A chemical element is a pure chemical substance consisting of one type of atom distinguished by its atomic number, which is the number of protons in its nucleus. Familiar examples of elements include gold, iron, copper, carbon, silicon, mercury, sodium, calcium, hydrogen, nitrogen, chlorine, and neon.
As of May 2011, 118 elements have been identified, the latest being ununoctium in 2002. Of the 118 known elements, only the first 94 are believed to occur naturally on Earth. Of these naturally occurring elements, 80 are stable or essentially so, while the others are radioactive, decaying into other, lighter elements over various timescales from hours to billions of years. Additional elements, of higher atomic numbers than those naturally occurring, have been produced technologically in recent decades as the products of nuclear reactions.
The properties of the chemical elements are often summarized using the periodic table that organizes the elements by increasing atomic number into rows ("periods") in which the columns ("groups") share recurring ("periodic") physical and chemical properties. Its invention is generally credited to Russian chemist Dmitri Mendeleev in 1869.
The universe's naturally occurring chemical elements are thought to have been produced by various cosmic processes, including hydrogen and helium creation during the Big Bang, production of elements as heavy as iron by stellar nucleosynthesis and cosmic-ray spallation, and formation of many heavier elements in supernovae and other cataclysmic cosmic events. While most elements are generally viewed as stable, transformation of one element to another occurs through decay of radioactive elements as well as other nuclear processes such as cosmic ray bombardment and natural nuclear fission of the nuclei of various heavy elements.
When two distinct elements are chemically combined, with the atoms held together by chemical bonds, the result is termed a chemical compound. Chemical compounds may be composed of elements combined in exact whole-number ratios of atoms, as in water, table salt, and such minerals as quartz, calcite, and some metal ores. However, chemical bonding of many types of elements may result in the formation of crystalline solids and metallic alloys for which exact chemical formulas do not exist. Most of the solid substance of the Earth is of this latter type: the atoms that are present in the substance of the Earth's crust, mantle, and inner core are combined into chemical compounds of many compositions, but these do not have precise empirical formulas.
While all of the 94 naturally occurring elements have been identified in mineral samples from the Earth's crust, only a few elements are found occasionally on Earth as recognizable, relative pure minerals. Among the more common of such "native elements" are copper, silver, gold, carbon (as coal, graphite, or diamonds), sulfur, and mercury. Air is primarily a mixture of gaseous elements, with nitrogen, oxygen, and argon being most abundant. Most of the various elements on Earth are present instead in various mixtures, alloys, and chemical compounds in which the physical and chemical properties of the individual elements are not apparent.
Hydrogen and helium are by far the most abundant elements in the universe. However, oxygen is the most abundant element in the Earth's crust, making up almost half of its mass. Although all known chemical matter is composed of these various elements, chemical matter itself constitutes only about 15% of the total matter in the universe. The remainder is dark matter, which is not believed to consist of chemical elements as we know them since it does not contain protons, neutrons or electrons.
The history of discovery of the chemical elements began with the numerous primitive human societies that found such native elements as copper and gold, and extracted (smelted) iron and a few other metallic elements from their ores. Alchemists and chemists subsequently identified and characterized many more, with nearly all of the naturally occurring elements known by 1900.
Many of the elements, alone or in various combined forms, are essential to various kinds of biological life, with carbon, hydrogen, nitrogen, oxygen, phosphorus, potassium, sodium, and sulfur among the most important. Certain kinds of organisms require particular additional elements, for example the magnesium in chlorophyll in green plants, the calcium in mollusc shells, or the iron in the hemoglobin in vertebrate animals' red blood cells. Humans require recurrent consumption of small or trace amounts of dozens of elements, often included in vitamin and mineral supplements.
In human society, almost every element has at least one unique household, commercial, industrial, scientific, or medical use, either in its pure forms or in various chemical compounds, mixtures, alloys, and other substances. Nearly all of the elements through uranium, and also americium, are now available industrially, most to high degrees of purity, except for a few radioactive ones that exist only transiently.
Description
The lightest of the chemical elements are hydrogen and
helium, both created by
Big Bang nucleosynthesis during the
first 20 minutes of the universe in a
ratio of around 3:1 by mass (approximately 12:1 by number of atoms). Almost all other elements found in nature, including some further hydrogen and helium created since then, were made by various natural or (at times) artificial methods of
nucleosynthesis. On Earth, small amounts of new atoms are naturally produced in
nucleogenic reactions, or in
cosmogenic processes, such as
cosmic ray spallation. New atoms are also naturally produced on Earth as
radiogenic daughter isotopes of ongoing
radioactive decay processes such as
alpha decay,
beta decay,
spontaneous fission,
cluster decay, and other rarer modes of decay.
Of the 94 naturally occurring elements, those with atomic numbers 1 through 40 are all considered to be stable isotopes. Elements with atomic numbers 41 through 82 are apparently stable (except technetium and promethium) but theoretically unstable, or radioactive. The half-lives of elements 41 through 82 are so long however that their radioactive decay has yet to be detected by experiment. These "theoretical radionuclides" have half-lives at least 100 million times longer than the estimated age of the universe. Elements with atomic numbers 83 through 94 are unstable to the point that their radioactive decay can be detected. Some of these elements, notably thorium (atomic number 90) and uranium (atomic number 92), have one or more isotopes with half-lives long enough to survive as remnants of the explosive stellar nucleosynthesis that produced the heavy elements before the formation of our solar system. For example, at over 1.9 years, over a billion times longer than the current estimated age of the universe, bismuth-209 (atomic number 83) has the longest known alpha decay half-life of any naturally occurring element. The very heaviest elements (those beyond plutonium, atomic number 94) undergo radioactive decay with half-lives so short that they have only been observed as the result of experimental observation.
As of 2010, there are 118 known elements (in this context, "known" means observed well enough, even from just a few decay products, to have been differentiated from any other element). Of these 118 elements, 94 occur naturally on Earth. Six of these occur in extreme trace quantities: technetium, atomic number 43; promethium, number 61; astatine, number 85; francium, number 87; neptunium, number 93; and plutonium, number 94. These 94 elements, and also possibly element 98 californium, have been detected in the universe at large, in the spectra of stars and also supernovae, where short-lived radioactive elements are newly being made. The first 94 elements have been detected directly on Earth as naturally-occurring fission or transmutation products of uranium and thorium. Some californium may be present on Earth, but at present, natural californium is only known from supernovae spectra and even there its presence is uncertain (see californium for detail).
