Composition of the Earth's core

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Discussion Overview

The discussion revolves around the composition of the Earth's core, specifically questioning the presence of heavier elements like uranium compared to the predominant elements of iron and nickel. Participants explore theories regarding the formation of the core during Earth's molten phase and the processes that led to the current elemental distribution.

Discussion Character

  • Exploratory
  • Debate/contested
  • Technical explanation

Main Points Raised

  • Some participants propose that the Earth's core is primarily composed of iron and nickel, with possible minor elements like sulfur and oxygen, based on prevailing scientific beliefs.
  • One participant suggests that the cosmic abundance of uranium is significantly lower than that of iron, which may explain its scarcity in the core.
  • Another participant notes that uranium tends to be found in less dense minerals, making it difficult for uranium to sink into the core during formation.
  • A participant expresses the assumption that heavier elements might be present in the core due to their sinking during planetary formation, linking this to the idea of radioactive decay contributing to the core's heat retention.
  • In response, another participant challenges this assumption, stating that while some heat in the Earth is radiogenic, the decay of uranium, thorium, and potassium primarily occurs in the mantle rather than the core.
  • This participant also mentions that the outer core is liquid and that heat is released during the crystallization process as the outer core solidifies into the inner core.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the presence of heavier elements in the core, with some arguing for their potential abundance and others disputing this notion based on elemental distribution and heat generation processes.

Contextual Notes

The discussion highlights uncertainties regarding the exact composition of the Earth's core and the processes involved in its formation, including the roles of density, elemental abundance, and heat generation mechanisms.

crazylum
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I understand that most scientists believe that the Earth's core is composed of iron, nickel and perhaps some other elements such as sulfur and oxygen. I also understand that they believe that the Earth's core formed during a time when the Earth was molten and that the core was formed by heavier elements sinking and compacting and lighter elements rising on convection currents. My question is if it was formed by this process why is it not composed of elements heavier than iron such as uranium?
 
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First you might consider the cosmic abundance of uranium in relation to iron. I think you'll find there's a hell of a lot more iron in the universe than there is uranium!

Second, uranium tends to get obund up in not especially dense minerals, like zircons, which makes it hard to sink.
 
Now this is interesting; I had always assumed ther were non-negligable amounts of heavy elements in the core. I heard a long time ago that the original heat of compression from Earth's formation should have been radiated away eons ago, and one speculation for why the core is taking so long to cool is decay of radioactive elements. From there, I guess I just assumed that these heavier elements must be more abundant in the core, having sunk there during planetary formation.
 
I don't know where you heard that, but it's wrong. Some of the heat generated in the Earth is radiogenic, although the decay of U, Th, and K is mainly occurring in the mantle. Note that the outer core is liquid, a lot of heat is released as latent heat of crystallization, as the outer core gradually freezes to develop the ever expanding inner core.
 

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