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Photochemical rate

Figure 5.4. Etch rate for PTFE at 248 nm and 300 fs pulse width. ( ) Kuper and Stuke experimental data — Baba et al. model, (--) photothermal rate, and (---) photochemical rate. Figure 5.4. Etch rate for PTFE at 248 nm and 300 fs pulse width. ( ) Kuper and Stuke experimental data — Baba et al. model, (--) photothermal rate, and (---) photochemical rate.
However, even if such measurements were possible, would the uncertainty of the result be small enough to establish that production does indeed balance observed loss of ozone The calculation of ozone loss in the Antarctic ozone hole was shown to have an uncertainty of 35 to 50%. The uncertainty for analyzing whether production balances loss in the midlatitude stratosphere is similarly 35 to 50%. About half of the uncertainty is in the measurements of stratospheric abundances, which are typically 5 to 35%, and half is in the kinetic rate constants, which are typically 10 to 20% for the rate constants near room temperature but are even larger for rate constants with temperature dependencies that must be extrapolated for stratospheric conditions below the range of laboratory measurements. In addition to uncertainties in the photochemical rate constants, there are those associated with possible missing chemistry, such as excited-state chemistry, and the effects of transport processes that operate on the same time scales as the photochemistry. Thus, simultaneous measurements, even with relatively large uncertainties, can be useful tests of our basic understanding but perhaps not of the details of photochemical processes. [Pg.163]

A similar analysis for the photochemical rate replaces the rate of thermal initiation, 2 1[Br2][M], by the rate of photochemical initiation 2/abs, giving... [Pg.216]

The individual values of k and k remain to be found, and these can be easily found if the photochemical rate is known. From Equations (6.96) and (6.99) the ratio of the two rates can be shown to be... [Pg.218]

Note, the argument involving the ratio of the photochemical rate to the thermal rate as a route to the determination of k only holds because the mechanisms for both reactions are the same. This method would not work with the photolysis and thermal decomposition of propanone, see Worked Problem 6.2 and Further Problem 4. These two reactions have totally different mechanisms the photolytic reaction has a nonchain mechanism whereas the thermal decomposition, which occurs at a much higher temperature, has a chain mechanism. [Pg.218]

In the absence of light scattering, the first-order photochemical rate constant can be rewritten as... [Pg.80]

In this case, 1 einstein (ein) is equal to 1 mole of photons. Furthermore, the photochemical rate of reaction can be expressed as follows for a well-controlled laboratory reactor or vessel with a primary reactant and chro-mophore, A ... [Pg.100]

A final but not unimportant check is provided by the rate constants and temperature coefficients of the photochemical rate constants. From Eqs. (XIII.4.8) and (XIII.4.6) the over-all photochemical rate of formation of IIBr in the absence of wall effects may be written as... [Pg.329]

G. K. Rollefson and M. Burton, Thotochemistry and the Mechanism of Chemical Reactions, p. 302, Prentice-Hall, Inc., hJnglewood Cliffs, N.J., 1939, have warned against the simple algebraic summation of thermal and photochemical rates when both mechanisms are operative. In this latter case (Br)Bs = [Ki 2(Br2) + ==... [Pg.329]

Cto 218 °C has been studied by Bodenstein and Lutkemeyer . They showed the photochemical rate of HBr formation to be accurately proportional to the square root of the absorbed light intensity. This implies that the mechanism of HBr production involves the attack of Br atoms on H2 molecules to give HBr and H. The rate otherwise depended in the same way on Hj, HBr and Br2 as the thermal experiments. [Pg.209]

Identification of the photoactive state is a prerequisite to the calculation of the photochemical rates by comparison of the photochemical yields and luminescence lifetimes. Although measurements of steady state quenching and the dynamics of intermediate formation have been used to infer the reactive states in several complexes, there is still much to be done in this area. The effect of thermally accessible higher energy states can be minimized by reducing the temperature. [Pg.244]