The remaining 24 heavier elements, not found today either on Earth or in astronomical spectra, have been derived artificially. All of the heavy elements that are derived solely through artificial means are radioactive, with very short half-lives; if any atoms of these elements were present at the formation of Earth, they are extremely likely to have already decayed, and if present in novae, have been in quantities too small to have been noted. Technetium was the first purportedly non-naturally occurring element to be synthesized, in 1937, although trace amounts of technetium have since been found in nature (and also the element may have been discovered naturally in 1925). This pattern of artificial production and later natural discovery has been repeated with several other radioactive, naturally-occurring rare elements.
Lists of the elements are available by name, by symbol, by atomic number, by density, by melting point, and by boiling point as well as Ionization energies of the elements. The nuclides of stable and radioactive elements are also available as a list of nuclides, sorted by length of half-life for those that are unstable. One of the most convenient, and certainly the most traditional presentation of the elements, is in form of periodic table, which groups elements with similar chemical properties (and usually also similar electronic structures) together.
Atomic number
The
atomic number of an element, ''Z'', is equal to the number of protons that defines the element. For example, all carbon atoms contain 6 protons in their
nucleus; so the atomic number "Z" of carbon is 6. Carbon atoms may have different numbers of neutrons; atoms of the same element having different numbers of neutrons are known as
isotopes of the element.
The number of protons in the atomic nucleus also determines its electric charge, which in turn determines the number of electrons of the atom in its non-ionized state. The electrons are placed into atomic orbitals which determine the atom's various chemical properties. The number of neutrons in a nucleus usually has very little effect on an elements' chemical properties (except in the case of hydrogen and deuterium). Thus, all carbon isotopes have nearly identical chemical properties because they all have six protons and six electrons, even though carbon atoms may differ in number of neutrons. It is for this reason that atomic number rather than mass number (or atomic weight) is considered the identifying characteristic of a chemical element.
Atomic mass
The
mass number of an element, ''A'', is the number of
nucleons (protons and neutrons) in the atomic nucleus. Different isotopes of a given element are distinguished by their mass numbers, which are conventionally written as a super-index on the left hand side of the atomic symbol (e.g.,
238U).
The relative atomic mass of an element is the average of the atomic masses of all the chemical element's isotopes as found in a particular environment, weighted by isotopic abundance, relative to the atomic mass unit (u). This number may be a fraction that is not close to a whole number, due to the averaging process. On the other hand, the atomic mass of a pure isotope is quite close to its mass number. Whereas the mass number is a natural (or whole) number, the atomic mass of a single isotope is a real number that is close to a natural number. In general, it differs slightly from the mass number as the mass of the protons and neutrons is not exactly 1 u, the electrons also contribute slightly to the atomic mass, and because of the nuclear binding energy. For example, the mass of 19F is 18.9984032 u. The only exception to the atomic mass of an isotope not being a natural number is 12C, which has a mass of exactly 12, because u is ''defined'' as 1/12 of the mass of a free neutral carbon-12 atom in the ground state.
Isotopes
Isotopes are atoms of the same element (that is, with the same number of protons in their atomic nucleus), but having ''different'' numbers of
neutrons. Most (66 of 94) naturally occurring elements have more than one stable isotope. Thus, for example, there are three main isotopes of carbon. All carbon atoms have 6 protons in the nucleus, but they can have either 6, 7, or 8 neutrons. Since the mass numbers of these are 12, 13 and 14 respectively, the three isotopes of carbon are known as carbon-12, carbon-13, and carbon-14, often abbreviated to
12C,
13C, and
14C. Carbon in everyday life and in
chemistry is a mixture of
12C,
13C, and
14C atoms.
Except in the case of the isotopes of hydrogen (which differ greatly from each other in relative mass—enough to cause chemical effects), the isotopes of the various elements are typically chemically nearly indistinguishable from each other. For example, the three naturally occurring isotopes of carbon have essentially the same chemical properties, but different nuclear properties. In this example, carbon-12 and carbon-13 are stable atoms, but carbon-14 is unstable; it is radioactive, undergoing beta decay into nitrogen-14.
As illustrated by carbon, all of the elements have some isotopes that are radioactive (radioisotopes), which decay into other elements upon radiating an alpha or beta particle. Certain elements ''only'' have radioactive isotopes: specifically the elements without any stable isotopes are technetium (atomic number 43), promethium (atomic number 61), and all observed elements with atomic numbers greater than 82.
Of the 80 elements with at least one stable isotope, 26 have only one stable isotope, and the mean number of stable isotopes for the 80 stable elements is 3.1 stable isotopes per element. The largest number of stable isotopes that occur for an element is 10 (for tin, element 50).
Allotropes
Atoms of pure elements may bond to each other chemically in more than one way, allowing the pure element to exist in multiple structures (spacial arrangements of atoms), known as
allotropes, which differ in their properties. For example, carbon can be found as
diamond, which has a tetrahedral structure around each carbon atom;
graphite, which has layers of carbon atoms with a hexagonal structure stacked on top of each other;
graphene, which is a single layer of graphite that is incredibly strong;
fullerenes, which have nearly spherical shapes; and
carbon nanotubes, which are tubes with a hexagonal structure (even these may differ from each other in electrical properties). The ability for an element to exist in one of many structural forms is known as 'allotropy'.
The standard state, or reference state, of an element is defined as its thermodynamically most stable state at 1 bar at a given temperature (typically at 298.15 K). In thermochemistry, an element is defined to have an enthalpy of formation of zero in its standard state. For example, the reference state for carbon is graphite, because it is more stable than the other allotropes.
Properties
Several kinds of descriptive categorizations can be applied broadly to the elements, including consideration of their general physical and chemical properties, their states of matter under familiar conditions, their melting and boiling points, their densities, their crystal structures as solids, and their origins.
