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Saturation range

Cells are generally operated using 1.5—6 wt % AI2O2 in the electrolyte. Saturation ranges between 6—12% AI2O2 depending upon composition and temperature. [Pg.97]

In Figure 10.1, it can be seen that even with substrate excesses of [S] = 20 KM> the saturation range is not yet reached. Conversely, the data in Figure 10.2 indicate that even for very small substrate concentrations ([S]=0.05 KM) the limiting case for the first-order reaction - when the rate is directly proportional to the substrate concentration - is not identical with the values from Eq. (1). [Pg.261]

Equation 8 has a standard error of estimate of 0.07 fraction gypsum saturation over the saturation range of 0.5-2.0. The equation is useful for monitoring the actual gypsum saturation... [Pg.258]

This equation shows discrepancies between experiment and theory in the saturation range. It gives better results for low stresses as compared with our approximation equation obtained from a simplified quasicubic model for molecular dislocations (Fig. 30)s7). [Pg.55]

Figure 53A illustrates the Hill plot of the 02 equilibrium curves of (a+CNp)A(aP)cXL in 0.1 M phosphate buffer at various pH values. The 02 equilibrium curves converge at a high-saturation range, as seen in (ap)A(aP)cXL, whereas the lower asymptotes diverge more than those of (aP)A(aP)cXL (see Miura et al. (1987). The 02 binding curves show high cooperativity at low pH, with a Hill coefficient value of 1.8. The estimated Kj (i = 1, 2, or 3) values are plotted against pH as shown in Fig. 53B. K3 of (a+CNP)A( P)cXL is observed to be less pH dependent than A and K2. Its value is very similar to those of K4 of (aP)A(aP)cXL and Hb A, which are essentially pH independent. The K value of (a+CNP)A(aP)cXL shows a pH dependence similar to that of K2 or K3 of (ap)A(aP)cXL rather than that of K of (aP)A(ap)cXL. The slope of the plot of P30 of (a+CNP)A(aP)cXL versus pH is about 0.6 at pH 7.1, which is steeper than that of (aP)A(aP)cXL,... Figure 53A illustrates the Hill plot of the 02 equilibrium curves of (a+CNp)A(aP)cXL in 0.1 M phosphate buffer at various pH values. The 02 equilibrium curves converge at a high-saturation range, as seen in (ap)A(aP)cXL, whereas the lower asymptotes diverge more than those of (aP)A(aP)cXL (see Miura et al. (1987). The 02 binding curves show high cooperativity at low pH, with a Hill coefficient value of 1.8. The estimated Kj (i = 1, 2, or 3) values are plotted against pH as shown in Fig. 53B. K3 of (a+CNP)A( P)cXL is observed to be less pH dependent than A and K2. Its value is very similar to those of K4 of (aP)A(aP)cXL and Hb A, which are essentially pH independent. The K value of (a+CNP)A(aP)cXL shows a pH dependence similar to that of K2 or K3 of (ap)A(aP)cXL rather than that of K of (aP)A(ap)cXL. The slope of the plot of P30 of (a+CNP)A(aP)cXL versus pH is about 0.6 at pH 7.1, which is steeper than that of (aP)A(aP)cXL,...
The 02 equilibrium curves of asymmetric cyanomet hybrid Hbs with two cyanomet subunits—(a+CNp+CN)A(aP)cXL and (aP+CN)A (a+CNp)cXL—were also measured. However, it was not feasible to estimate reliable values of Kt and by curve fitting (Miura et al., 1987). We found that it was difficult to fit the 02 binding scheme with two binding constants over the entire saturation range of the... [Pg.270]

In the second alternative, i.e. with the quench, the task is to reduce an excessive steam/gas ratio. Method B shows one way of doing this. A waste heat boiler is located downstream of the quench. It operates in the saturation range of the gas. The excess water is removed by means of partial condensation of the water vapour, thus producing the desired S/G ratio. The heat of condensation obtained can be utilized for generating steam. The pressure of the steam generated in this way can, at the most, only correspond to the partial pressure of the steam within the gas. This method will therefore only be advisable when the total pressure is at an appropriately high level. [Pg.158]

In Fig. 1 the super saturation range is located below the equilibrium curve corresponding to the equality fis,oo = fie,oo- In the case when ps < / c>00, the difference Ps Pc,oo <0 defines the electrochemical undersaturation, which, if applied, would cause the electrochemical dissolution of the bulk liquid or crystalline new phase. Thus, the quantity Ap defines the thermodynamic driving force of the two opposite types of electrochemical first-order -+ phase transition and it is of fundamental importance to express it by means of physical quantities, which can be easily measured and controlled. [Pg.648]

For the saturation range, S = 60-70 % (which is the transition region) on the other hand, there is a minimum for the three pressure applications. This tendency is seen better in the Fig.3. [Pg.578]

In the saturation range, all injected electrons are forced to move into the bulk and measured as a current. The current was found to be proportional to the light intensity. It should be emphasized that we have here a photocurrent caused by the injection of majority carriers, whereas an excitation within the semiconductor itself always leads to the transfer of minority carriers across a corresponding interface. The same results have been obtained with other semiconductor electrodes such as ZnO [28], Ti02 and SnS2 [21, 22]. [Pg.312]

