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The rate constant for that process is k = 1.8×10-12 cc molecules-1 s-1 e-1370/T where Ea/R = 1370 K. If you don't like molecules/cc as a concentration unit, 1 M = 6.023×1020 molecules/cc, but you'll find molecules/cc works just fine.
The daytime concentration of the reactants are [NO]0~3×108 and [O3]0~2×1012 molecules/cc. If we ignore [O] and therefore the other half of the NOX catalytic cycle (O+NO2®O2+NO), we see that NO is the limiting reactant...so much so that [O3] will be effectively constant at [O3]0. (HINT: that makes k[O3] fixed!)
The temperature at 20 km is about 220 K.
How many minutes will it take for stratospheric O3 to eat up 99% of the stratospheric NO at 20 km in the dark?
| [A]0 (M) | [B]0 (M) | [C]0 (M) | d[P]/dt (M/s) |
| 0.1 | 0.1 | 0.1 | 0.5 |
| 0.2 | 0.2 | 0.2 | 2.0 |
| 0.2 | 0.1 | 0.2 | 0.25 |
| 0.2 | 0.2 | 0.4 | 2.0 |
Indicate by the standard double dagger () where the
ABC activated complex is.Be that as it may, the question posed by this new bobsled run is whether or not it is as demanding as the above in terms of the requirement of part (b)? As that product channel gets bent further and further down toward the reaction one, will the demand in (b) become more acute or less relevent to reaction? Why? [HINT: Think like a bobsledder.]
Is Cu+(aq) stable in solution? If so, why? If not, what happens to it?
Note that it is exactly the average between the two standard reduction potentials in (8). Why must that be so? [HINT: Think DG.]
Deja vu.
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