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  2. Ozone micro-nanobubbles - Wikipedia

    en.wikipedia.org/wiki/Ozone_micro-nanobubbles

    Hydroxyl radicals will form by the shrinking of microbubbles; it is due to an increase in the value of electromotive force on the liquid interface. Hydroxyl radical(•OH) and H + accumulate rapidly at the bubble interface. Ozone reacts with hydroxyl ions and hydroxyl radicals will form. The formation of hydroxyl radicals is pH-dependent.

  3. Ozone–oxygen cycle - Wikipedia

    en.wikipedia.org/wiki/Ozone–oxygen_cycle

    Most of the ozone production occurs in the tropical upper stratosphere and mesosphere. The total mass of ozone produced per day over the globe is about 400 million metric tons. The global mass of ozone is relatively constant at about 3 billion metric tons, meaning the Sun produces about 12% of the ozone layer each day. [1]

  4. NOx - Wikipedia

    en.wikipedia.org/wiki/NOx

    Then, photolysis of NO 2 leads to the formation of ozone and the further formation of hydroxyl radicals (·OH) through ozone photolysis. Since the major sink of methane in the atmosphere is by reaction with • OH radicals, the NO x emissions from ship travel may lead to a net global cooling. [ 34 ]

  5. Advanced oxidation process - Wikipedia

    en.wikipedia.org/wiki/Advanced_oxidation_process

    Hydroxyl radicals are produced with the help of one or more primary oxidants (e.g. ozone, hydrogen peroxide, oxygen) and/or energy sources (e.g. ultraviolet light) or catalysts (e.g. titanium dioxide). Precise, pre-programmed dosages, sequences and combinations of these reagents are applied in order to obtain a maximum •OH yield.

  6. Ozonolysis - Wikipedia

    en.wikipedia.org/wiki/Ozonolysis

    When the solution has stopped absorbing ozone, the excess ozone oxidizes the iodide to iodine, which can easily be observed by its violet color. [6] For closer control of the reaction itself, an indicator such as Sudan Red III can be added to the reaction mixture. Ozone reacts with this indicator more slowly than with the intended ozonolysis ...

  7. Null cycle - Wikipedia

    en.wikipedia.org/wiki/Null_cycle

    O (1 D) + M → O (3 P) + M O (3 P) + O 2 → O 3. Net: hv → H The null cycle can be broken in the presence of certain molecules, leading to a net increase or decrease in ozone in the stratosphere. One important example is NO x emissions into the stratosphere. The NO x reacts with both the atomic oxygen and ozone leading to a net decrease in ...

  8. TCEQ issues ozone pollution alert affecting North Texas Thursday

    www.aol.com/tceq-issues-ozone-pollution-alert...

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  9. Fenton's reagent - Wikipedia

    en.wikipedia.org/wiki/Fenton's_reagent

    For example, the hydroxyl is a powerful, non-selective oxidant. [6] Oxidation of an organic compound by Fenton's reagent is rapid and exothermic and results in the oxidation of contaminants to primarily carbon dioxide and water. Reaction was suggested by Haber and Weiss in the 1930s as part of what would become the Haber–Weiss reaction. [7]