General properties
Several terms are commonly used to characterize the general physical and chemical properties of the chemical elements. A first distinction is between the
metals, which readily conduct
electricity, and the
nonmetals, which do not, with a small group (the ''
metalloids'') having intermediate properties, often behaving as
semiconductors.
A more refined classification is often shown in colored presentations of the periodic table; this system restricts the terms "metal" and "nonmetal" to only certain of the more broadly defined metals and nonmetals, adding additional terms for certain sets of the more broadly viewed metals and nonmetals. The version of this classification used in the periodic tables presented here includes: actinides, alkali metals, alkaline earth metals, halogens, lanthanides, metals (or "other metals"), metalloids, noble gases, nonmetals (or "other nonmetals"), and transition metals. In this system, the alkali metals, alkaline earth metals, and transition metals, as well as the lanthanides and the actinides, are special groups of the metals viewed in a broader sense. Similarly, the halogens and the noble gases are nonmetals, viewed in the broader sense. In some presentations, the halogens are not distinguished, with astatine identified as a metalloid and the others identified as nonmetals.
States of matter
Another commonly used basic distinction among the elements is their
state of matter (phase),
solid, liquid, or
gas, at a selected standard temperature and pressure (
STP). Most of the elements are solids at conventional temperatures and atmospheric pressure, while several are gases. Only
bromine and
mercury are liquids at 0 degrees Celsius (32 degrees Fahrenheit) and normal atmospheric pressure;
caesium and
gallium are solids at that temperature, but melt at 28.4 °C (83.2 °F) and 29.8 °C (85.6 °F), respectively.
Melting and boiling points
Melting and
boiling points, typically expressed in degrees Celsius at a pressure of one atmosphere, are commonly used in characterizing the various elements. While known for most elements, either or both of these measurements is still undetermined for some of the radioactive elements available in only tiny quantities. Since
helium remains a liquid even at
absolute zero at atmospheric pressure, it has only a boiling point, and not a melting point, in conventional presentations.
Densities
The
density at a selected standard temperature and pressure (
STP) is frequently used in characterizing the elements. Density is often expressed in
grams per cubic centimeter (g/cm
3). Since several elements are gases at commonly encountered temperatures, their densities are usually stated for their gaseous forms; when liquefied or solidified, the gaseous elements have densities similar to those of the other elements.
When an element has allotropes with different densities, one representative allotrope is typically selected in summary presentations, while densities for each allotrope can be stated where more detail is provided. For example, the three familiar allotropes of carbon (amorphous carbon, graphite, and diamond) have densities of 1.8–2.1, 2.267, and 3.515 g/cm3 respectively.
Crystal structures
The elements studied to date as solid samples have eight kinds of
crystal structures:
cubic, body-centered cubic, face-centered cubic, hexagonal, monoclinic, orthorhombic, rhombohedral, and
tetragonal. For some of the synthetically produced transuranic elements, available samples have been too small to determine crystal structures.
Origins
The elements may also be categorized by their origins, with the first 94 considered
naturally occurring, and those with atomic numbers beyond 94 being
synthetic (produced technologically, but not known to occur naturally). Of the naturally occurring elements, 84 are considered
primordial, either stable or long-persisting, and the remaining 10
transient, produced either recurrently or incidentally as
decay products or through other
nuclear processes, but not themselves long-persisting. The 91
regularly occurring natural elements include the 80 stable or essentially stable, primordial elements (from
hydrogen through
lead, omitting
technetium and
promethium);
bismuth,
thorium,
uranium, and
plutonium (radioactive but still remaining from primordial times); and the 7 transiently existing but recurrently produced decay products of thorium, uranium, and plutonium (
polonium,
astatine,
radon,
francium,
radium,
actinium, and
protactinium). Three additional naturally occurring elements, technetium, promethium, and
neptunium, are only
incidentally occurring, present in natural materials only as transiently existing atoms produced from uranium or other heavy elements by rare nuclear processes. Note that
helium is recurrently produced naturally from radioactive decay, but little if any primordial helium still exists at the Earth's surface, since this light gas readily escapes from the atmosphere into outer space.
The periodic table
The properties of the chemical elements are often summarized using the periodic table, which powerfully and elegantly organizes the elements by increasing atomic number into rows ("periods") in which the columns ("groups") share recurring ("periodic") physical and chemical properties. The current standard table contains 118 confirmed elements as of April 10, 2010.
Although earlier precursors to this presentation exist, its invention is generally credited to Russian chemist Dmitri Mendeleev in 1869, who intended the table to illustrate recurring trends in the properties of the elements. The layout of the table has been refined and extended over time, as new elements have been discovered, and new theoretical models have been developed to explain chemical behavior.
Use of the periodic table is now ubiquitous within the academic discipline of chemistry, providing an extremely useful framework to classify, systematize and compare all the many different forms of chemical behavior. The table has also found wide application in physics, geology, biology, materials science, engineering, agriculture, medicine, nutrition, environmental health, and astronomy. Its principles are especially important in chemical engineering.
Nomenclature and symbols
The various chemical elements are formally identified by their unique atomic numbers, by their accepted names, and by their symbols.
Atomic numbers
The known elements have atomic numbers from 1 through 118, conventionally presented as
Arabic numerals.
Since the elements can be uniquely sequenced by atomic number, conventionally from lowest to hightest (as in a periodic table), sets of elements are sometimes specified by such notation as "through", "beyond", or "from ... through", as in "through iron", "beyond uranium", or "from lanthanum through lutetium". The terms "light" and "heavy" are sometimes also used informally to indicate relative atomic numbers (not densities!), as in "lighter than carbon" or "heavier than lead", although technically the weight or mass of atoms of an element (their atomic weights or atomic masses) do not always increase monotonically with their atomic numbers.
