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Rich exothermic atmosphere

The highly exothermic reaction for the formation of MgF2 heats up the carbon soot formed to approx. 2200 K, which then emits the IR radiation. Moreover, in Mg rich formulations (m > 2), the evaporating Mg is oxidized in the gas phase (3100 K). In addition, the carbon which is formed from the reductive elimination of fluorine from Teflon can be oxidized further to CO or C02 by atmospheric oxygen ... [Pg.84]

See other pages where Rich exothermic atmosphere is mentioned: [Pg.77]    [Pg.138]    [Pg.867]    [Pg.192]    [Pg.138]    [Pg.825]    [Pg.385]    [Pg.316]    [Pg.900]    [Pg.1045]    [Pg.17]    [Pg.390]    [Pg.628]    [Pg.238]   
See also in sourсe #XX -- [ Pg.316 ]



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