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Ozone and Hydrogen

Many technologies have been proposed for detoxifying waste by processes that destroy chemical bonds pyrolytic biological and catalyzed and imcatalyzed reactions with oxygen, hydrogen, and ozone. The following sections deal only with research opportunities in the areas of thermal destmction, biodegradation, separation processes, and wet oxidation. [Pg.133]

M. Nicolet, Aeronomic reactions of hydrogen and ozone, Aeronomica Acta A no. 79, 1970, and in Mesospheric Models and Related Experiments, Fiocco, ed., pp. 1-57, D. Reidel, Dordrecht, the Netherlands, 1971. [Pg.77]

Table IV. A. 2 - Performance and Reaction Products of Hydrogen and Ozone at 1000 psia. Shifting Equilibrium and Frozen Expansion to One Atmosphere (optimum area ratio) and to Vacuum (100 1 area ratio))... Table IV. A. 2 - Performance and Reaction Products of Hydrogen and Ozone at 1000 psia. Shifting Equilibrium and Frozen Expansion to One Atmosphere (optimum area ratio) and to Vacuum (100 1 area ratio))...
Fig. 68. Summary of catalytic reaction data by fluid beds for ethylene hydrogenation and ozone decomposition curves were calculated by the successive contact model. Fig. 68. Summary of catalytic reaction data by fluid beds for ethylene hydrogenation and ozone decomposition curves were calculated by the successive contact model.
The vertical profile of hydrogen and ozone in the vicinity of the tropopause according to Schmidt (1974). [Pg.32]

The OH Meinel bands are generated between 80 and 100 km altitude by the reaction between atomic hydrogen and ozone... [Pg.46]

Kang, B., Heo, Y., Tien, L., Norton, D., Ren, E, Gila, B. and Pearton, S. (2005a) Hydrogen and ozone gas sensing using multiple ZnO nanorods . Applied Physics A-Materials Science Processing, 80(5), 1029-1032. [Pg.209]

Hydrogen and ozone gas sensing using multiple ZnO nanorods. Applied Physics A Materials Science cj Procedures, 80, 1029. [Pg.466]

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]

In general, the presence of fatty acid groups in the phosphoHpid molecule permits reactions such as saponification, hydrolysis, hydrogenation, halogenation, sulfonation, phosphorylation, elaidinization, and ozonization (6). [Pg.99]

The aromatic ring of a phenoxy anion is the site of electrophilic addition, eg, in methylolation with formaldehyde (qv). The phenoxy anion is highly reactive to many oxidants such as oxygen, hydrogen peroxide, ozone, and peroxyacetic acid. Many of the chemical modification reactions of lignin utilizing its aromatic and phenoHc nature have been reviewed elsewhere (53). [Pg.143]

Polymeric OC-Oxygen-Substituted Peroxides. Polymeric peroxides (3) are formed from the following reactions ketone and aldehydes with hydrogen peroxide, ozonization of unsaturated compounds, and dehydration of a-hydroxyalkyl hydroperoxides consequendy, a variety of polymeric peroxides of this type exist. Polymeric peroxides are generally viscous Hquids or amorphous soHds, are difficult to characterize, and are prone to explosive decomp o sition. [Pg.116]

The refining process most commonly used involves treatment with hot aqueous alkaH to convert free fatty acids to soaps, followed by bleaching, usually with hydrogen peroxide, although sodium chlorite, sodium hypochlorite, and ozone have also been used. Other techniques include distillation, steam stripping, neutralization by alkaH, Hquid thermal diffusion, and the use of active adsorbents, eg, charcoal and bentonite, and solvent fractionation... [Pg.355]

Stearolic acid, C H- Oa, yields stearic acid on catalytic hydrogenation and undergoes oxidative cleavage with ozone to yield nonanoic acid and nonanedioic acid. What is the structure of stearolic acid ... [Pg.1094]