Element names
The naming of various substances now known as elements precedes the atomic theory of matter, as names were given locally by various cultures to various minerals, metals, compounds, alloys, mixtures, and other materials, although at the time it was not known which chemicals were elements and which compounds. As they were identified as elements, the existing names for anciently-known elements (''e.g.,'' gold, mercury, iron) were kept in most countries. National differences emerged over the names of elements either for convenience, linguistic niceties, or nationalism. For a few illustrative examples: German speakers use "Wasserstoff" (water substance) for "hydrogen", "Sauerstoff" (acid substance) for "oxygen" and "Stickstoff" (smothering substance) for "nitrogen", while English and some
romance languages use "sodium" for "natrium" and "potassium" for "kalium", and the French, Italians, Greeks, Portuguese and Poles prefer "azote/azot/azoto" (from roots meaning "no life") for "nitrogen".
For purposes of international communication and trade, the official names of the chemical elements both ancient and more recently recognized are decided by the International Union of Pure and Applied Chemistry (IUPAC), which has decided on a sort of international English language, drawing on traditional English names even when an element's chemical symbol is based on a Latin or other traditional word, for example adopting "gold" rather than "aurum" as the name for the 79th element (Au). IUPAC prefers the British spellings "aluminium" and "caesium" over the U.S. spellings "aluminum" and "cesium", and the U.S. "sulfur" over the British "sulphur". However, elements that are practical to sell in bulk in many countries often still have locally used national names, and countries whose national language does not use the Latin alphabet are likely to use the IUPAC element names.
According to IUPAC, chemical elements are not proper nouns in English; consequently, the full name of an element is not routinely capitalized in English, even if derived from a proper noun, as in californium and einsteinium. Isotope names of chemical elements are also uncapitalized if written out, ''e.g.,'' carbon-12 or uranium-235.
In the second half of the twentieth century, physics laboratories became able to produce nuclei of chemical elements with half-lives too short for an appreciable amount of them to exist at any time. These are also named by IUPAC, which generally adopts the name chosen by the discoverer. This practice can lead to the controversial question of which research group actually discovered an element, a question that has delayed naming of elements with atomic number of 104 and higher for a considerable time. (See element naming controversy).
Precursors of such controversies involved the nationalistic namings of elements in the late 19th century. For example, ''lutetium'' was named in reference to Paris, France. The Germans were reluctant to relinquish naming rights to the French, often calling it ''cassiopeium''. Similarly, the British discoverer of ''niobium'' originally named it ''columbium,'' in reference to the New World. It was used extensively as such by American publications prior to international standardization.
Chemical symbols
Specific chemical elements
Before chemistry became a
science,
alchemists had designed arcane symbols for both metals and common compounds. These were however used as abbreviations in diagrams or procedures; there was no concept of atoms combining to form molecules. With his advances in the atomic theory of matter,
John Dalton devised his own simpler symbols, based on circles, which were to be used to depict molecules.
The current system of chemical notation was invented by Berzelius. In this typographical system chemical symbols are not used as mere abbreviations – though each consists of letters of the Latin alphabet – they are symbols intended to be used by peoples of all languages and alphabets. The first of these symbols were intended to be fully universal; since Latin was the common language of science at that time, they were abbreviations based on the Latin names of metals – Cu comes from Cuprum, Fe comes from Ferrum, Ag from Argentum. The symbols were not followed by a period (full stop) as abbreviations were. Later chemical elements were also assigned unique chemical symbols, based on the name of the element, but not necessarily in English. For example, sodium has the chemical symbol 'Na' after the Latin ''natrium''. The same applies to "W" (wolfram) for tungsten, "Fe" (ferrum) for Iron, "Hg" (hydrargyrum) for mercury, "Sn" (stannum) for tin, "K" (kalium) for potassium, "Au" (aurum) for gold, "Ag" (argentum) for silver, "Pb" (plumbum) for lead, "Cu" (Cuprum) for Copper, and "Sb" (stibium) for antimony.
Chemical symbols are understood internationally when element names might need to be translated. There are sometimes differences; for example, the Germans have used "J" instead of "I" for iodine, so the character would not be confused with a roman numeral.
The first letter of a chemical symbol is always capitalized, as in the preceding examples, and the subsequent letters, if any, are always lower case (small letters). Thus, the symbols for californium or einsteinium are Cf and Es.
General chemical symbols
There are also symbols for series of chemical elements, for comparative formulas. These are one capital letter in length, and the letters are reserved so they are not permitted to be given for the names of specific elements. For example, an "
X" is used to indicate a variable group amongst a class of compounds (though usually a
halogen), while "
R" is used for a
radical, meaning a compound structure such as a hydrocarbon chain. The letter "
Q" is reserved for "heat" in a chemical reaction. "
Y" is also often used as a general chemical symbol, although it is also the symbol of
yttrium. "
Z" is also frequently used as a general variable group. "
L" is used to represent a general
ligand in inorganic and organometallic chemistry. "
M" is also often used in place of a general metal.
At least one additional, two-letter generic chemical symbol is also in informal usage, "Ln" for any lanthanide element.
Isotope symbols
Isotopes are distinguished by the atomic mass number (total protons and neutrons) for a particular isotope of an element, with this number combined with the pertinent element's symbol. IUPAC prefers that isotope symbols be written in superscript notation when practical, for example
12C and
235U. However, other notations, such as carbon-12 and uranium-235, or C-12 and U-235, are also used.
As a special case, the three naturally occurring isotopes of the element hydrogen are often specified as H for 1H (protium), D for 2H (deuterium), and T for 3H (tritium). This convention is easier to use in chemical equations, replacing the need to write out the mass number for each atom. For example, the formula for heavy water may be written D2O instead of 2H2O.
Origin of the elements
Only about 4% of the total mass of the
universe is made of
atoms or
ions, and thus represented by chemical elements. This fraction is about 15% of the total matter, with the remainder of the matter (85%) being
dark matter. The nature of dark matter is unknown, but it is not composed of atoms of chemical elements because it contains no protons, neutrons, or electrons. (The remaining non-matter part of the mass of the universe is composed of the even more mysterious
dark energy).
The universe's 94 naturally occurring chemical elements are thought to have been produced by at least four cosmic processes. Most of the hydrogen and helium in the universe was produced primordially in the first few minutes of the Big Bang. Three recurrently occurring later processes are thought to have produced the remaining elements. Stellar nucleosynthesis, an ongoing process, produces all elements from carbon through iron in atomic number, but little lithium, beryllium, or boron. Elements heavier in atomic number than iron, as heavy as uranium and plutonium, are produced by explosive nucleosynthesis in supernovas and other cataclysmic cosmic events. Cosmic ray spallation (fragmentation) of carbon, nitrogen, and oxygen is important to the production of lithium, beryllium and boron.
