By autoxidation The most important (in a commercial sense) peroxides are produced by
autoxidation, the direct reaction of with a hydrocarbon. Autoxidation is a radical reaction that begins with the abstraction of an H atom from a relatively weak
C-H bond. Important compounds made in this way include
tert-butyl hydroperoxide,
cumene hydroperoxide and
ethylbenzene hydroperoxide: : :
Auto-oxidation reaction is also observed with common
ethers, such as
diethyl ether,
diisopropyl ether,
tetrahydrofuran, and
1,4-dioxane. An illustrative product is
diethyl ether peroxide. Such compounds can result in a serious explosion when distilled. :
From hydrogen peroxide Many industrial peroxides are produced using hydrogen peroxide. Reactions with aldehydes and ketones yield a series of compounds depending on conditions. Specific reactions include addition of hydrogen peroxide across the C=O double bond: : In some cases, these hydroperoxides convert to give cyclic diperoxides: : Addition of this initial adduct to a second equivalent of the carbonyl: : Further replacement of alcohol groups: : Triphenylmethanol reacts with hydrogen peroxide in the presence of acid to give the hydroperoxide: :
Naturally occurring hydroperoxides Many hydroperoxides are derived from fatty acids, steroids, and
terpenes. The biosynthesis of these species is affected extensively by enzymes. is generated by conversion of
linolenic acid to the hydroperoxide by the action of a
lipoxygenase followed by the lyase-induced formation of the hemiacetal. In the remote troposphere, hydrogen peroxide (H₂O₂) and
methyl hydroperoxide (CH₃OOH) are among the most abundant hydroperoxides and act as reservoirs for HOx (OH +
HO₂), buffering radical concentrations and tracing oxidation chemistry. Formation in the remote troposphere is dominated by peroxy-radical chemistry: HO₂ + HO₂ → H₂O₂ + O₂ and CH₃O₂ + HO₂ → CH₃OOH + O₂ Global aircraft observations during NASA's Atmospheric Tomography (ATom) mission show that their distributions reflect formation via peroxy-radical chemistry and are modulated by season and recent convection. Under atmospheric conditions, the reaction of organic peroxyl radicals (RO₂) with HO₂—an important source of ROOH—exhibits a generally negative temperature dependence, and its product branching competes with RO₂ autoxidation (isomerization) and RO₂+RO₂ channels. Many functionalized RO₂ types (for example, β-hydroxy or highly oxygenated RO₂) still lack good laboratory data on rates and products. Because of that, the predicted ROOH yields—and how they change with temperature—remain uncertain. == Inorganic hydroperoxides ==