Table III. Summary of Primary Photochemical Processes in Urban Air Estd. Upper Limit for Primary Photochemical Rate in Urban Air, P.P.H.M. Hour-1 ... Table III. Summary of Primary Photochemical Processes in Urban Air Estd. Upper Limit for Primary Photochemical Rate in Urban Air, P.P.H.M. Hour-1 ...
Figure 5.70. Upper panel Concentration (cm-3) of OH and HO2 as a function of the NOx (NO + NO2) mole fraction (pptv) for conditions representative of the upper troposphere (UT-solid line) and planetary boundary layer (PBL-dashed line). Lower panel Same, but for the net photochemical rate (ppb/hr) of ozone. The values corresponding to the upper troposphere are multiplied by 10. From Brune (2000). Figure 5.70. Upper panel Concentration (cm-3) of OH and HO2 as a function of the NOx (NO + NO2) mole fraction (pptv) for conditions representative of the upper troposphere (UT-solid line) and planetary boundary layer (PBL-dashed line). Lower panel Same, but for the net photochemical rate (ppb/hr) of ozone. The values corresponding to the upper troposphere are multiplied by 10. From Brune (2000).
Further, a change in temperature will modify all temperature-dependent photochemical rates and hence will feed back to the ozone chemistry. This renders the temperature-ozone relation into a tightly coupled and non-linear system that can be better understood with the aid of some simple chemical arguments. If a pure oxygen atmosphere is assumed (see Chapter 5), the interaction between ozone density and temperature dependent rates is expressed by ... [Pg.446]

As discussed in Chapter 3, the use of rate constants can be helpful for comparative purposes under the same irradiation conditions however, the quantitative expression of photochemical rate should be given in the terms of the quantum yield of the reaction. To determine the quantum yield in the solid state is unfortunately not a straightforward process. As a result, most studies in the literature refer to an apparent reaction order calculated from the degradation of a minor fraction of the sample. Such data should preferentially be supported by some detail of the reaction mechanism. [Pg.355]

Johnston, H. S., and G. Whitten (1973). Instantaneous photochemical rates in the global stratosphere. Pure Appl. Geophys. 106-108, 1468-1489. [Pg.670]

Johnston, H. S., O. Serang, and J. Podolske (1979). Instantaneous global nitrous oxide photochemical rates. J. Geophys. Res. 84, 5077-5082. [Pg.670]

Finally, the monochromatic accumulation rate Is Integrated over the solar spectrum to obtain the total accumulation rate. The results of this procedure are Illustrated In Figure 1, which shows the variation with depth of the photochemical rate of production of 2 2 midday at 40 N for summer and winter In a freshwater sample. A rapid decrease of Che rate with depth Is apparent, particularly In this dark colored freshwater sample which attenuates most of Che near-ultraviolet radiation In Che upper 20 cm. Figure 2 shows how Che calculated rate of photochemical production varies with time of day and extent of cloud cover at a chosen latitude and season. [Pg.253]

ApH therefore has an important control function in chloroplasts -it determines the efficiency of light capture by PSII by controlling both the rate of thermal dissipation and also the photochemical rate. The former involves unknown changes in the antenna chlorophylls. The latter could involve the initiation of a cyclic flow of electrons around PSII that would give photochemical quenching but not O2 evolution. Whilst this cycle is the best explanation for the in vitro data, photochemical dissipation of a different kind could be involved... [Pg.2886]

Our recent electronic structure calculations 3deld a potential energy surface adequate to explain, at least qualitatively and within the uncertainties due to an incomplete knowledge of relaxation rates, the available experimental observations for the hydrogen-iodine reaction. The rate expressions, the rate constants, their temperature dependence, the vibrational excitation of HI products, the excitation and/or dissociation of reactant I2, the photochemical rates - all are compatible with the recent ab initio potential energy surface and with the classical trajectory calculations carried out with a similar surface. And all are compatible with either the bimolecular or termolecular mechanisms. It appears most likely that both mechanisms contribute, but the matter is not resolved as yet. [Pg.175]

Like aU photolysis reactions, those initiated by vibrational overtone absorption are analyzed as first-order kinetic processes with a photochemical rate, /, which depends upon the absorption coefficient a(A) of the absorbing compound, the... [Pg.6]


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See also in sourсe #XX -- [ Pg.216 , Pg.218 ]




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Factors Controlling the Rate of Photochemical Degradation

Other Factors Affecting Photochemical Degradation Rates of Polymers

Photochemical formation rate

Photochemical isomerization rates

Photochemical rate equation

Photochemical reaction rate

Photochemical reactions chemical change rate

Photochemical reductive dissolution overall rate constant

Rate constants photochemical degradation

Rate constants, photochemical reaction

Rate constants. photochemical

Rate of photochemical initiation

Rate of photochemical reaction

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