During the early phases of the Big Bang, nucleosynthesis of hydrogen nuclei resulted in the production of hydrogen-1 (protonium, 1H) and helium-4 (4He), as well as a smaller amount of deuterium (2H) and very minuscule amounts (on the order of 10−10) of lithium and beryllium. Even smaller amounts of boron may have been produced in the Big Bang, since it has been observed in some very old stars, while carbon has not. It is generally agreed that no heavier elements than boron were produced in the Big Bang. As a result, the primordial abundance of atoms (or ions) consisted of roughly 75% 1H, 25% 4He, and 0.01% deuterium, with only tiny traces of lithium, beryllium, and perhaps boron. Subsequent enrichment of galactic halos occurred due to stellar nucleosynthesis and supernova nucleosynthesis. However, the element abundance in intergalactic space can still closely resemble primordial conditions, unless it has been enriched by some means.
On Earth (and elsewhere), trace amounts of various elements continue to be produced from other elements as products of natural transmutation processes. These include some produced by cosmic rays or other nuclear reactions (see cosmogenic and nucleogenic nuclides), and others produced as decay products of long-lived primordial nuclides. For example, trace (but detectable) amounts of carbon-14 (14C) are continually produced in the atmosphere by cosmic rays impacting nitrogen atoms, and argon-40 (40Ar) is continually produced by the decay of primordially occurring but unstable potassium-40 (40K). Also, three primordially occurring but radioactive actinides, thorium, uranium, and plutonium, decay through a series of recurrently produced but unstable radioactive elements such as radium and radon, which are transiently present in any sample of these metals or their ores or compounds. Three other radioactive elements, technetium, promethium, and neptunium, occur only incidentally in natural materials, produced as individual atoms by natural fission of the nuclei of various heavy elements or in other rare nuclear processses.
Human technology has produced various additional elements beyond these first 94, with those through atomic number 118 now known.
Abundance
The following graph (note log scale) shows abundance of elements in our solar system. The table shows the twelve most common elements in our galaxy (estimated spectroscopically), as measured in parts per million, by mass. Nearby galaxies that have evolved along similar lines have a corresponding enrichment of elements heavier than hydrogen and helium. The more distant galaxies are being viewed as they appeared in the past, so their abundances of elements appear closer to the primordial mixture. As physical laws and processes appear common throughout the visible universe, however, it is expected that these galaxies will likewise have evolved similar abundances of elements.
{|class="wikitable"
|-
!Element!!Parts per millionby mass
|-
|Hydrogen
|739,000
|-
|Helium
|240,000
|-
|Oxygen
|10,400
|-
|Carbon
|4,600
|-
|Neon
|1,340
|-
|Iron
|1,090
|-
|Nitrogen
|960
|-
|Silicon
|650
|-
|Magnesium
|580
|-
|Sulfur
|440
|-
|Potassium
|210
|-
|Nickel
|100
|}
History
Evolving definitions
The concept of an "element" as an undivisible substance has developed through three major historical phases: Classical definitions (such as those of the ancient Greeks), chemical definitions, and atomic definitions.
Classical definitions
Ancient philosophy posited a set of
classical elements to explain observed patterns in
nature. These ''elements'' originally referred to ''
earth'', ''
water'', ''
air'' and ''
fire'' rather than the chemical elements of modern science.
The term 'elements' (''stoicheia'') was first used by the Greek philosopher Plato in about 360 BCE, in his dialogue Timaeus, which includes a discussion of the composition of inorganic and organic bodies and is a speculative treatise on chemistry. Plato believed the elements introduced a century earlier by Empedocles were composed of small polyhedral ''forms'': tetrahedron (fire), octahedron (air), icosahedron (water), and cube (earth).
Aristotle, c. 350 BCE, also used the term ''stoicheia'' and added a fifth element called ''aether,'' which formed the heavens. Aristotle defined an element as:
Chemical definitions
In 1661,
chemist Robert Boyle showed that there were more than just the four
classical elements that the ancients had assumed. The first modern list of chemical elements was given in
Antoine Lavoisier's 1789 ''Elements of Chemistry'', which contained thirty-three elements, including
light and caloric. By 1818,
Jöns Jakob Berzelius had determined atomic weights for forty-five of the forty-nine then-accepted accepted elements.
Dmitri Mendeleev had sixty-six elements in his
periodic table of 1869.
From Boyle until the early 20th century, an element was defined as a pure substance that could not be decomposed into any simpler substance. Put another way, a chemical element cannot be transformed into other chemical elements by chemical processes. Elements during this time were generally distinguished by their atomic weights, a property measurable with fair accuracy by available analytical techniques.
Atomic definitions
The 1913 discovery by
Henry Moseley that the nuclear charge is the physical basis for an atom's atomic number, further refined when the nature of
protons and
neutrons became appreciated, eventually led to the current definition of an element, based on atomic number (number of protons per atomic nucleus). The use of atomic numbers, rather than atomic weights, to distinguish elements has greater predictive value (since these numbers are integers), and also resolves some ambiguities in the chemistry-based view due to varying properties of
isotopes and
allotropes within the same element. Currently
IUPAC defines an element to exist if it has isotopes with a lifetime longer than the 10
−14 seconds which takes the nucleus to form an electronic cloud.
By 1914, seventy-two elements were known, all naturally occurring. The remaining naturally occurring elements were discovered or isolated is subsequent decades, and various additional elements have also been produced synthetically, with much of that work pioneered by Glenn T. Seaborg. In 1955, element 101 was discovered and named mendelevium in honor of D.I. Mendeleev, the first to arrange the elements in a periodic manner. Most recently, the synthesis of element 118 was reported in October 2006, and the synthesis of element 117 was reported in April 2010.