All attempts to oxidize either cis- or trans-di-t-butylthiirane oxides failed122 (see equation 20). Reagents investigated included m-chloroperbenzoic acid, sodium peroxide, hydrogen peroxide, ozone and aqueous potassium permanganate. The cis oxide was resistant to oxidation (apparently steric hindrance), and the trans isomer was consumed with excess oxidizing agent but no identifiable products could be isolated. [Pg.407]

Disinfection. Chlorine, as gaseous chlorine or as the hypochlorite ion, is widely used as a disinfectant. However, its use in some cases can lead to the formation of toxic organic chlorides and the discharge of excess chlorine can be harmful. Hydrogen peroxide and ozone are alternative disinfectants that lead to products that have a lower toxic potential. Treatment is enhanced by ultraviolet light. Indeed, disinfection can be achieved by ultraviolet light on its own. [Pg.593]

The atmosphere is a reservoir of aggressive air pollutants that may cause serious deterioration to archaeological objects some of the most active pollutants are sulfur dioxide, hydrogen sulfide, and ozone. [Pg.453]

Listed in the Table 6.1 are some of the more common sources of oxygen employed for oxidations of organic compounds. Dioxygen is not listed because it requires a catalyst for oxidation at low temperatures. Likewise, hydrogen peroxide and ozone exhibit different activities when used with the proper heterogeneous catalyst. [Pg.230]

Intensification can be achieved using this approach of combination of cavitation and advanced oxidation process such as use of hydrogen peroxide, ozone and photocatalytic oxidation, only for chemical synthesis applications where free radical attack is the governing mechanism. For reactions governed by pyrolysis type mechanism, use of process intensifying parameters which result in overall increase in the cavitational intensity such as solid particles, sparging of gases etc. is recommended. [Pg.58]

Chand R, Ince NH, Gogate PR, Bremner DH (2009) Phenol degradation using 20, 300 and 520 kHz ultrasonic reactors with hydrogen peroxide, ozone and zero valent metals. Sep Purif Technol 67 103-109... [Pg.311]

Liquid hydrogen and solid ozone form very powerfully explosive mixtures. [Pg.1869]

The wavelengths at which most of the components of a primitive Earth atmosphere absorb lie, with few exceptions, under 200 nm. The exceptions include ammonia (< 230 nm), hydrogen sulphide (<260 nm) and ozone (180-300 nm). However, ozone was probably present in the primeval atmosphere only in trace amounts, since free oxygen was only available in extremely low concentrations. The young Earth thus had no protective ozone layer, so short-wavelength UV irradiation could readily penetrate the atmosphere. [Pg.111]

In 1899, the Curies first reported the coloration of glass and porcelain and the formation of ozone from oxygen by radioactive radiation. Giesel (1900) noted that the coloration of alkali halides under these radiations was similar to the effect of cathode rays he also observed the decomposition of water. R Curie and Debierne (1901) observed continuous evolution of hydrogen and oxygen... [Pg.1]

The unsaturated structure of the diene hydrocarbon rubbers makes them susceptible to attack by both oxygen and ozone. Oxidative degradation of all rubbers, irrespective of their structures, is inevitable as the energy associated with incident natural light is approximately three times that of a typical carbon-carbon or carbon-hydrogen bond. [Pg.134]


See other pages where Ozone and Hydrogen is mentioned: [Pg.264]    [Pg.389]    [Pg.502]    [Pg.246]    [Pg.278]    [Pg.9]    [Pg.166]    [Pg.295]    [Pg.24]    [Pg.456]    [Pg.240]    [Pg.258]    [Pg.238]    [Pg.791]    [Pg.63]    [Pg.528]    [Pg.664]    [Pg.1522]    [Pg.203]    [Pg.225]    [Pg.1063]    [Pg.598]    [Pg.1040]    [Pg.54]   
See also in sourсe #XX -- [ Pg.15 , Pg.16 , Pg.17 , Pg.47 , Pg.118 , Pg.119 , Pg.120 ]




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