When atmospheric-pressure plasmas (APPs) are applied to living mammalian cells, which typically coexist with saline, the cells may be exposed to various bactericidal agents, including hydrogen peroxide (H₂O₂), generated by the plasmas, and possibly protected from bacterial infections. However, an earlier study demonstrated that H₂O₂ was decomposed in a phosphate-buffered saline (PBS) solution exposed to APPs. In other words, the bactericidal effect of H₂O₂ may be mitigated under such conditions. The decomposition was attributed to the liquid-phase reaction between H₂O₂ and hypochlorite anion (ClO⁻). A more recent study has also shown, using global simulations of a liquid-phase chemical reaction model, that chlorine monoxide ClO, rather than ClO⁻ , decomposes H₂O₂ more efficiently in a PBS solution exposed to APPs, although the generation of ClO is required for the presence of ClO⁻ . A question, however, remained as to whether the H₂O₂ decomposition by ClO occurs only near the solution surface or in the solution bulk because a global simulation cannot distinguish the location of chemical reactions inside a solution. The present study is motivated to provide a better understanding of the H₂O₂ decomposition mechanism. The present study has demonstrated, using one-dimensional numerical simulations, that the reaction between H₂O₂ and ClO is indeed the dominant decomposition pathway for H₂O₂ even in the presence of diffusion of chemical species into the solution bulk, and the location of the dominant H₂O₂ decomposition reaction is not limited to the solution surface region; it can also occur in the bulk of the PBS solution.
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Alfianto et al. (2025) studied this question.
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