Earth & climate · the experiment
Rain iron on the young Earth
You take over the Copenhagen proto-Earth: a magma ocean, a rain of iron, three gases to follow. Four questions, from beginner to expert, to check what the core really swallowed.
1 · Explain the spared nitrogen
Beginner
Nitrogen likes metal more than hydrogen does, yet only 4% of it ends up in the core. Why?
2 · Double the iron's appetite
The study's limiting formula, for a gas fully dissolved in the magma and delivered before the planet reaches mass M₀: the share left outside the core is (M₀/M)^(D × core/mantle), where D measures the metal's appetite for that gas. Hydrogen delivered before 0.02 Earth masses, planet finished at 0.64, core 30% against 70% mantle, D = 1: about 23% remains.
Intermediate
What if iron liked hydrogen twice as much, D = 2?
3 · Raise the hydrogen budget
The study sets its total hydrogen from what is thought to hide in today's core: the equivalent of 9 Earth oceans in the reference model, 45 in the high variant.
Expert
With 45 oceans instead of 9, what share of the hydrogen does the core swallow during pebble growth?
4 · Dissolve twice as much CO
The solubility of carbon monoxide in magma is the most influential and least measured input. Suppose new experiments find it twice as large.
Expert
In the pebble scenario, the carbon left outside the core becomes…
Iron rain over
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