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:

$3O_2(g)2O_3(g)$

At a given instant, the reaction rate in terms of $O_2$ is $2\mathrm{.}12{10}^{-5}\frac{\text{m}\text{o}\text{l}}{L*s}.$ What is it in terms of $O_3?$ Be sure your answer has the correct number of significant figures.

$\frac{\text{m}\text{o}\text{l}}{L*s}$