Chemical Element Article Index for
Chemical
Articles about
Chemical Element
Website Links For
Chemical
 

Information About

Chemical Element




A chemical element, or '''element''', is a type of Atom that is defined by its Atomic Number ; that is, by the number of Proton s in its Nucleus . The term is also used to refer to a pure chemical substance composed of atoms with the same number of protons. Compendium Of Chemical Terminology , chemical element

Common examples of elements are Hydrogen , Nitrogen , and Carbon . In total, 117 elements have been observed as of 2007, of which 94 occur naturally on Earth. Elements with atomic numbers greater than 82 (i.e,. Bismuth and those above), are inherently unstable and undergo radioactive decay. In addition, elements 43 and 61 ( Technetium and Promethium ) have no stable Isotopes , and also decay. However, even the elements up to atomic number 94 with no stable nuclei are nevertheless found in nature, as a result of the natural decay processes of Uranium and Thorium .A. Earnshaw, Norman Greenwood. ''Chemistry of the Elements, Second Edition''. Butterworth-Heinemann, 1997

All Chemical Matter consists of these elements. New elements are discovered from time to time through artificial Nuclear Reaction s.


HISTORY

The term ' (fire), Octahedron (air), Icosahedron (water), and Cube (earth).1

Adding to the Four Elements of the Greek philosopher Empedocles , in about 350 BC, Aristotle also used the term "element" and conceived of a fifth element called " Quintessence ", which formed the heavens. Aristotle defined an element as:

Building on this theory, in c. 790 Arabian chemist Jabir ibn-Hayyan ( Geber ) postulated that metals were formed out of two elements: sulphur, ‘the stone which burns’, which characterized the principle of combustibility, and mercury, which contained the idealized principle of metallic properties.Strathern, Paul. (2000). Mendeleyev’s Dream – the Quest for the Elements. New York: Berkley Books. Shortly thereafter, this evolved into the Arabic concept of the three principles: sulphur giving flammability or combustion, mercury giving volatility and stability, and salt giving solidity.

In 1524, Swiss chemist Paracelsus adopted Aristotle’s four element theory, but reasoned that they appeared in bodies as Geber’s three principles. Paracelsus saw these principles as fundamental, and justified them by recourse to the description of how wood burns in fire. Mercury included the cohesive principle, so that when it left in smoke the wood fell apart. Smoke represented the volatility (the mercury principle), the heat-giving flames represented flammability (sulphur), and the remnant ash represented solidity (salt).

In 1669, German physician and chemist Johann Becher published his Physica Subterranea, in which, in modification on the ideas of Paracelsus, he argued that the constituents of bodies are air, water, and three types of earth: ''terra fluida'', the mercurial element, which contributes fluidity and volatility; ''terra lapida'', the solidifying element, which produces fusibility or the binding quality; and ''terra pinguis'', the fatty element, which gives material substance its oily and combustible qualities.Partington, J.R. (1937). A Short History of Chemistry. New York: Dover Publications, Inc. These three earths correspond with Geber’s three principles. A piece of wood, for example, according to Becher, is composed of ash and terra pinguis; when the wood is burnt, the terra pinguis is released, leaving the ash. In other words, in combustion the fatty earth burns away.

In 1661, Robert Boyle showed that there were more than just four Classical Element s as 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 accepted elements. In 1869, in Mendeleev 's famous Periodic Table , shown below, there were sixty-six elements.
's 1869 Periodic Table ]]

From Boyle until the early 20th century, an element was defined as a pure Substance that cannot be decomposed into any simpler substance.3 Said another way, an "element" cannot be transformed into other chemical substances by Chemical processes. In 1913, Henry Moseley discovered that the physical basis of the atomic number of the atom was its nuclear charge, which eventually led to the current definition. The current definition also avoids some ambiguities due to Isotopes and Allotropes .

By 1919, there were seventy-two known elements.4 In 1955, element 101 was discovered and named Mendelevium in honor of Mendeleev, the first to arrange the elements in a periodic manner. In October 2006, the synthesis of element 118 was reported; however, element 117 has not yet been created in the laboratory.


DESCRIPTION

The lightest elements are , including occasionally by activities such as Nuclear Fission .

, 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 remaining 22 elements not found on Earth or in astronomical spectra have been derived artificially. All of the solely-artificially derived elements 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 are 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 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 trace elements.

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 the atomic number "Z" of carbon is 6. Carbon atoms may have different numbers of neutrons, which are known as Isotope s of the element.

The number of protons in the atomic nucleus also detemines its Electric Charge , which in turn determines the Electron s of the atom in its Non-ionized state. This in turn (by means of the Exclusion Principle ) determines the atom's various Chemical Properties . So all carbon atoms, for example, ultimately have identical chemical properties because they all have the same number of protons in their nucleus, and therefore have the same atomic number. It is for this reason that atomic number rather than Mass Number (or Atomic Weight ) is considered the identifying characteristic of an 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 which 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 which is close to a natural number, which in general differs slightly from the mass number because the mass of the protons and neutrons is not exactly 1 u, because 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, due to the ''definition of u'' (it is fixed as 1/12th of the mass of a free carbon-12 atom, exactly).


Isotopes

Isotope s are atoms of the same element (that is, with the same number of protons in their atomic nucleus), but having ''different'' numbers of Neutron s. Most naturally-occurring elements have more than one 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.

All three of the isotopes of carbon have the same chemical properties. But they have different nuclear properties. In this example, carbon-12 and carbon-13 are stable atoms, but Carbon-14 is unstable; it is slightly Radioactive , decaying over time into other elements.

Like carbon, some greater than 82.


Allotropes

Some elements can be found as multiple elementary substances, known as Allotropes , which differ in their structure and 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, and Fullerene s, which have nearly spherical shapes. The ability for an element to exist in one of several structural forms is known as 'allotropy'.


Standard state

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.


NOMENCLATURE

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 Language s use "sodium" for "natrium" and "potassium" for "kalium", and the French, Greeks and Poles prefer "azote/azot" for "nitrogen".

But for international trade, the 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 Symbol s, 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 , "Pb" (plumbum) for Lead , 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

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 mass number for each atom. It is written like this:

D2O ( Heavy Water )

Instead of writing it like this:

2H2O


ABUNDANCE

See Also: Abundance of the chemical elements