Periodic Table of Elements
Click any element to see its properties
Click any element to see its atomic number, weight, electron configuration, state, and key properties. Color-coded by element category.
Click any element to see its properties
The periodic table organizes all 118 known elements by atomic number. An element's position encodes its properties:
Symbols often look nothing like English names because many come from Latin:
Named after places: Francium (France), Germanium (Germany), Americium, Berkelium (Berkeley, CA). Named after scientists: Curium (Marie and Pierre Curie), Einsteinium, Fermium.
An atom's chemical behavior is almost entirely determined by its valence (outermost) electrons. The octet rule: atoms tend to gain, lose, or share electrons to achieve 8 valence electrons (the stable noble gas configuration). This drives all of chemistry. Sodium (1 valence electron) gives it up; Chlorine (7 valence electrons) desperately wants one more. Na donates to Cl; both reach stable configurations; ionic NaCl (table salt) forms.
Isotopes are variants of the same element with the same protons but different neutrons. Carbon-12 (6p, 6n) and Carbon-14 (6p, 8n) are both carbon with identical chemistry — but very different nuclear stability. Carbon-14 decays at a known rate, enabling radiocarbon dating. Uranium-235 and U-238 are both uranium; U-235 undergoes fission more readily, making it the isotope used in nuclear reactors. The atomic mass on the periodic table is the weighted average of all natural isotopes.
The most recently confirmed elements are synthetic — created in particle accelerators and existing for only fractions of a second:
Scientists are pursuing element 119, which would begin Period 8 of the periodic table.
In 1869, Russian chemist Dmitri Mendeleev published the first widely recognized periodic table, arranged by atomic weight. His crucial insight was leaving gaps for undiscovered elements and predicting their properties based on position. When gallium (1875), scandium (1879), and germanium (1886) were discovered with almost exactly Mendeleev's predicted properties, his table gained widespread acceptance.
The modern table was reorganized by atomic number after Henry Moseley's X-ray experiments in 1913, resolving inconsistencies in Mendeleev's ordering. New elements have been added to its outer edges as heavy synthetic elements are created.