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Ozone temperature

Heterogeneous chemistry leading to ozone destruction can also lead to ozone-temperature correlations since many of the important reactions forming active chlorine are faster at lower temperatures (see Chapter 12). In addition, there is more PSC formation at the poles and hence more ozone destruction in these regions associated with lower temperatures (see Fig. 13.14 and associated discussion below). [Pg.737]

By comparison of the n-alkylmercurial results alone, it is possible to generalize that both higher ozonation temperatures and the presence of a halogen ligand on mercury promote carbon-carbon cleavage during the ozonolysis of the carbon-mercury bond. [Pg.83]

Even where an aldehyde is formed as a carbonyl fragment in the ozonolysis of an olefin, 1,2,4,5-tetroxans are often formed in a side reaction, depending on the solvent,131 the concentration, and the ozonization temperature. Thus dimeric acetone peroxide is obtained from isobutylene,132 dimeric benzaldehyde peroxide (129) from styrene132 and stilbene,96 132 and dimeric acetophenone peroxide (130) from a-methylstyrene.132... [Pg.199]

Douglass, A.R., R.B. Rood, and R.S. Stolarski, Interpretation of ozone temperature correlations. 2, Analysis of SBUV ozone data. J Geophys Res 90, 10,693, 1985. [Pg.512]

High-resolution laboratory absorption cross section of ozone. Temperature effect, Chem. Phys. Lett. 213 (1993) 610. [Pg.281]

Ozone, temperature resistance, and other properties of TPU are increased when blended with NR [70]. [Pg.758]

Photochemical degradation may cause changes in the monomer imit (by oxidation reactions), the macromolecular chain (through crossUnking or chain scission reactions), and even on the macroscopic scale [7, 25]. Thermal-oxidative degradation, hydrolysis and microbial attack are simultaneously promoted by the presence of the other associated factors (oxygen and ozone, temperature and freeze-thaw cycles, environmental moisture and microorganisms) and contribute to the overall effect [26-29]. [Pg.115]

Another approach is to use the LB film as a template to limit the size of growing colloids such as the Q-state semiconductors that have applications in nonlinear optical devices. Furlong and co-workers have successfully synthesized CdSe [186] and CdS [187] nanoparticles (<5 nm in radius) in Cd arachidate LB films. Finally, as a low-temperature ceramic process, LB films can be converted to oxide layers by UV and ozone treatment examples are polydimethylsiloxane films to make SiO [188] and Cd arachidate to make CdOjt [189]. [Pg.562]

It is slightly soluble in water, giving a neutral solution. It is chemically unreactive and is not easily oxidised or reduced and at room temperature it does not react with hydrogen, halogens, ozone or alkali metals. However, it decomposes into its elements on heating, the decomposition being exothermic ... [Pg.229]

Ozone is formed in certain chemical reactions, including the action of fluorine on water (p. 323) and the thermal decomposition ofiodic(VII) (periodic) acid. It is also formed when dilute (about 1 M) sulphuric acid is electrolysed at high current density at low temperatures the oxygen evolved at the anode can contain as much as 30% ozone. [Pg.263]

At room temperature ozone is a slightly blue diamagnetie gas which condenses to a deep blue liquid. It has a characteristic smell, and is toxic. Ozone is a very endothermic compound ... [Pg.264]

It decomposes exothermically to oxygen, a reaction which can be explosive. Even dilute ozone decomposes slowly at room temperature the decomposition is catalysed by various substances (for example manganese(IV) oxide and soda-lime) and occurs more rapidly on heating. [Pg.264]

Ozone s presence in the atmosphere (amounting to the equivalent of a layer 3 mm thick under ordinary pressures and temperatures) helps prevent harmful ultraviolet rays of the sun from reaching the earth s surface. Pollutants in the atmosphere may have a detrimental effect on this ozone layer. Ozone is toxic and exposure should not exceed 0.2 mg/m (8-hour time-weighted average - 40-hour work week). Undiluted ozone has a bluish color. Liquid ozone is bluish black and solid ozone is violet-black. [Pg.21]

Nitrile mbber finds broad application in industry because of its excellent resistance to oil and chemicals, its good flexibility at low temperatures, high abrasion and heat resistance (up to 120°C), and good mechanical properties. Nitrile mbber consists of butadiene—acrylonitrile copolymers with an acrylonitrile content ranging from 15 to 45% (see Elastomers, SYNTHETIC, NITRILE RUBBER). In addition to the traditional applications of nitrile mbber for hoses, gaskets, seals, and oil well equipment, new applications have emerged with the development of nitrile mbber blends with poly(vinyl chloride) (PVC). These blends combine the chemical resistance and low temperature flexibility characteristics of nitrile mbber with the stability and ozone resistance of PVC. This has greatly expanded the use of nitrile mbber in outdoor applications for hoses, belts, and cable jackets, where ozone resistance is necessary. [Pg.186]

