Chemistry, 13.09.2019 02:30 mgollaoutlaw35
Just as the depletion of stratospheric ozone threatens life on earth today, its accumulation was one of the crucial processes that allowed life to develop in prehistoric times: 3o2(g) → 2o3(g) at a given instant, the reaction rate in terms of [o2] is 2.17 × 10−5 mol/l·s. what is it in terms of [o3]? enter your answer in scientific notation.
Answers: 2
is 
![-\frac{1}{3}\frac{\Delta [O_{2}]}{\Delta t}=\frac{1}{2}\frac{\Delta [O_{3}]}{\Delta t}](/tpl/images/0229/5301/d09c4.png)
![-\frac{\Delta [O_{2}]}{\Delta t}](/tpl/images/0229/5301/8d0a6.png)
represents rate of disappearance of 
and ![\frac{\Delta [O_{3}]}{\Delta t}](/tpl/images/0229/5301/a4078.png)
represents rate of formation of ![-\frac{\Delta [O_{2}]}{\Delta t}=2.17\times 10^{-5}mol/L.s](/tpl/images/0229/5301/30722.png)
So, ![\frac{\Delta [O_{3}]}{\Delta t}=\frac{2}{3}\times -\frac{\Delta [O_{2}]}{\Delta t}=\frac{2}{3}\times (2.17\times 10^{-5}mol/L.s)=1.45\times 10^{-5}mol/L.s](/tpl/images/0229/5301/a8f01.png)
Hence rate in terms of formation of 
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