Discovery and recognition of various elements
Ten materials familiar to various prehistoric cultures are now known to be chemical elements: Carbon, copper, gold, iron, lead, mercury, silver, sulfur, tin, and zinc. Three additional materials now accepted as elements, arsenic, antimony, and bismuth, were recognized as distinct substances prior to 1500 AD. Phosphorus, cobalt, and platinum were isolated before 1750.
Most of the remaining naturally occurring chemical elements were identified and characterized by 1900, including:
Such now-familiar industrial materials as aluminum, silicon, nickel, chromium, magnesium, and tungsten
Reactive metals such as lithium, sodium, potassium, and calcium
The halogens fluorine, chlorine, bromine, and iodine
Gases such as hydrogen, oxygen, nitrogen, helium, argon, and neon
Most of the rare-earth elements, including cerium, lanthanum, gadolinium, and neodymium, and
The more common radioactive elements, including uranium, thorium, radium, and radon
Elements isolated or produced since 1900 include:
The three remaining undiscovered regularly occurring stable natural elements: hafnium, lutetium, and rhenium
Plutonium, first produced synthetically but now also known from a few long-persisting natural occurrences
The three incidentally occurring natural elements (neptunium, promethium, and technetium), all first produced synthetically but later discovered in trace amounts in certain geological samples
Three scarcer decay products of uranium or thorium (astatine, francium, and protactinium),
Various synthetic transuranic elements, beginning with americium, curium, berkelium, and californium
Recently discovered elements
The first
transuranium element (element with
atomic number greater than 92) discovered was
neptunium in 1940. As of February 2010, only the elements up to 112,
copernicium, have been confirmed as discovered by
IUPAC, while claims have been made for synthesis of elements
113,
114,
115,
116,
117 and
118. The discovery of element 112 was acknowledged in 2009, and the name 'copernicium' and the atomic symbol 'Cn' were suggested for it. The name and symbol were officially endorsed by IUPAC on February 19, 2010. The heaviest element that is believed to have been synthesized to date is element 118,
ununoctium, on October 9, 2006, by the
Flerov Laboratory of Nuclear Reactions in
Dubna, Russia. Element 117 was the latest element claimed to be discovered, in 2009.
IUPAC officially recognized ununquadium and ununhexium, elements 114 and 116, in June 2011.
List of the 118 known chemical elements
The following sortable table includes the 118 known chemical elements, with the names linking to the ''Wikipedia'' articles on each.
Atomic number, name, and symbol all serve independently as unique identifiers.
Names are those accepted by IUPAC; provisional names for recently produced elements not yet formally named are in parentheses.
Group, period, and block refer to an element's position in the periodic table.
State of matter ''(solid, liquid,'' or ''gas)'' applies at standard
temperature and
pressure conditions (
STP).
Occurrence distinguishes naturally occurring elements, categorized as either ''primordial'' or ''transient'' (from decay), and additional ''synthetic'' elements that have been produced technologically, but are not known to occur naturally.
Description summarizes an element's properties using the broad categories commonly presented in periodic tables: ''Actinide, alkali metal, alkaline earth metal, halogen, lanthanide, metal, metalloid, noble gas, non-metal,'' and ''transition metal.''
+ List of elements
|
Atomic number>Atomic no.
|
! Name
|
Chemical symbol>Symbol
|
Group (periodic table)>Group
|
Period (periodic table)>Period
|
Periodic table block>Block
|
! State of matter |
! Occurrence
|
! Description
|
1
|
[[Hydrogen
|
H
|
1
|
1
|
s
|
Gas
|
Primordial
|
Non-metal
|
2
|
Helium
|
He
|
18
|
1
|
s
|
Gas
|
Primordial
|
Noble gas
|
3
|
Lithium
|
Li
|
1
|
2
|
s
|
Solid
|
Primordial
|
Alkali metal
|
4
|
Beryllium
|
Be
|
2
|
2
|
s
|
Solid
|
Primordial
|
Alkaline earth metal
|
5
|
Boron
|
B
|
13
|
2
|
p
|
Solid
|
Primordial
|
Metalloid
|
6
|
Carbon
|
C
|
14
|
2
|
p
|
Solid
|
Primordial
|
Non-metal
|
7
|
Nitrogen
|
N
|
15
|
2
|
p
|
Gas
|
Primordial
|
Non-metal
|
8
|
Oxygen
|
O
|
16
|
2
|
p
|
Gas
|
Primordial
|
Non-metal
|
9
|
Fluorine
|
F
|
17
|
2
|
p
|
Gas
|
Primordial
|
Halogen
|
10
|
Neon
|
Ne
|
18
|
2
|
p
|
Gas
|
Primordial
|
Noble gas
|
11
|
Sodium
|
Na
|
1
|
3
|
s
|
Solid
|
Primordial
|
Alkali metal
|
12
|
Magnesium
|
Mg
|
2
|
3
|
s
|
Solid
|
Primordial
|
Alkaline earth metal
|
13
|
Aluminium
|
Al
|
13
|
3
|
p
|
Solid
|
Primordial
|
Metal
|
14
|
Silicon
|
Si
|
14
|
3
|
p
|
Solid
|
Primordial
|
Metalloid
|
15
|
Phosphorus
|
P
|
15
|
3
|
p
|
Solid
|
Primordial
|
Non-metal
|
16
|
Sulfur
|
S
|
16
