Abstract
Recent reports on the formation of hydrogen peroxide (H
O
) in water microdroplets produced
pneumatic spraying or capillary condensation have garnered significant attention. How covalent bonds in water could break under such mild conditions challenges our textbook understanding of physical chemistry and water. While there is no definitive answer, it has been speculated that ultrahigh electric fields at the air-water interface are responsible for this chemical transformation. Here, we report on our comprehensive experimental investigation of H
O
formation in (i) water microdroplets sprayed over a range of liquid flow-rates, (shearing) air flow rates, and air composition, and (ii) water microdroplets condensed on hydrophobic substrates formed
hot water or humidifier under controlled air composition. Specifically, we assessed the contributions of the evaporative concentration and shock waves in sprays and the effects of trace O
(g) on the H
O
formation. Glovebox experiments revealed that the H
O
formation in water microdroplets was most sensitive to the air-borne ozone (O
) concentration. In the absence of O
(g), we could not detect H
O
(aq) in sprays or condensates (detection limit ≥250 nM). In contrast, microdroplets exposed to atmospherically relevant O
(g) concentration (10-100 ppb) formed 2-30 µM H
O
(aq), increasing with the gas-liquid surface area, mixing, and contact duration. Thus, the water surface area facilitates the O
(g) mass transfer, which is followed by the chemical transformation of O
(aq) into H
O
(aq). These findings should also help us understand the implications of this chemistry in natural and applied contexts.