structural classes: intact hydrated chlorine, hydrogen-transferred, and charge-transferred configurations.
Main Results:
- Identified three distinct structural classes of isomers: intact, hydrogen-transferred, and charge-transferred.
- Charge-transferred isomers significantly stabilized with increased hydration, energetically approaching hydrogen-transferred forms.
- Observed that hydration levels studied were insufficient to achieve energetic crossover between intact complexes and charge-separated configurations.
Conclusions:
- Internal hydration of ions is likely required for complete charge separation in these systems.
- Complete charge separation is anticipated to occur at larger cluster sizes.
- Provides experimentally verifiable computational predictions for vibrational signatures.
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