Very high in Earth's atmosphere, there's a lot more atomic oxygen than anything else. Although I'm sure the energies involved in keeping oxygen in this state are an important variable, I'm interested (for now) in what compounds would form.

Mistake here: should be targeting $\ce{Li2O}$, not $\ce{LiO2}$. Would you get $\ce{LiO}$, then $\ce{LiO2}$? If so, will $\ce{LiO}$ be stable enough to bond with another $\ce{O}$ atom later? I can easily believe that lithium metal will simply erode away faster than a film of oxide could develop, given temperatures in the thermosphere and above. I just haven't seen much chemistry on this, however.

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    $\begingroup$ It would form $\ce{Li2O}$? $\endgroup$
    – DHMO
    Oct 10, 2016 at 14:30
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    $\begingroup$ In those conditions, nearly everything would prefer to stay atomic. $\endgroup$ Oct 10, 2016 at 14:46
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    $\begingroup$ You know, if you say metallic lithium, that implies a concentration of lithium atoms in a small area (or else it would not be able to form metallic bonding). $\endgroup$
    – DHMO
    Oct 10, 2016 at 14:55
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    $\begingroup$ Adding to the comment from @DHMO - look at a Li-O phase diagram. For an example, K. Chang and B. Hallstedt, CALPHAD 35 160-164 (2011). $Li_{2}O$ is much more stable than $Li_{2}O_{2}$ (as it is named there). $\endgroup$
    – Jon Custer
    Oct 10, 2016 at 15:23
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    $\begingroup$ $\ce{LiO}$ does not exist, $\ce{Li2O}$ does. $\endgroup$ Oct 10, 2016 at 17:22

1 Answer 1


As explained in Long-term ozone decline and its effect on night airglow intensity of Li 6708 ˚A at Varanasi (25◦N, 83◦E) and Halley Bay (76◦S, 27◦W) Journal of Earth System Science 120, No. 2, April 2011, pp. 291–300:

$\ce{Li + O -> LiO}$

$\ce{Li + O2 -> LiO2}$

$\ce{Li + O3 -> LiO + O2}$

$\ce{LiO2 + O -> LiO + O2}$

The article gives rate coefficients for each of these reactions.

The article also gives $\ce{Li}$, $\ce{O}$ and $\ce{O3}$ concentrations as a function of altitude for the range 80-99km (85km being considered the lower boundary of the thermosphere)


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