### The Xenon Paradox
Compared to chondritic meteorites, Earth’s atmosphere contains only about of the xenon () expected relative to other noble gases, such as krypton () and argon (). Two scientists discuss competing hypotheses for this "missing xenon."
Scientist 1
The missing xenon is sequestered in Earth’s deep interior. At pressures exceeding and temperatures above , which are characteristic of the core-mantle boundary, xenon ceases to be chemically inert. Under these extreme conditions, xenon reacts with iron () and nickel () to form stable intermetallic compounds that sink into the core. In contrast, krypton and argon do not form stable compounds with iron or nickel under core conditions, allowing them to remain in the atmosphere.
Scientist 2
The missing xenon escaped into space early in Earth's history. During the Hadean eon, solar extreme ultraviolet (EUV) radiation was much stronger than it is today. Xenon has a lower first ionization energy () than krypton () and argon (). Consequently, xenon was selectively ionized by EUV radiation. The resulting ions were dragged out of the atmosphere along with escaping hydrogen () ions driven by hydrodynamic escape. Because krypton and argon remained mostly neutral, they were unaffected by the electromagnetic drag and remained bound to Earth.
Suppose new laboratory experiments demonstrate that at pressures of and temperatures of , krypton and argon form stable intermetallic compounds with iron and nickel that are just as stable and dense as those formed by xenon. This finding would most directly support or weaken which of the scientists' hypotheses?
- AIt supports Scientist 1's hypothesis, because it confirms that noble gases can react with core metals at high pressures and temperatures.
- BIt weakens Scientist 2's hypothesis, because it demonstrates that chemical sequestration in the core is a more thermodynamically favorable process than hydrodynamic escape.
- It weakens Scientist 1's hypothesis, because it suggests that krypton and argon would also have been sequestered in Earth's core, leaving the atmosphere depleted of these gases as well.Answer
- DIt supports Scientist 2's hypothesis, because it provides an alternative mechanism for atmospheric noble gas retention that does not rely on ionization potential.