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OH has been shown to form o-, m-, and p-Tyr.
The particulate-induced formation of OH has been linked with oxidative stress [12, 13] and genotoxicity [14, 13].
It has been elucidated that, O2− is the main active species, and OH has been also generated in the reaction system.
The extreme reactivity of OH has been implicated in several diseases [10, 11] and the reactivity of OH toward organics has been exploited in the remediation of organic solvents [12, 13].
Except for hydrogrossular-andradite, garnet that forms at low pressure is a nominally anhydrous mineral, but OH has been identified in garnet of mantle origin at concentrations ranging up to hundreds of ppmw (ppm wt% as H2O) (Aines and Rossman 1984; Ogasawara et al. 2012, 2013).
To conclude, during the last years the change in Finnish OH has been substantial.
Similar(49)
Also, the stretching of bonds as –OH had been investigated from 3388.2 to 3444.39 cm−1.
Roles of high valence metal ions, reaction intermediates and surface hydroxyls (OH) have been in-depth and newly cognized.
In vivo, hydroxyl radicals (OH) have been implicated in causing oxidative stress [2, 3] and several diseases [4, 5].
The values of rate constants of some chemical reactions involving N2O, NO, and OH have been specified.
Minerals that induce the formation of OH have been shown to cause strand breakage in DNA [9, 36], which is of interest in genotoxicology (for review see [36]).
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