I've been thinking about ammonia and its role in the early atmosphere.
The early atmosphere was apparently reducing which, put another way, meant that the atmosphere was filled with reducing agents (elements/molecules that would donate electrons); however, I'm having trouble fitting this with the ammonia molecule.
Oxidation can be thought of in a few ways, but I'll focus on electron transfer and hydrogen transfer. From what I've learned, oxidation can be thought of as either losing electrons or losing hydrogen. Unfortunately, these two definitions seem to clash with the ammonia molecule, and I haven't been able to reconcile the difference.
NH
3 + H
+ --> NH
4+In this example there has been no change in the oxidation state for nitrogen (no reduction and no oxidation); however, it has clearly gained a hydrogen (reduction by the second definition).
How can NH
3 be a reducing agent (something that is oxidized) if reactions like the above are either non-redox or reduction reactions? Moreover, how come these definitions can lead to two different answers as to whether something is or isn't a redox reaction?
Any input is greatly appreciated
Edit: I thought I would post the link I used to learn about the different definitions of reduction and oxidation, just in case my explanation wasn't clear:
http://www.chemguide.co.uk/inorganic/redox/definitions.html