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Other forms of oxygen

The blue colour of the sky is, of course, due to Rayleigh scattering and not to electronic absorption by O2 molecules. [Pg.607]


Recently a new allotrope of oxygen was discovered. When is subjected to great pressure, it is converted into O, which is a deep red solid that is a much more powerful oxidizer than the other forms of oxygen. [Pg.225]

The activity of an oxide catalyst in the absence of gas phase oxygen provides direct evidence that lattice oxygen can perform the selective oxidation process, although it does not exclude the possibility that, in the presence of gas phase oxygen, other forms of oxygen also participate in some stage of the reaction. Pulse experiments are the most suitable for this purpose, because rapid catalyst reduction is then avoided. As pulse experiments have been amply reviewed in Sect. 2, only the conclusions will be discussed here. [Pg.237]

According to these data no reactive atomic oxygen at low and intermediate oxygen concentrations should be present on carbon, which is in clear contradiction to many chemical facts reported above. Other forms of oxygen activation must co-exist with this immediate functionalization of prismatic faces. [Pg.147]

Combustion unit - the electrically fired combustion unit was used in this work, although there is no reason why other forms of oxygen flask should not be used, with appropriate calibration. [Pg.120]

The equihbrium leading to the two other forms of oxygen vacancies ... [Pg.80]

Crystalline Silica. Sihca exists in a variety of polymorphic crystalline forms (23,41—43), in amorphous modifications, and as a Hquid. The Hterature on crystalline modifications is to some degree controversial. According to the conventional view of the polymorphism of siHca, there are three main forms at atmospheric pressure quart2, stable below about 870°C tridymite, stable from about 870—1470°C and cristobaHte, stable from about 1470°C to the melting point at about 1723°C. In all of these forms, the stmctures are based on SiO tetrahedra linked in such a way that every oxygen atom is shared between two siHcon atoms. The stmctures, however, are quite different in detail. In addition, there are other forms of siHca that are not stable at atmospheric pressure, including that of stishovite, in which the coordination number of siHcon is six rather than four. [Pg.472]

Although these localized corrosion mechanisms all involve oxygen to a greater or lesser extent (and thus may be considered forms of oxygen corrosion), they also often involve other corrosive species. Also, the corrosion processes tend to become more indirect in nature, at... [Pg.245]

Fig. 10-13. The links between the cycling of C, N, and O2 are indicated. Total primary production is composed of two parts. The production driven by new nutrient input to the euphotic zone is called new production (Dugdale and Goering, 1967). New production is mainly in the form of the upward flux of nitrate from below but river and atmospheric input and nitrogen fixation (Karl et al, 1997) are other possible sources. Other forms of nitrogen such as nitrite, ammonia, and urea may also be important under certain situations. The "new" nitrate is used to produce plankton protoplasm and oxygen according to the RKR equation. Some of the plant material produced is respired in the euphotic zone due to the combined efforts... Fig. 10-13. The links between the cycling of C, N, and O2 are indicated. Total primary production is composed of two parts. The production driven by new nutrient input to the euphotic zone is called new production (Dugdale and Goering, 1967). New production is mainly in the form of the upward flux of nitrate from below but river and atmospheric input and nitrogen fixation (Karl et al, 1997) are other possible sources. Other forms of nitrogen such as nitrite, ammonia, and urea may also be important under certain situations. The "new" nitrate is used to produce plankton protoplasm and oxygen according to the RKR equation. Some of the plant material produced is respired in the euphotic zone due to the combined efforts...
These two steps were chosen because they are the most activated versions of 0-0 bond scission and 0-H bond formation, respectively. There is evidence that the reactivity of other hydrogenated forms of oxygen follows a similar trend to that of atomic oxygen [Shao et al., 2007a]. [Pg.290]

While oxygen is present in the air, it is even more abundant in water. It is also found in chemically combined form in rocks, sand, and in all plants and animals. In the air it occurs as the free uncombined element but, like hydrogen, the form of oxygen in this state is not a single atom, O, but is a molecule containing two atoms, formula 02. Like H2, it is a colorless, odorless gas, but some of its other properties are quite different. [Pg.27]

Dithiothreitol (DTT) and dithioerythritol (DTE) are the trans and cis isomers of the compound 2,3-dihydroxy-1,4-dithiolbutane. The reducing potential of these versatile reagents was first described by Cleland in 1964. Due to their low redox potential (—0.33 V) they are able to reduce virtually all accessible biological disulfides and maintain free thiols in solution despite the presence of oxygen. The compounds are fully water-soluble with very little of the offensive odor of the 2-mercaptoethanol they were meant to replace. Since Cleland s original report, literally thousands of references have cited the use of mainly DTT for the reduction of cystine and other forms of disulfides. [Pg.88]

Other more direct methods of assessing the oxygen coverage are available through AES (J 8), XPS (1 9), UPS ( 0) and other forms of electron spectroscopy. Figure 5 shows a nice example taken from the work of Tatsuo Matsushima and David Almy (1J3). In this work on polycrystalline Pt, a steady-state reaction was established at various temperatures with Pq2/Pc0 At time t = 0, the O2 pressure... [Pg.42]

In this case, direct electron transfer between the catalyst and O2 produces the superoxide radical (or other reduced forms of oxygen) which can be involved in a series of subsequent redox reactions. If these reactions are relatively fast, the rate determining step is Eq. (3) and the overall process can be interpreted in terms of relatively simple rate laws. [Pg.398]

Comparison of Reactions Involving Oxygen Ions on MgO. One of the most significant observations in this series of studies was the large difference in the reactivities of the three forms of oxygen ions on MgO. Taking ethylene as an example, 0 ions reacted readily at -60°C and 07 ions reacted at 25°C with a half-life of 5 min., whereas about two-thirds of the 07 ions remained unreacted after contact with CaHi at 175°C for 2 h. These results, which are qualitatively the same for other simple hydrocarbons, indicate that the order of reactivity is 0 07 07. [Pg.139]


See other pages where Other forms of oxygen is mentioned: [Pg.607]    [Pg.607]    [Pg.609]    [Pg.611]    [Pg.313]    [Pg.53]    [Pg.13]    [Pg.607]    [Pg.607]    [Pg.609]    [Pg.611]    [Pg.223]    [Pg.607]    [Pg.607]    [Pg.609]    [Pg.611]    [Pg.313]    [Pg.53]    [Pg.13]    [Pg.607]    [Pg.607]    [Pg.609]    [Pg.611]    [Pg.223]    [Pg.4]    [Pg.211]    [Pg.240]    [Pg.780]    [Pg.244]    [Pg.163]    [Pg.64]    [Pg.28]    [Pg.118]    [Pg.136]    [Pg.248]    [Pg.26]    [Pg.165]    [Pg.1004]    [Pg.1027]    [Pg.1038]    [Pg.26]    [Pg.455]    [Pg.254]    [Pg.24]    [Pg.24]    [Pg.44]   


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