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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. 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 ]

  4. 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.

  5. 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 ...

  6. Fenton's reagent - Wikipedia

    en.wikipedia.org/wiki/Fenton's_reagent

    The free radicals generated by this process engage in secondary reactions. 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.

  7. Photoinitiator - Wikipedia

    en.wikipedia.org/wiki/Photoinitiator

    In the stratosphere, molecular oxygen (O 2) is an important photoinitiator that begins the ozone-production process in the ozone layer. Oxygen can be photolyzed into atomic oxygen by light with wavelength less than 240 nm. [3] O 2 → 2O. Atomic oxygen can then combine with more molecular oxygen to form ozone. O + O 2 → O 3

  8. 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 ...

  9. Radiolysis - Wikipedia

    en.wikipedia.org/wiki/Radiolysis

    Radiolysis is the dissociation of molecules by ionizing radiation.It is the cleavage of one or several chemical bonds resulting from exposure to high-energy flux.The radiation in this context is associated with ionizing radiation; radiolysis is therefore distinguished from, for example, photolysis of the Cl 2 molecule into two Cl-radicals, where (ultraviolet or visible spectrum) light is used.