Does this sound backwards to you as it does to me?
If it stopped absorbing Neutrons as water was deminished that would SPEED UP the reaction.
Yep, sounds backward to me, too. And I can't pretend to understand it. Thought it was fascinating, though, that there was a natural fission reactor on Earth that ran safely, unattended for 150 million years!
You are absolutely correct. More later.
As for "and storing its own waste in a safe manner.", others I've read (ages ago) have hypothesized the site as one of the main drivers of the initial diversification of life through the halo of higher than normal radiation induced mutation around the structure...
Depends on the type of reactor the dynamics of the natural core. Funny thing is, natural cores act have a tendency to act the opposite of what was just described, i.e, + void coefficient of reactivity. Some have the opposite effect.
I'm not sure, but if the water absorbs an atoms neutrons, it destabilizes the atomic weight of the atom losing the neutron and that then creates the reaction with another atom. That's why as it steams out, the reaction settles don.
The water wasn't "absorbing" the neutrons, it was changing their speed. If neutrons are moving too fast, they cannot be "captured" by the uranium-235 muclei, and fission won't occur. The protons (hydrogen atoms) of the water are very similar in size to a neutron, so when a neutron hits a proton, it loses its kinetic energy to it (think one billard ball hitting another--the first ball slows down drastically or stops completely, and the second "zips away" from the collision site). If the water is converted to steam, its density goes down by a factor of >1000, and the possibilities of a neutron hitting a proton and slowing down also drop. Therefore there are fewer "slow" neutrons available to be captured, and the fission process slows down.
See my comments on reactivity in Nbr 32 & 33.
That's sharp thinking! You are correct about the discrepancy. Perhaps, what the author meant to say was that the water acted as a moderator, much like graphite did, when it was used in the crude reactors of the 1950's.
The graphite slowed the neutrons enough that their absorption was more likely by the uranium 232. Else the neutrons were simply lost to the reaction, and the reaction would diminish.
What the author didn't remark on was that Uranium 238 will also absorb neutrons, and after a microsecond or so as uranium 239, will emit an electron and become neptunium 239. The Neptunium 239 will then after a few microseconds emit yet another electron and become Plutonium 239, which, if my old memory doesn't fail me from so long ago then has a half-life of 24,000 years.
If in fact, this reaction has occurred as postulated, the presence of Plutonium, (a case of the world's first natural slow-breeder reactor), would be discovered.
At least, that's what they taught us back in the 70's.