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Spectroscopic and Computational Studies of Ionic Clusters as Models of Solvation and Atmospheric Reactions

Citation

Kuwata, Keith Tadao (1998) Spectroscopic and Computational Studies of Ionic Clusters as Models of Solvation and Atmospheric Reactions. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/27ng-zt31. https://resolver.caltech.edu/CaltechTHESIS:06182021-193858046

Abstract

Ionic clusters are useful as model systems for the study of fundamental processes in solution and in the atmosphere. Their structure and reactivity can be studied in detail using vibrational predissociation spectroscopy, in conjunction with high level ab initio calculations. This thesis presents the applications of infrared spectroscopy and computation to a variety of gas-phase cluster systems.

A crucial component of the process of stratospheric ozone depletion is the action of polar stratospheric clouds (PS Cs) to convert the reservoir species HCl and chlorine nitrate (CIONO₂) to photochemically labile compounds. Quantum chemistry was used to explore one possible mechanism by which this activation is effected:
CI⁻ + CIONO₂ → CI₂ + NO₃⁻ (1)
Correlated ab initio calculations predicted that the direct reaction of chloride ion with CIONO₂ is facile, which was confirmed in an experimental kinetics study. In the reaction a weakly bound intermediate Cl₂--NO₃⁻ is formed, with ~70% of the charge localized on the nitrate moiety. This enables the Cl₂--NO₃⁻ cluster to be well solvated even in bulk solution, allowing (1) to be facile on PSCs.

Quantum chemistry was also applied to the hydration of nitrosonium ion (NO⁺), an important process in the ionosphere. The calculations, in conjunction with an infrared spectroscopy experiment, revealed the structure of the gas-phase clusters NO⁺(H₂O)ₙ. The large degree of covalent interaction between NO⁺ and the lone pairs of the H₂O ligands is contrasted with the weak electrostatic bonding between iodide ion and H₂O.

Finally, the competition between ion solvation and solvent self-association is explored for the gas-phase clusters CI⁻(H₂O)ₙ, and CI⁻(NH₃)ₙ. For the case of water, vibrational predissociation spectroscopy reveals less hydrogen bonding among H₂O ligands than predicted by ab initio calculations. Nevertheless, for n≥5, cluster structure is dominated by water-water interactions, with CI⁻ only partially solvated by the water cluster. Preliminary infrared spectra and computations on CI⁻(NH₃)ₙ indicate that NH₃ preferentially binds to CI⁻ ion instead of forming inter-solvent networks.

Item Type:Thesis (Dissertation (Ph.D.))
Subject Keywords:Stratosphere, ozone depletion, chlorine nitrate, halide-water cluster, halide-ammonia cluster, nitrosonium ion, time-of-flight mass spectrometry, optical parametric oscillator, infrared predissociation spectroscopy, ab initio, solvation, hydrogen bonding
Degree Grantor:California Institute of Technology
Division:Chemistry and Chemical Engineering
Major Option:Chemistry
Thesis Availability:Public (worldwide access)
Research Advisor(s):
  • Okumura, Mitchio
Thesis Committee:
  • Beauchamp, Jesse L. (chair)
  • Okumura, Mitchio
  • Goddard, William A., III
  • Yung, Yuk L.
Defense Date:17 April 1998
Record Number:CaltechTHESIS:06182021-193858046
Persistent URL:https://resolver.caltech.edu/CaltechTHESIS:06182021-193858046
DOI:10.7907/27ng-zt31
ORCID:
AuthorORCID
Kuwata, Keith Tadao0000-0002-3542-2081
Default Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:14280
Collection:CaltechTHESIS
Deposited By: Kathy Johnson
Deposited On:18 Jun 2021 20:10
Last Modified:22 Jun 2021 21:55

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