Question: A popular thermodynamic reference state used for many decades involves the composition of the atmosphere, the ocean, and the top few meters of the earth's

A popular thermodynamic reference state used for many decades involves the composition of the atmosphere, the ocean, and the top few meters of the earth's crust. This reference state was devised when the world was empty. Now that the world is full, have the compositions in this reference state changed in any way?

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