rjh01 said:
- Minerals are composed of elements

Gee, I've taken innumerable geology classes and have five years' experience in the field and no one EVER told me that!!!!!
Yes, minerals are composed of elements. However, when dealing with density THAT DOES NOT MATTER. Ships are composed of iron. Iron sinks. Ships, unless someone puts a hole in them, do not. Gee, I wonder why that is. Volcanic glass sinks, but for some reason pumice floats! Oxygen and hydrogen are gasses, so H2O should have slightly more boyancy than oxygen, right?
Unless we are dealing with native elements, the density of the element is only part of the story. The density of the mineral it's in is the rest of it--the part you persist on ignoring. And if you're going to persist in assuming that only one element is important in that calculation you will look progressively more ridiculous.
- I agree that once the Earth cooled then any uranium (or anything else for that matter) that was on the surface would stay on the surface (ignoring plate tectonics)
You'd be wrong. Particularly the "anything else" part and the "ignoring plate tectonics" part. Huge volumes of material have been subducted well into the mantle, sometimes coliding with the outer core. If you want to argue otherwise, please find me a Frasnian-aged piece of oceanic crust that hasn't been thrust onto a continent.
- Minerals are made up of elements. Any time I have mentioned elements it also includes minerals
You can redefine the words to your heart's content--just don't say that I'm the one that doesn't make sense. Elements are elements. Minerals are composed of one or more elements. If you use "elements" to mean "minerals" you are wrong by every definition of the words.
- Uranium minerals would have to have a huge % of other elements to make it less dense than iron oxide
You obviously know very little about minerology. Here's a hint: silica tetrahedrons can form minierals of varying density. Yes, yes, I know uranium ores aren't usually silicates, but it's the principle I'm driving at here, not the specifics.
Or, go back to the ship idea. Iron sinks. Steel ships float. Obviously, elemental composition is not the only factor here. It gets even more complex when you're talking about crystalization (because now you're not just talking the boyancy of a single element, but of minereal SYSTEMS [ie, if one mineral is captured within another one, something not uncommon in igneous rocks, the density of the whole system must be considered, not just any one crystal and especially not any one element]).
As for uraninite, again (and for the last time), I merely chose a uranium ore I could remember the composition of. I did not intend that to be an exhaustive listing of uranium ores.
- If the % of uranium in the core is very small it would not be mentioned by most references.
Define "most references". And you're ignoring half the equation. There's a large amount of uranium at the surface.
Here's some light reading.
While normally I shun Wiki for technical discussions, this article isn't bad and it hits a number of points that you're ignoring. For example, uranium is more abundant than silver (a lighter element) in the crust, and it's highly mobile in alkaline pH solutions (not as rare as people assume in the oceans).
The issue isn't "What happened to the uranium when the Earth was formed?" We know what happened--a lot of it (everyone I've talked to argues most of it) is at the surface. The issue you need to address is "Why is there so much at the surface?" Because even if it's not most of the uranium there's a remarkable amount up here. I may be wrong about the density thing, but simply pretending that there's not a large amount of uranium is simply bad science. It requires you to ignore data. I've proposed a mechanism; you've proposed flaws. Okay, hot shot--what mechanism do YOU propose? Because there's got to be one; the uranium's here somehow.
- Oxygen and other lighter elements could be in the core because it came down with other elements as part of various minerals, like iron oxide.
I need to find that smiley that shows a guy bashing his head against a wall....If you understand how LIGHT elements can be brought DOWN due to the difference between a mineral and an element, you can apply the same principle to explain why HEAVY elements were brought UP. It actually is precisely the same principles, merely different applications. You've already accepted what I'm arguing, you simply refuse to acknowledge the necessary implications of your own statements.
Also, to play by your rules I should now consider ALL minerals that contain oxygen to be iron oxide. Nothing else--just iron oxide. There are no other oxides, because you've only mentioned iron oxide. I can assume that silicates don't include oxygen, because you've only mentioned iron oxide.
Do you see where that can get extremely frustrating?
If it was iron that went to the core then it would have been uranium also that went to the core for the same reasons.
And ya backslid. If you can prove that all the uranium was UO2 while the Earth was molten, I'll consider agreeinig with you. Good luck with that.
I have now answered every one of your petulant "points to answer". Can we now have a grown-up discussion, or are you going to continue to refuse to read what I've written and make assinine assumptions about what I've said that contradict what I've said? I'm not asking you to agree with me--I'm merely asking you to acknowledge my points as written. I'm also not asking you to respect me--anyone who hands another person a list of "points to answer" has no respect for the other person. I'm just asking for an honest hearing, which I thus far have not gotten.
Libra said:
I always understood that the geophysical work that's been done on the Earth's core, utilised seismic events as the energy source to track the propagation of various waves and the results of this, in combination with aspects like thermal and moment of inertia, was used to infer the model.
Is this still the case ?
My understanding is that experimental minerology is also used. It's one thing to estimate the density and temperatures; it's another entirely to estimate composition. The latter requires some good old-fashioned lab experiments. Had a friend that switched from paleo to doing exactly that (only for the mantle, not the core). Phase diagrams and the rest are wonderful tools, but there are more things in Heaven and all that.
I am assuming that just as much, or perhaps maybe more, variation could be expected between the current inferred model and the actual ?
The structural stuff is at the 1:1,000,000,000 scale.