Similarly, we used correlations developed by Fulcher et al. (1985) by fitting their experimental data to calculate the ratio of water to oil. The k, ratio of a high IFT system is compared with that of a lower IFT in Figure 7.40. The same observation can be made from this figure. We also checked other pubhshed data (not shown here to avoid tedious presentation), and they all show that the k, ratio is decreased when IFT is lower thus, the oil displacement efficiency is improved in the high aqueous phase saturation range as IFT is reduced. [Pg.322]

In order to force the energy balance to result in a flat curvature spectrum, the dissipation term -fikE is replaced by a different one, SS(j (E), the shape of which is chosen exactly so that it balances the energy input terms if B(k) is flat. Although this is somewhat artificial, the same argument has been used by Phillips (1985) in his attempt to obtain a k05 curvature spectrum. Reverting to a constant a4, we obtain (in the saturation range) ... [Pg.211]

Concerning the actual choice of p and p2, it can be noted that p = 0, p2 = 2 would lead to a trivial equation for the energy balance. The next simplest choice is 7>i =p2= 1, and this will be used. This means that we take the dissipation in the saturation range proportional to E2. (Calculations have been made for various combinations of p and p2 taken from 0, 1,2, and they actually give rather similar results.)... [Pg.212]

The results are shown in Fig. 1. In this calculation, a neutrally stable atmosphere with Tair = Tsea = 10 °C is used, and the wave age is set at 25. No slicks are used. (In the standard VIERS-1 spectrum, a wind-dependent slick coverage is assumed.) The integration over the saturation range gives rise to a flat curvature spectrum, as it should, and the overall shape of the spectra is practically identical to the original VIERS-1 form. [Pg.212]

Fig. 2. Curvature spectrum B(k) for wind speeds Uw = 6, 10, 15 m s 1, according to the RAW model (dashed) and the DBJ model (dotted). The spectral level in the saturation range (half the Phillips constant ) was set to the same value as in Fig. 1... Fig. 2. Curvature spectrum B(k) for wind speeds Uw = 6, 10, 15 m s 1, according to the RAW model (dashed) and the DBJ model (dotted). The spectral level in the saturation range (half the Phillips constant ) was set to the same value as in Fig. 1...
The fact that in the saturation range the computed relaxation rate is realistic, means that the choice oip =p2 = 1 in Eqs. 15, 18 appears to be justified. The values of p and p2 determine to which of the coefficients f, f2 or f3 the breaking terms Ssd (that were introduced, Eq. 15, to force a flat saturation spectrum) contribute, thereby directly influencing p. [Pg.217]

Figures 6 and 7 show the effect of a slick on the computed relaxation rate. The same slick as for Fig. 3 was used. In the saturation range, the presence of the slick lowers the relaxation rate by the same order of magnitude as it lowers the spectrum. Around k = 100 rad m"1, the slick leads to a more stable spectrum. In the capillary range (k > 200 rad m"1) the relaxation rate is reduced by exactly the same factor as the spectrum, regardless whether // is positive or negative. Figures 6 and 7 show the effect of a slick on the computed relaxation rate. The same slick as for Fig. 3 was used. In the saturation range, the presence of the slick lowers the relaxation rate by the same order of magnitude as it lowers the spectrum. Around k = 100 rad m"1, the slick leads to a more stable spectrum. In the capillary range (k > 200 rad m"1) the relaxation rate is reduced by exactly the same factor as the spectrum, regardless whether // is positive or negative.
Here I, represents the drain current and ju, jUp the respective electron and hole mobility. C defines the area capacitance of the insulator. The channel geometry is defined by the channel width W and length L. The ambipolar range, described by Eq. (3), is only valid as long as both electrons and holes can be injected and further transported in the active layer of the transistor. However, in most cases the injection and/or the transport in the transistor channel are suppressed for one charge carrier type. In that case, the FET operates only in the unipolar and saturation range as described by Eqs. (1) and (2). [Pg.515]

Second, after foam flooding cores, Bernard et al. (32) flushed with water or brine to estimate trapped-gas saturation. They assumed that water or brine filled the pore space through which gas flowed but did not substantially alter the fraction of gas trapped. Their trapped saturations ranged from 10 to 70% depending upon the surfactant type and the presence of oil in the porous medium during the foam flood. Such measured saturations apply only to trapped gas following a waterflood, and not to dynamic or steady-state foam flooding. [Pg.128]


See other pages where Saturation range is mentioned: [Pg.305]    [Pg.71]    [Pg.267]    [Pg.1488]    [Pg.160]    [Pg.194]    [Pg.287]    [Pg.70]    [Pg.75]    [Pg.606]    [Pg.4]    [Pg.360]    [Pg.267]    [Pg.134]    [Pg.396]    [Pg.12]    [Pg.648]    [Pg.577]    [Pg.152]    [Pg.527]    [Pg.220]    [Pg.7]    [Pg.321]    [Pg.390]    [Pg.205]    [Pg.210]    [Pg.221]    [Pg.515]    [Pg.38]    [Pg.143]    [Pg.152]   
See also in sourсe #XX -- [ Pg.205 , Pg.210 , Pg.211 , Pg.214 , Pg.217 , Pg.218 , Pg.221 ]




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