In the early 1800s, elements were classified by atomic masses, and Mendeleev introduced gaps for undiscovered elements, predicting their properties.
In the early 1800s, elements were classified primarily based on atomic masses, where elements with similar properties were arranged together.
Mendeleev made two significant changes to the early periodic tables: he arranged elements based on atomic masses but left gaps for undiscovered elements, and he predicted properties of these missing elements that matched those of later-discovered elements, solidifying the acceptance of his periodic table.
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