Un elemento químico es un tipo de materia constituida por átomos de la misma clase. En su forma más simple posee un número determinado de protones en su núcleo, haciéndolo pertenecer a una categoría única clasificada con el número atómico, aún cuando éste pueda desplegar distintas masas atómicas. Es un átomo con características físicas únicas, aquella sustancia que no puede ser descompuesta mediante una reacción química, en otras más simples. Si existen dos átomos de un mismo elemento con características distintas y, en el caso de que estos posean número másico distinto, pertenecen al mismo elemento pero en lo que se conoce como uno de sus isótopos. También es importante diferenciar entre los «elementos químicos» de una sustancia simple. Los elementos se encuentran en la tabla periódica de los elementos. El ozono (O3) y el dioxígeno (O2) son dos sustancias simples, cada una de ellas con propiedades diferentes. Y el elemento químico que forma estas dos sustancias simples es el oxígeno (O). Algunos elementos se han encontrado en la naturaleza y otros obtenidos de manera artificial, formando parte de sustancias simples o de compuestos químicos. Otros han sido creados artificialmente en los aceleradores de partículas o en reactores atómicos. Estos últimos suelen ser inestables y sólo existen durante milésimas de segundo. A lo largo de la historia del universo se han ido generando la variedad de elementos químicos a partir de nucleosíntesis en varios procesos, fundamentalmente debidos a estrellas. Los nombres de los elementos químicos son nombres comunes y como tales deben escribirse sin mayúscula inicial, salvo que otra regla ortográfica lo imponga.

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A chemical element or element is a species of atoms having the same number of protons in their atomic nuclei (i.e. the same atomic number, Z). There are 118 elements that have been identified, of which the first 94 occur naturally on Earth with the remaining 24 being synthetic elements. There are 80 elements that have at least one stable isotope and 38 that have exclusively radioactive isotopes, which decay over time into other elements. Iron is the most abundant element (by mass) making up Earth, while oxygen is the most common element in the crust of Earth. Chemical elements constitute all of the ordinary matter of the universe. However astronomical observations suggest that ordinary observable matter is only approximately 15% of the matter in the universe: the remainder is dark matter, the composition of which is unknown, but it is not composed of chemical elements.The two lightest elements, hydrogen and helium were mostly formed in the Big Bang and are the most common elements in the universe. The next three elements (lithium, beryllium and boron) were formed mostly by cosmic ray spallation, and are thus more rare than those that follow. Formation of elements with from six to twenty six protons occurred and continues to occur in main sequence stars via stellar nucleosynthesis. The high abundance of oxygen, silicon, and iron on Earth reflects their common production in such stars. Elements with greater than twenty-six protons are formed by supernova nucleosynthesis in supernovae, which, when they explode, blast these elements far into space as supernova remnants, where they may become incorporated into planets when they are formed. The term "element" is used for a kind of atoms with a given number of protons (regardless of whether they are or they are not ionized or chemically bonded, e.g. hydrogen in water) as well as for a pure chemical substance consisting of a single element (e.g. hydrogen gas). For the second meaning, the terms "elementary substance" and "simple substance" have been suggested, but they have not gained much acceptance in the English-language chemical literature, whereas in some other languages their equivalent is widely used (e.g. French corps simple, Russian простое вещество). One element can form multiple substances different by their structure; they are called allotropes of the element. When different elements are chemically combined, with the atoms held together by chemical bonds, they form chemical compounds. Only a minority of elements are found uncombined as relatively pure minerals. Among the more common of such "native elements" are copper, silver, gold, carbon (as coal, graphite, or diamonds), and sulfur. All but a few of the most inert elements, such as noble gases and noble metals, are usually found on Earth in chemically combined form, as chemical compounds. While about 32 of the chemical elements occur on Earth in native uncombined forms, most of these occur as mixtures. For example, atmospheric air is primarily a mixture of nitrogen, oxygen, and argon, and native solid elements occur in alloys, such as that of iron and nickel. The history of the discovery and use of the elements began with primitive human societies that found native elements like carbon, sulfur, copper and gold. Later civilizations extracted elemental copper, tin, lead and iron from their ores by smelting, using charcoal. Alchemists and chemists subsequently identified many more, with almost all of the naturally-occurring elements becoming known by 1900. The properties of the chemical elements are summarized on the periodic table, which organizes the elements by increasing atomic number into rows ("periods") in which the columns ("groups") share recurring ("periodic") physical and chemical properties. Save for unstable radioactive elements with short half-lives, all of the elements are available industrially, most of them in high degrees of purity.

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