M
MeteorWayne
Guest
That's one of the points. Even if by some method the H and O were disassociated in the lower atmosphere, the lifetime of the separated atoms is seconds since they will recombine to create water again. It's a VERY efficient process. Only in the far outer reaches of the atmosphere is the contact time long enough, and the UV rate of disassociation high enough for oxygen to be liberated and hydrogen swept away.
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"In fact H2O one part hydrogen and two parts oxygen molecules do get released to form a water vapor atmosphere and as this water vapor enters the stratosphere condenses back to water in the form of attenuation. During this water cycle some of the hydrogen and oxygen ions break free from their bonds as was the case when our earth was primordial."
And what is there is not being returned to the lower atmosphere by "attenuation", whatever that is.
"
"In fact H2O one part hydrogen and two parts oxygen molecules do get released to form a water vapor atmosphere and as this water vapor enters the stratosphere condenses back to water in the form of attenuation. During this water cycle some of the hydrogen and oxygen ions break free from their bonds as was the case when our earth was primordial."
And what is there is not being returned to the lower atmosphere by "attenuation", whatever that is.