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I am reading a paper[1] that contains the line:

Most of the $\small H_2$ in the Earth's mantle escaped to space early in the Earth's history; consequently, the overwhelming majority of the abiotic geochemical reactions are based on acid/base chemistry, i.e., transfers of protons without electrons.

The connection between the loss of $\small H_2$ and acid/base chemistry is not clear to me.

Why would the loss of $\small H_2$ to space make acid/base chemistry the default?

  1. Falkowski, P. G., T. Fenchel, and E. F. Delong. (2008) The microbial engines that drive Earth's biogeochemical cycles. Science 320:1034-1038.
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I think what is happening here is this... we know we have abundant H2 gas today, so where did it come from if all the H2 gas disappeared in the early stages of the Earth? I'm going to over-simplify the answer to this question. The author is alluding to acid-base chemistry as the explanation for the existing H2 gas, so it seems. –  LordStryker Aug 28 '12 at 14:46
    
I edited the LaTeX out of the title for indexing purposes, as the markup would end up showing on search engines, etc., otherwise. –  jonsca Aug 28 '12 at 22:51

1 Answer 1

up vote 2 down vote accepted

The statement you cite contains a reference to “How Earth’s atmosphere evolved to an oxic state: A status report”, D. C. Catling and M. W. Claire, Earth and Planetary Science Letters 237 (2005) 1–20. This paper in turns give some more details on this assertion, which I'll summarize below.

It all turns around the question of how reducing the prebiotic atmosphere was. The paper I cited above contains this quote:

before life existed the atmosphere contained mainly N2, with negligible O2, probably more CO2 than today, and only minor levels of reducing gases such as H2.

So, in the absence of widely available gases such as oxidative O2 or reducing H2, oxygen was mainly present as H2O and CO2. This means redox reactions are not big players in the overall chemical scheme of the periodic atmosphere, and acide-base reactions dominate (by default).

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