Tetrafluoroethylene Oxide TFEO has only been prepared by a process employing oxygen or ozone because of its extreme reactivity with ionic reagents. This reactivity may best be illustrated by its low temperature reaction with the weak nucleophile, dimethyl ether, to give either of two products (47) (eq. 10). [Pg.304]

The relevant properties of peroxide and superoxide salts are given in Table 4 (see Peroxides and peroxide compounds, inorganic). Potassium peroxide is difficult to prepare and lithium superoxide is very unstable. The ozonides, MO3, of the alkah metals contain a very high percentage of oxygen, but are only stable below room temperature (see Ozone). [Pg.486]

Reaction 1 is the rate-controlling step. The decomposition rate of pure ozone decreases markedly as oxygen builds up due to the effect of reaction 2, which reforms ozone from oxygen atoms. Temperature-dependent equations for the three rate constants obtained by measuriag the decomposition of concentrated and dilute ozone have been given (17—19). [Pg.491]

The calculated half-life of 1 mol % (1.5 wt %) of pure gaseous ozone diluted with oxygen at 25, 100, and 250°C (based on rate constants from Ref. 19) is 19.3 yr, 5.2 h, and 0.1 s, respectively. Although pure ozone—oxygen mixtures are stable at ordinary temperatures ia the absence of catalysts and light, ozone produced on an iadustrial scale by silent discharge is less stable due to the presence of impurities however, ozone produced from oxygen is more stable than that from air. At 20°C, 1 mol % ozone produced from air is - 30% decomposed ia 12 h. [Pg.491]

Ha.logen Compounds. Fluorine is unreactive toward ozone at ordinary temperatures. Chlorine is oxidized to Cl20 and Cl20y, bromine to Br Og, and iodine to I2O2 and I4O2. Oxidation of haUde ions by ozone increases with the atomic number of haUde. Fluoride is unreactive chloride reacts slowly, ultimately forming chlorate and bromide is readily oxidized to hypobromite (38). Oxidation of iodide is extremely rapid, initially yielding hypoiodite the estimated rate constant is 2 x 10 (39). HypohaUte ions are oxidized to haUtes hypobromite reacts faster than hypochlorite (40). [Pg.492]

Oxygen Compounds. Although hydrogen peroxide is unreactive toward ozone at room temperature, hydroperoxyl ion reacts rapidly (39). The ozonide ion, after protonation, decomposes to hydroxyl radicals and oxygen. Hydroxyl ions react at a moderate rate with ozone (k = 70). [Pg.492]

The unstable ammonium ozonide [12161 -20-5] NH O, prepared at low temperatures by reaction of ozone withHquid ammonia, decomposes rapidly at room temperature to NH NO, oxygen, and water (51). Tetrametbylammonium ozonide [78657-29-1] also has been prepared. [Pg.493]

The rate of aqueous ozonation reactions is affected by various factors such as the pH, temperature, and concentration of ozone, substrate, and radical scavengers. Kinetic measurements have been carried out in dilute aqueous solution on a large number of organic compounds from different classes (56,57). Some of the chemistry discussed in the foUowing sections occurs more readily at high ozone and high substrate concentrations. [Pg.493]


See other pages where Ozone temperature is mentioned: [Pg.110]    [Pg.391]    [Pg.135]    [Pg.509]    [Pg.45]    [Pg.448]    [Pg.459]    [Pg.523]    [Pg.8]    [Pg.317]    [Pg.664]    [Pg.138]    [Pg.141]    [Pg.110]    [Pg.391]    [Pg.135]    [Pg.509]    [Pg.45]    [Pg.448]    [Pg.459]    [Pg.523]    [Pg.8]    [Pg.317]    [Pg.664]    [Pg.138]    [Pg.141]    [Pg.888]    [Pg.290]    [Pg.293]    [Pg.476]    [Pg.327]    [Pg.469]    [Pg.269]    [Pg.511]    [Pg.490]    [Pg.490]    [Pg.491]    [Pg.492]    [Pg.493]    [Pg.494]   
See also in sourсe #XX -- [ Pg.45 , Pg.178 ]




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