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Water Content of Air Fig

FIG. 2-4 Water content of air, = ( F — 32) X handshaum, Dadds, and Stutzman. Repiinted from -doI. 47, januaiy 1955 issue of Ind. Eng. Chem. [p. 192]. Copyright 1955 hy the American Chemical Society and r eproduced hy permission of the copyright owner )... [Pg.134]

Fig. 16-4 pH sensitivity to SO4- and NH4. Model calculations of expected pH of cloud water or rainwater for cloud liquid water content of 0.5 g/m. 100 pptv SO2, 330 ppmv CO2, and NO3. The abscissa shows the assumed input of aerosol sulfate in fig/m and the ordinate shows the calculated equilibrium pH. Each line corresponds to the indicated amoimt of total NH3 + NH4 in imits of fig/m of cloudy air. Solid lines are at 278 K, dashed ones are at 298 K. The familiar shape of titration curves is evident, with a steep drop in pH as the anion concentration increases due to increased input of H2SO4. (From Charlson, R. J., C. H. Twohy and P. K. Quinn, Physical Influences of Altitude on the Chemical Properties of Clouds and of Water Deposited from the Atmosphere." NATO Advanced Research Workshop Acid Deposition Processes at High Elevation Sites, Sept. 1986. Edinburgh, Scotland.)... [Pg.427]

The RM of the dried product was measured at 50 °C over P205 or in an oven with circulating air at 50 °C, or in the same oven at 90 °C over silica gel. Identical measurements were made with fresh bones. For NMR measurements, a known amount of D20 was added to the bone in a glass container. After equilibrium between DzO and H20 was reached, a known amount of the product was taken from the solution and studied in a Perkin Elmer NMR-spectrometer. In Fig. 3.23 the water contents of fresh and freeze dried bones are listed measured by NMR and the gravimetric methods at 90 °C. The data show that only a certain amount of the total water can be removed at 90 °C, while another amount is so... [Pg.228]

Acid Dew Point For fossil fuels, the acid dew point temperature is that temperature at which the actual mixed acid vapor pressure equals the mixed acid vapor saturation pressure. The mixed acid dew point can be approximated by the sulfuric acid dew point (Fig. 24-56). It can be described as a function of the SO3 and water content of the flue gas (Huijbregts). These concentrations result from the sulfur, hydrogen, and free water content of the fuel the relative humidity of the air and the amount of excess air used. Using the equation of Ver-hoff, where T is degrees K and P is mm Hg (see OUces, A.G.) ... [Pg.52]

Fig. 1. Water content of saturated air at various temperatures and pressures... Fig. 1. Water content of saturated air at various temperatures and pressures...
Fig. 5. Water content of different secipitated silicas at 50% air humidity. Fig. 5. Water content of different secipitated silicas at 50% air humidity.
The relationship between i/j and the water content of a porous medium is also determined empirically Fig. 3-23 shows typical ijs — 0 curves. When is zero, the porous medium is at its saturated moisture content, which is equal to porosity (assuming that there is negligible trapped gas). The pressure head can become somewhat negative before air enters (and water leaves) some soils the value ijja at which air begins to enter is called the air entry value. Water leaves the matrix as i/j (defined as pressure head) becomes more negative than ifsa as water leaves the soil, the hydraulic conductivity also decreases. [Pg.243]

Polymeric proton exchange membrane needs to be maintained properly humidified to guarantee a satisfactory ion conductivity during stack operation (see Sect. 3.2). In fact it exists a strong relationship between proton conductivity and water content of Nafion material used as membrane in PEMFC [24, 25]. Unfortunately the water produced at cathode side and the air moisture could be not sufficient to maintain properly wet the membranes in all working conditions, because of complex phenomena involving water within MEA [26] (Fig. 4.7). [Pg.116]

Fig. 4. Effects of drought and NaCl pretreatment on the leakage of electrolytes from leaves of chilled rice seedlings. Drought pretreatment seedlings were air-dried, maintained in light for 8 h until leaves were rather wilted and the water content of leaves had decreased from 82% to 75%. Plants were then rewatered for 1 h to recovery. NaCl pretreatment seedlings were removed to 0.1 mol/1 NaCl solution for 24 h, then changed to distilled water. Plants from both treatments were then exposed to 8-10 C. /, 2 Dansheng No. 3,4 Guichao No. 2 7, 3 control 2, 4 treatment [see 12]... Fig. 4. Effects of drought and NaCl pretreatment on the leakage of electrolytes from leaves of chilled rice seedlings. Drought pretreatment seedlings were air-dried, maintained in light for 8 h until leaves were rather wilted and the water content of leaves had decreased from 82% to 75%. Plants were then rewatered for 1 h to recovery. NaCl pretreatment seedlings were removed to 0.1 mol/1 NaCl solution for 24 h, then changed to distilled water. Plants from both treatments were then exposed to 8-10 C. /, 2 Dansheng No. 3,4 Guichao No. 2 7, 3 control 2, 4 treatment [see 12]...
Rather different chemistry is displayed by small rhodium carbonyl clusters on the surfaces of these oxides. Much of this is dominated by the same equilibria as in solution, between [Rh(C0)2X]2> Rh4(C0)i2 Rh5(C0)] 5. As in solution, the species observed are very sensitive to the acidity and water content of the reaction media. Rh4(C0) 2 is substantially converted to Rh5(C0)i5 on a dried silica surface [62] this can be inhibited by a CO atmosphere. Treatment with water and air affords metallic particles and Rh sites, respectively [62,63]. A similar sensitivity to pretreatment is observed on an alumina surface. The proportions of the initially observed species also vary with the degree of hydroxylation of the alumina, with these being principally Rh6(C0)] 5 and Rh (C0)2 sites (Fig. A) [62,64-66] this provides an active water gas shift catalyst [44]. [Pg.56]

Cautiously add 250 g. (136 ml.) of concentrated sulphuric acid in a thin stream and with stirring to 400 ml. of water contained in a 1 litre bolt-head or three-necked flask, and then dissolve 150 g. of sodium nitrate in the diluted acid. Cool in a bath of ice or iced water. Melt 94 g. of phenol with 20 ml. of water, and add this from a separatory funnel to the stirred mixture in the flask at such a rate that the temperature does not rise above 20°. Continue the stirring for a further 2 hours after all the phenol has been added. Pour oflF the mother liquid from the resinous mixture of nitro compounds. Melt the residue with 500 ml. of water, shake and allow the contents of the flask to settle. Pour oflF the wash liquor and repeat the washing at least two or three times to ensure the complete removal of any residual acid. Steam distil the mixture (Fig. II, 40, 1 or Fig. II, 41, 1) until no more o-nitrophenol passes over if the latter tends to solidify in the condenser, turn oflF the cooling water temporarily. Collect the distillate in cold water, filter at the pump, and drain thoroughly. Dry upon filter paper in the air. The yield of o-nitrophenol, m.p. 46° (1), is 50 g. [Pg.677]


See other pages where Water Content of Air Fig is mentioned: [Pg.46]    [Pg.46]    [Pg.138]    [Pg.157]    [Pg.75]    [Pg.299]    [Pg.46]    [Pg.75]    [Pg.54]    [Pg.306]    [Pg.387]    [Pg.460]    [Pg.522]    [Pg.256]    [Pg.242]    [Pg.104]    [Pg.504]    [Pg.128]    [Pg.450]    [Pg.147]    [Pg.319]    [Pg.106]    [Pg.103]    [Pg.255]    [Pg.433]    [Pg.440]    [Pg.273]    [Pg.287]    [Pg.525]   


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Air contents

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