|
3
|
p
|
Solid
|
Primordial
|
Non-metal
|
17
|
Chlorine
|
Cl
|
17
|
3
|
p
|
Gas
|
Primordial
|
Halogen
|
18
|
Argon
|
Ar
|
18
|
3
|
p
|
Gas
|
Primordial
|
Noble gas
|
19
|
Potassium
|
K
|
1
|
4
|
s
|
Solid
|
Primordial
|
Alkali metal
|
20
|
Calcium
|
Ca
|
2
|
4
|
s
|
Solid
|
Primordial
|
Alkaline earth metal
|
21
|
Scandium
|
Sc
|
3
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
22
|
Titanium
|
Ti
|
4
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
23
|
Vanadium
|
V
|
5
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
24
|
Chromium
|
Cr
|
6
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
25
|
Manganese
|
Mn
|
7
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
26
|
Iron
|
Fe
|
8
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
27
|
Cobalt
|
Co
|
9
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
28
|
Nickel
|
Ni
|
10
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
29
|
Copper
|
Cu
|
11
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
30
|
Zinc
|
Zn
|
12
|
4
|
d
|
Solid
|
Primordial
|
Transition metal
|
31
|
Gallium
|
Ga
|
13
|
4
|
p
|
Solid
|
Primordial
|
Metal
|
32
|
Germanium
|
Ge
|
14
|
4
|
p
|
Solid
|
Primordial
|
Metalloid
|
33
|
Arsenic
|
As
|
15
|
4
|
p
|
Solid
|
Primordial
|
Metalloid
|
34
|
Selenium
|
Se
|
16
|
4
|
p
|
Solid
|
Primordial
|
Non-metal
|
35
|
Bromine
|
Br
|
17
|
4
|
p
|
Liquid
|
Primordial
|
Halogen
|
36
|
Krypton
|
Kr
|
18
|
4
|
p
|
Gas
|
Primordial
|
Noble gas
|
37
|
Rubidium
|
Rb
|
1
|
5
|
s
|
Solid
|
Primordial
|
Alkali metal
|
38
|
Strontium
|
Sr
|
2
|
5
|
s
|
Solid
|
Primordial
|
Alkaline earth metal
|
39
|
Yttrium
|
Y
|
3
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
40
|
Zirconium
|
Zr
|
4
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
41
|
Niobium
|
Nb
|
5
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
42
|
Molybdenum
|
Mo
|
6
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
43
|
Technetium
|
Tc
|
7
|
5
|
d
|
Solid
|
Transient
|
Transition metal
|
44
|
Ruthenium
|
Ru
|
8
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
45
|
Rhodium
|
Rh
|
9
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
46
|
Palladium
|
Pd
|
10
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
47
|
Silver
|
Ag
|
11
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
48
|
Cadmium
|
Cd
|
12
|
5
|
d
|
Solid
|
Primordial
|
Transition metal
|
49
|
Indium
|
In
|
13
|
5
|
p
|
Solid
|
Primordial
|
Metal
|
50
|
Tin
|
Sn
|
14
|
5
|
p
|
Solid
|
Primordial
|
Metal
|
51
|
Antimony
|
Sb
|
15
|
5
|
p
|
Solid
|
Primordial
|
Metalloid
|
52
|
Tellurium
|
Te
|
16
|
5
|
p
|
Solid
|
Primordial
|
Metalloid
|
53
|
Iodine
|
I
|
17
|
5
|
p
|
Solid
|
Primordial
|
Halogen
|
54
|
Xenon
|
Xe
|
18
|
5
|
p
|
Gas
|
Primordial
|
Noble gas
|
55
|
Caesium
|
Cs
|
1
|
6
|
s
|
Solid
|
Primordial
|
Alkali metal
|
56
|
Barium
|
Ba
|
2
|
6
|
s
|
Solid
|
Primordial
|
Alkaline earth metal
|
57
|
Lanthanum
|
La
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
58
|
Cerium
|
Ce
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
59
|
Praseodymium
|
Pr
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
60
|
Neodymium
|
Nd
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
61
|
Promethium
|
Pm
|
3
|
6
|
f
|
Solid
|
Transient
|
Lanthanide
|
62
|
Samarium
|
Sm
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
63
|
Europium
|
Eu
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
64
|
Gadolinium
|
Gd
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
65
|
Terbium
|
Tb
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
66
|
Dysprosium
|
Dy
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
67
|
Holmium
|
Ho
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
68
|
Erbium
|
Er
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
69
|
Thulium
|
Tm
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
70
|
Ytterbium
|
Yb
|
3
|
6
|
f
|
Solid
|
Primordial
|
Lanthanide
|
71
|
Lutetium
|
Lu
|
3
|
6
|
d
|
Solid
|
Primordial
|
Lanthanide
|
72
|
Hafnium
|
Hf
|
4
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
73
|
Tantalum
|
Ta
|
5
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
74
|
Tungsten
|
W
|
6
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
75
|
Rhenium
|
Re
|
7
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
76
|
Osmium
|
Os
|
8
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
77
|
Iridium
|
Ir
|
9
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
78
|
Platinum
|
Pt
|
10
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
79
|
Gold
|
Au
|
11
|
6
|
d
|
Solid
|
Primordial
|
Transition metal
|
80
|
|
Hg
|
12
|
6
|
d
|
Liquid
|
Primordial
|
Transition metal
|
81
|
Thallium
|
Tl
|
13
|
6
|
p
|
Solid
|
Primordial
|
Metal
|
82
|
Lead
|
Pb
|
14
|
6
|
p
|
Solid
|
Primordial
|
Metal
|
83
|
Bismuth
|
Bi
|
15
|
6
|
p
|
Solid
|
Primordial
