Why Does Earth Have an Iron Core?

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Discussion Overview

The discussion revolves around the composition of Earth's nucleus, specifically why it is predominantly made of iron. Participants explore various theories and concepts related to planetary formation, differentiation, and the historical context of Earth's development.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • Some participants suggest that iron is the most common siderophile, which influences its concentration in the Earth's core.
  • Others argue that the lack of sufficient oxygen on Earth allows for a significant amount of iron to remain unbound, contributing to its presence in the core.
  • It is proposed that iron, when alloyed with siderophile elements, is denser than surrounding rocks, leading it to sink to the center during the differentiation process.
  • A historical perspective is provided regarding the iron catastrophe, where the sinking of iron and nickel due to heating and melting contributed to the formation of the core.
  • One participant mentions the significance of Earth's second-generation solar system status, indicating that much of its material originated from the remnants of a previous star, which predominantly produced iron as a final nuclear product.

Areas of Agreement / Disagreement

Participants present multiple competing views regarding the reasons for iron's predominance in Earth's nucleus, and the discussion remains unresolved with no consensus reached.

Contextual Notes

Some claims depend on specific definitions of siderophile and lithophile elements, and the discussion includes assumptions about the processes involved in planetary differentiation and the historical context of Earth's formation.

Chemist@
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Why is Earth's nucleus mostly made from iron?
 
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Chemist@ said:
Why is Earth's nucleus mostly made from iron?

1) Iron is the most common siderophile
2) Earth does not contain enough oxygen to bind to all iron. While a lot of iron is bound to oxygen and found in rocks, some of it concentrated in iron ores and some scattered, much iron is left over as metal.
3) Iron with siderophile alloying elements is denser than rocks and sinks to centre. Everything else is either siderophile and mixed with iron, or lithophile which mixes with less dense rocks and floats in top of iron.
 
http://en.wikipedia.org/wiki/Iron_catastrophe

The iron catastrophe was a major event early in the history of Earth. After accumulation of the Earth's material into a spherical mass, the material was mostly uniform in composition. While residual heat from the collision of the material that formed the Earth was significant, heating from radioactive materials in this mass further increased the temperature until a critical condition was reached, when the material was molten enough to allow movement. At this point, the denser iron and nickel, evenly distributed throughout the mass, sank to the centre of the planet to form the core - an important process of planetary differentiation. The gravitational potential energy released by the sinking of the dense NiFe globules increased the temperature of the protoplanet above the melting point resulting in a global silicate magma which accelerated the process. This event occurred at about 500 million years into the formation of the planet.
 
We have a second generation solar system, which means that much of the material came from the death of a previously-existing star. As stars gradually reach the end of their life, their chemical composition changes in the direction of the element that has the lowest amount of nuclear potential energy, which is iron. Iron is to nuclear reactions what ash is to combustion, an end product out of which no more energy can be extracted.
 
The catastrophe looks like Archimedes' law. Thanks for every answers. It is nice to understand nature as much as it is possible.
 

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