Chemical element

A chemical element, often called simply an element, is a substance that cannot be decomposed or transformed into other chemical substances by ordinary chemical processes. All matter consists of these elements and as of 2006, 117 unique elements have been discovered or artificially created. The smallest particle of such an element is an atom, which consists of electrons centered about a nucleus of protons and neutrons.



Chemistry terminology

Earlier an element or pure element was defined as a substance which "can't be further broken down into another compound with different chemical properties"—which should be taken to mean it consists of atoms of one element. However, because of allotropy, the isotope effect, and the confusion with the more useful term referring to the general class of atoms (irrespective of what compound it may be in), this usage is in disfavor amongst contemporary chemists, and sees restricted, mostly historical, use. This definition was motivated by the observation that these elements could not be dissociated by chemical means into other compounds. For example, water could be converted into hydrogen and oxygen, but hydrogen and oxygen could not be further decomposed, thus "elemental". There are also many counterexamples (for example "elemental oxygen" (O2) can be decomposed by solely chemical means into oxygen ions and atoms which have drastically different chemical properties). This article will concern itself with the latter definition.



The lightest elements are hydrogen and helium. All the heavier elements are made, both naturally and artificially, through various methods of nucleosynthesis. As of 2006, there are 117 known elements: 94 occur naturally on Earth (six in trace quantities: technetium, atomic number 43; promethium, atomic number 61; astatine, atomic number 85; francium, atomic number 87; neptunium, atomic number 93; and plutonium, atomic number 94) and 95 (including californium) have been detected in the universe at large. The 23 elements not found on earth are derived artificially; 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 the element may have been discovered naturally in 1925. All artificially derived elements are radioactive with short half-lives, so if any atoms of these elements were present at the formation of Earth they are extremely likely to have already decayed.

Lists of the elements by name, by symbol, by atomic number, by density, by melting point, and by boiling point as well as Ionization energies of the elements are available. The most convenient presentation of the elements is in the periodic table, which groups elements with similar chemical properties together.


Atomic number

The atomic number of an element, Z, is equal to the number of protons which defines the element. For example, all carbon atoms contain 6 protons in their nucleus, so for carbon Z=6. These atoms may have different numbers of neutrons, which are known as isotopes of the element.


Atomic mass

The atomic mass of an element, A, as measured in unified atomic mass units (u) is the average mass of all the atoms of the element in an environment of interest (usually the earth's crust and atmosphere). Since electrons are of negligible mass, and neutrons are barely more than the mass of the proton, for lighter elements this often corresponds to the sum of the protons and neutrons in the nucleus of the most abundant isotope. However, particularly with heavier elements, more than one stable isotopes contributes significantly to the average atomic mass. An example is chlorine, which is about three-quarters 35Cl and a quarter 37Cl.

The atomic masses that are given on the periodic table are actually the mean abundance-corrected atomic masses for natural samples of the element, which are calculated by the following method. As an example, assume there naturally exist two isotopes of chlorine with respective atomic masses 35 and 37 AMU. Assume that 75% of the atoms in natural chlorine happen to be the 35 AMU version and 25% of the total number of atoms (particles) happen to be about 37 AMU in mass. Multiplying these gives 35 * 0.75 = 26.25 AMU and 37 * 0.25= 9.25 AMU, and the fraction-weighted atomic mass that results is the sum of these numbers, which is 35.5 AMU. For an element with three naturally occurring isotopes the method is the same: sum the masses of the isotopes weighted by atom-fraction. This method of calculating the average mass takes into account the relative abundance of all of the isotopes of an element, so that this mass number always gives the same total number of atoms, for a natural sample of any element. This allows for approximate counting of atoms in a natural element sample, by simply weighing the sample. There are many instances in nature (particularly with light and volitile elements) where isotope ratios are slightly affected by natural sorting processes, but in most cases the atomic masses given may be used to estimate number of atoms in a natural sample to four or more significant figures.



Some isotopes are radioactive and decay into other elements upon radiating an alpha or beta particle. Certain elements have no nonradioactive 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.



The naming of elements precedes the atomic theory of matter, although at the time it was not known which chemicals were elements and which compounds. When it was learned, existing names (e.g., gold, mercury, iron) were kept in most countries, and national differences emerged over the names of elements either for convenience, linguistic niceties, or nationalism. For example, the Germans use "Wasserstoff" for "hydrogen" and "Sauerstoff" for "oxygen," while English and some romance languages use "sodium" for "natrium" and "potassium" for "kalium," and the French, Greeks and Poles prefer "azote/azot" for "nitrogen."

But for international trade, the official names of the chemical elements both ancient and recent are decided by the International Union of Pure and Applied Chemistry, which has decided on a sort of international English language. That organization has recently prescribed that "aluminium" and "caesium" take the place of the US spellings "aluminum" and "cesium," while the US "sulfur" takes the place of the British "sulphur." But chemicals which are practicable to be sold in bulk within many countries, however, still have national names, and those which do not use the Latin alphabet cannot be expected to use the IUPAC name. According to IUPAC, the full name of an element is not capitalized, even if it is derived from a proper noun such as the elements californium or einsteinium (unless it would be capitalized by some other rule, for instance if it begins a sentence, or an article or subsection title in a Wikipedia article). Isotopes of chemical elements are also uncapitalized if written out: carbon-12 or uranium-235.

In the second half of the twentieth century physics laboratories became able to produce nuclei of chemical elements that have a half life too short for them to remain in any appreciable amounts. These are also named by IUPAC, which generally adopts the name chosen by the discoverer. This can lead to the controversial question of which research group actually discovered an element, a question which delayed the 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 nineteenth 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. 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

For the listing of current and not used Chemical symbols, and other symbols that look like chemical symbols, please see List of elements by symbol.

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 - 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, "Hg" (hydrargyrum) for mercury, "K" (kalium) for potassium, "Au" (aurum) for gold, 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).


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.


Isotope symbols

Although not officially used, in nuclear physics the three main isotopes of the element hydrogen are often written as H for protium, D for deuterium and T for tritium. This is in order to make it easier to use them in chemical equations, as it replaces the need to write out the AMU for each isotope. It is written like this:

D2O (heavy water)

Instead of writing it like this:



Most common elements in the Universe

These are the ten most common elements in the Universe as measured in parts per million, by mass:

Element Parts per million
Hydrogen 739,000
Helium 240,000
Oxygen 10,700
Carbon 4,600
Neon 1,340
Iron 1,090
Nitrogen 970
Silicon 650
Magnesium 580
Sulfur 440

Recently discovered elements

The first transuranium element (element with atomic number greater than 92) discovered was Neptunium in 1940. The heaviest element that has been found to date is element 118, Ununoctium, which was successfully synthesized on October 9, 2006, by the Flerov Laboratory of Nuclear Reactions in Dubna, Russia[1]

Element 117, Ununseptium, is yet to be created or discovered, although its place in the periodic table is preestablished, and likewise for possible elements beyond 118.



  1. Controversy-Plagued Element 118, the Heaviest Atom Yet, Finally Discovered (2006-10-13).

See also


External links


Chemical information

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