|
Metal
|
84
|
Polonium
|
Po
|
16
|
6
|
p
|
Solid
|
Transient
|
Metalloid
|
85
|
Astatine
|
At
|
17
|
6
|
p
|
Solid
|
Transient
|
Halogen
|
86
|
Radon
|
Rn
|
18
|
6
|
p
|
Gas
|
Transient
|
Noble gas
|
87
|
Francium
|
Fr
|
1
|
7
|
s
|
Solid
|
Transient
|
Alkali metal
|
88
|
Radium
|
Ra
|
2
|
7
|
s
|
Solid
|
Transient
|
Alkaline earth metal
|
89
|
Actinium
|
Ac
|
3
|
7
|
f
|
Solid
|
Transient
|
Actinide
|
90
|
Thorium
|
Th
|
3
|
7
|
f
|
Solid
|
Primordial
|
Actinide
|
91
|
Protactinium
|
Pa
|
3
|
7
|
f
|
Solid
|
Transient
|
Actinide
|
92
|
Uranium
|
U
|
3
|
7
|
f
|
Solid
|
Primordial
|
Actinide
|
93
|
Neptunium
|
Np
|
3
|
7
|
f
|
Solid
|
Transient
|
Actinide
|
94
|
Plutonium
|
Pu
|
3
|
7
|
f
|
Solid
|
Primordial
|
Actinide
|
95
|
Americium
|
Am
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
96
|
Curium
|
Cm
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
97
|
Berkelium
|
Bk
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
98
|
Californium
|
Cf
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
99
|
Einsteinium
|
Es
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
100
|
Fermium
|
Fm
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
101
|
Mendelevium
|
Md
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
102
|
Nobelium
|
No
|
3
|
7
|
f
|
Solid
|
Synthetic
|
Actinide
|
103
|
Lawrencium
|
Lr
|
3
|
7
|
d
|
Solid
|
Synthetic
|
Actinide
|
104
|
Rutherfordium
|
Rf
|
4
|
7
|
d
|
|
Synthetic
|
Transition metal
|
105
|
Dubnium
|
Db
|
5
|
7
|
d
|
|
Synthetic
|
Transition metal
|
106
|
Seaborgium
|
Sg
|
6
|
7
|
d
|
|
Synthetic
|
Transition metal
|
107
|
Bohrium
|
Bh
|
7
|
7
|
d
|
|
Synthetic
|
Transition metal
|
108
|
Hassium
|
Hs
|
8
|
7
|
d
|
|
Synthetic
|
Transition metal
|
109
|
Meitnerium
|
Mt
|
9
|
7
|
d
|
|
Synthetic
|
|
110
|
Darmstadtium
|
Ds
|
10
|
7
|
d
|
|
Synthetic
|
|
111
|
Roentgenium
|
Rg
|
11
|
7
|
d
|
|
Synthetic
|
|
112
|
Copernicium
|
Cn
|
12
|
7
|
d
|
|
Synthetic
|
Transition metal
|
113
|
(Ununtrium)
|
Uut
|
13
|
7
|
p
|
|
Synthetic
|
|
114
|
(Ununquadium)
|
Uuq
|
14
|
7
|
p
|
|
Synthetic
|
|
115
|
(Ununpentium)
|
Uup
|
15
|
7
|
p
|
|
Synthetic
|
|
116
|
(Ununhexium)
|
Uuh
|
16
|
7
|
p
|
|
Synthetic
|
|
117
|
(Ununseptium)
|
Uus
|
17
|
7
|
p
|
|
Synthetic
|
|
118
|
(Ununoctium)
|
Uuo
|
18
|
7
|
p
|
|
Synthetic
|
|
See also
Compound
Chemistry
Discovery of the chemical elements
Element collecting
Fictional element
Goldschmidt classification
Island of stability
List of elements by name
Systematic element name
Prices of elements and their compounds
Periodic Systems of Small Molecules
Table of nuclides
List of nuclides
References
Further reading
External links
Videos for each element by the University of Nottingham
Category:Chemistry
af:Chemiese element
als:Chemisches Element
ar:عنصر كيميائي
an:Elemento quimico
ast:Elementu químicu
az:Kimyəvi element
bn:মৌলিক পদার্থ
zh-min-nan:Hoà-ha̍k goân-sò͘
ba:Химик элемент
be:Хімічны элемент
be-x-old:Хімічны элемэнт
bs:Hemijski element
br:Elfenn gimiek
bg:Химичен елемент
ca:Element químic
cv:Хими элеменчĕсем
cs:Chemický prvek
cy:Elfen gemegol
da:Grundstof
de:Chemisches Element
et:Keemiline element
el:Χημικό στοιχείο
es:Elemento químico
eo:Kemia elemento
eu:Elementu kimiko
fa:عنصر (شیمی)
hif:Rasaenik element
fo:Frumevni
fr:Élément chimique
fy:Elemint
fur:Element chimic
ga:Dúil cheimiceach
gv:Bunstoo
gl:Elemento químico
hak:Ngièn-su
ko:화학 원소
haw:Kumumea kemikala
hi:रासायनिक तत्व
hr:Kemijski element
io:Kemia elemento
id:Unsur kimia
ia:Elemento chimic
is:Frumefni
it:Elemento chimico
he:יסוד כימי
jv:Unsur kimia
kn:ಮೂಲಧಾತು
ka:ქიმიური ელემენტი
sw:Elementi za kikemia
ht:Eleman chimik
ku:Element
la:Elementum
lv:Ķīmiskais elements
lt:Cheminis elementas
jbo:selratni
lmo:Element chimich
hu:Kémiai elem
mk:Хемиски елемент
ml:മൂലകം
mt:Element kimiku
mr:मूलद्रव्य
ms:Unsur kimia
mn:Химийн элемент
my:ဒြပ်စင်
nl:Chemisch element
ne:रसायनिक तत्त्व
new:रसायनिक तत्त्व
ja:元素
no:Grunnstoff
nn:Grunnstoff
nrm:Êlément
nov:Elemente
oc:Element quimic
mhr:Химий тӱҥлык
uz:Kimyoviy unsur
pa:ਰਸਾਇਣਕ ਤੱਤ
pnb:کیمیائی عنصر
pap:Elemento kímiko
pms:Element chìmich
nds:Cheemsch Element
pl:Pierwiastek chemiczny
pt:Elemento químico
ro:Element chimic
qu:Qallawa
rue:Хемічный елемент
ru:Химический элемент
sah:Химия элемена
sco:Element
stq:Element
sq:Lista e elementeve kimikë
scn:Elimentu chìmicu
si:රසායනික මූලද්රව්යය
simple:Chemical element
sk:Chemický prvok
sl:Kemični element
sr:Хемијски елемент
sh:Kemijski element
su:Unsur kimia
fi:Alkuaine
sv:Grundämne
tl:Elementong kimikal
ta:தனிமம்
roa-tara:Elemende chìmeche
tt:Химик элемент
te:మూలకము
th:ธาตุเคมี
tg:Элементҳои кимёӣ
tr:Kimyasal element
uk:Хімічний елемент
ur:کیمیائی عنصر
vec:Elemento chimego
vi:Nguyên tố hóa học
fiu-vro:Keemiline element
war:Elemento kimiko
wo:Xeet
yi:כעמישער עלעמענט
yo:Apilẹ̀ṣẹ̀ kẹ́míkà
zh-yue:元素
bat-smg:Kemėnis elements
zh:化學元素