00:01
Quite a bit of writing on this, but not too hard.
00:04
A reaction that contributes to the depletion of ozone in the stratosphere is the direct reaction of oxygen atoms plus ozone.
00:13
And here's our product.
00:16
At 298 kelvin, the rate constant for this reaction is 4 .8 times 10 to the 5th.
00:43
Based on the units for the rate constant, we're asked to write the likely rate law.
01:13
And there are four parts to this.
01:16
So the rate constant, m to the minus 1, s to the minus 1, indicates that this is second overall.
01:30
So i would probably think that this would be 0 .03k equals rate.
01:46
That's what i would guess it would probably be.
01:48
It could also be the rate equals k times o squared or o3 squared.
02:06
It could be either one of those.
02:10
But i don't know if two of them like this, i would just guess it was the other one.
02:16
B.
02:19
What does b ask us? let's do each one of these on a separate page.
02:26
Would you expect this reaction to occur via a single elementary process? yes or no? and explain why.
03:03
We came up with yes here.
03:06
Most atmospheric processes are initiated by collision.
03:37
So we could imagine an activated complex of four o atoms collapsing to form two, 02 molecules.
04:19
Also our rate constant is pretty large and that is less likely for multi -step.
04:50
And based on information in the test this text, this react reaction is similar to to the destruction of 03 by chlorine atoms.
05:15
And your text this is 18 .7.
05:18
Equation 18 .7.
05:20
And this is also second order and has a large rate constant...