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Gases common

Absorption of pollutant gases is accomplished by using a selective liquid in a wet scrubber, packed tower, or bubble tower. Pollutant gases commonly controlled by absorption include sulfur dioxide, hydrogen sulfide, hydrogen chloride, chlorine, ammonia, oxides of nitrogen, and low-boiling hydrocarbons. [Pg.478]

Table 4.6 Gases commonly stored in liquefied form ... Table 4.6 Gases commonly stored in liquefied form ...
GC is particularly useful in soil analysis because of both the wide variety of columns available for separating specific mixtures and because of the variety of very sensitive detectors available. There are specific columns for separation of gases commonly found in the soil atmosphere and specific columns for the analysis of herbicides, insecticides, and pollutants. [Pg.186]

Table 7-1 gives an overview of various irritant and nonirritant gases commonly found in the atmosphere, their solubility in water, and their main sites of action. The Henry s law constant indicates the relative solubility in waterlike lung fluid. Although most of the information goes back to 1924, it is supported and extended by numerous studies of the effects of war gases and industrial irritants. - " ... [Pg.282]

Key material properties for SOFC, such as the ionic conductivity as a function of temperature, are available in refs 36—39. In addition, Todd and Young ° compiled extensive data and presented estimation methods for the calculation of diffusion coefficients, thermal conductivities, and viscosities for both pure components and mixtures of a wide variety of gases commonly encountered in SOFCs. Another excellent source of transport properties for gases and mixtures involved in a SOFC is the CHEMKIN thermodynamic database. ... [Pg.493]

Natural gases commonly contain hydrogen sulfide, carbon dioxide, and nitrogen. The presence of nitrogen does not greatly affect the z-factor obtained by methods previously described z-factor increases by about 1% for each 5% of nitrogen in the gas.9... [Pg.120]

The equivalent values for inert gases commonly used are given in Table 6.6. The inert gases show a similar range in molecular mass and density with reference to air. [Pg.139]

Looking at Table 6.6, it is obvious that the inert gases commonly available cover a few points only in density range to comply with the requirements for a test gas given in the p-standards. Thus, a mixture of two test gases A, B with molecular weights MA, Mg can substitute the flammable gas C with molecular weight Me-... [Pg.142]

Table 3.2. Correction for non-ideality for a few gases commonly used in adsorption experiments. Table 3.2. Correction for non-ideality for a few gases commonly used in adsorption experiments.
Diffusivities in liquids are very much lower than dif-fusivities in gases, commonly by a factor of 10". ... [Pg.3876]

A third type of double-replacement reaction that occurs in aqueous solutions results in the formation of a gas. Some gases commonly produced in these reactions are carbon dioxide, hydrogen cyanide, and hydrogen sulfide. [Pg.296]

Type 1 isotherms exhibit prominent adsorption at low relative pressures p/po (the relative pressure p/po is defined as the equilibrium v or pressure divided by the saturation vapor pressure) and then level off. Type 1 isotherm is usually considered to be indicative of adsorption in micropores (e.g., adsorption of benzene on microporous active carbon) or monolayer adsorption due to the stror adsorbent-adsorbate interactions (which may be the case for chemisorption, which involves chemical bonding between adsorbate and the adsorbent surface, e.g., adsorption of hydrogen on iron). In the case of nonpolar gases commonly used for charactmzation of porous solids (nitrogen, argon) [10, 12, 13, 17, 56], chemisorption is unlikely and therefore e I reflects usually adsorption on microporous solids. However, type I isotherms may also be observed for mesoporous materials with pore size close to the micropore range. In particular, in the case of adsorption of N2 at 77 K or Ar at both 77 K and 87 K in cylindrical pores, a type I isotherm would have to level off below the relative pressure of about 0.1 for the material to be exclusively microporous, as inferred fi-om tile results of recent studies of siliceous and carbonaceous ordered mesoporous materials (OMM) [57-59]. Consequently, when a type 1 isotherm does not level off below the relative... [Pg.115]


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See also in sourсe #XX -- [ Pg.217 ]




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