Detection of reactive oxygen species supplied into the water bottom by atmospheric non-thermal plasma jet using iodine-starch reaction

The supply of reactive oxygen species (ROS) to a target through liquid by plasma jet should be clarified. In this study, a non-thermal plasma jet was irradiated onto the water surface in atmospheric air, and the ROS reaching the water bottom were detected using a gel reagent with iodine-starch reactions. As a result, two-dimensional ROS distributions were visually obtained at the bottom, and the relative ROS concentration was obtained by absorbance measurement. Oxygen addition to helium led to a higher ROS supply into the bottom than helium plasma jet and ozone exposure. A doughnut-shaped ROS distribution was clearly observed at the bottom under certain conditions. The ROS concentration at the bottom significantly depended on irradiation distance and water layer thickness. It is observed from the results obtained using a liquid reagent that the plasma-jet-induced flow and the mixing effect play an important role in ROS supply into the bottom.