A chemical element can be defined in one of two ways: experimentally or theoretically. Experimentally, an element is any substance that cannot be broken down into any simpler substance. Imagine that you are given a piece of pure iron and asked to break it down using any device or method ever invented by chemists. Nothing you can do will ever change the iron into anything simpler. Iron, therefore, is an element.
The experimental definition of an element can be explained by using a second definition: an element is a substance in which all atoms are of the same kind. If there were a way to look at each of the individual atoms in the bar of pure iron mentioned above, they would all be the same—all atoms of iron. In contrast, a chemical compound, such as iron oxide, always contains at least two different kinds of atoms, in this case, atoms of iron and atoms of oxygen.
Words to Know
Atomic mass: The mass of the protons, neutrons, and electrons that make up an atom.
Atomic number: The number of protons in the nucleus of an element's atom.
Chemical symbol: A letter or pair of letters that represents some given amount of an element.
Compound, chemical: A substance that consists of two or more chemical elements joined to each other in a specific proportion.
Metal: An element that loses electrons in chemical reactions with other elements.
Metalloid: An element that acts sometimes like a metal and sometimes like a nonmetal.
Nonmetal: An element that tends to gain electrons in chemical reactions with other elements.
Periodic table: A system of classifying the chemical elements according to their atomic number.
Synthetic element: An element that is made artificially in a laboratory but is generally not found in nature.
Natural and synthetic elements
Ninety-two chemical elements occur naturally on Earth. The others have been made synthetically or artificially in a laboratory. Synthetic elements are usually produced in particle accelerators (devices used to increase the velocity of subatomic particles such as electrons and protons) or nuclear reactors (devices used to control the energy released by nuclear reactions). The first synthetic element to be produced was technetium, discovered in 1937 by Italian American physicist Emilio Segrè (1905–1989) and his colleague C. Perrier. Except for technetium and promethium, all synthetic elements have larger nuclei than uranium.
Two Dozen Common and Important Chemical Elements
|Percent of all atoms*|
|Element||Symbol||In the universe||In Earth's crust||In sea water||In the human body||Characteristics under ordinary room conditions|
|*If no number is entered, the element constitutes less than 0.1 percent.|
|Aluminum||Al||—||6.3||—||—||A lightweight, silvery metal|
|Calcium||Ca||—||2.1||—||.02||Common in minerals, seashells, and bones|
|Carbon||C||—||—||—||10.7||Basic in all living things|
|Chlorine||Cl||—||—||0.3||—||A toxic gas|
|Copper||Cu||—||—||—||—||The only red metal|
|Gold||Au||—||—||—||—||The only yellow metal|
|Helium||He||7.1||—||—||—||A very light gas|
|Hydrogen||H||92.8||2.9||66.2||60.6||The lightest of all elements; a gas|
|Iodine||I||—||—||—||—||A nonmetal; used as antiseptic|
|Iron||Fe||—||2.1||—||—||A magnetic metal; used in steel|
|Lead||Pb||—||—||—||—||A soft, heavy metal|
|Magnesium||Mg||—||2.0||—||—||A very light metal|
|Mercury||Hg||—||—||—||—||A liquid metal; one of the two liquid elements|
|Nickel||Ni||—||—||—||—||A noncorroding metal; used in coins|
|Nitrogen||N||—||—||—||2.4||A gas; the major component of air|
|Oxygen||O||—||60.1||33.1||25.7||A gas; the second major component of air|
|Phosphorus||P||—||—||—||0.1||A nonmetal; essential to plants|
|Potassium||K||—||1.1||—||—||A metal; essential to plants; commonly called "potash"|
|Silicon||Si||—||20.8||—||—||A semiconductor; used in electronics|
|Silver||Ag||—||—||—||—||A very shiny, valuable metal|
|Sodium||Na||—||2.2||0.3||—||A soft metal; reacts readily with water, air|
|Sulfur||S||—||—||—||0.1||A yellow nonmetal; flammable|
|Titanium||Ti||—||0.3||—||—||A light, strong, noncorroding metal used in space vehicles|
|Uranium||U||—||—||—||—||A very heavy metal; fuel for nuclear power|
At the beginning of the twenty-first century, there were 114 known elements, ranging from hydrogen (H), whose atoms have only one electron, to the as-yet unnamed element whose atoms contain 114 electrons. New elements are difficult to produce. Only a few atoms can be made at a time, and it usually takes years before scientists agree on who discovered what and when.
More than 100 years ago, chemists began searching for ways to organize the chemical elements. At first, they tried listing them by the size (mass) of their nucleus, their atomic mass. Later, they found that using the number of protons in their atomic nuclei was a more effective technique. They invented a property known as atomic number for this organization. The atomic number of an element is defined as the number of protons in the nucleus of an atom of that element. Hydrogen has an atomic number of 1, for example, because the nuclei of hydrogen atoms each contain one—and only one—proton. Similarly, oxygen has an atomic number of 8 because the nuclei of all oxygen atoms contain 8 protons. The accompanying table (periodic table of the elements) contains a list of the known chemical elements arranged in order according to their atomic number.
Notice that the chemical symbol for each element is also included in the table. The chemical symbol of an element is a letter or pair of letters that stands for some given amount of the element, for example, for one atom of the element. Thus, the symbol Ca stands for one atom of calcium, and the symbol W stands for one atom of tungsten. Chemical symbols, therefore, are not really abbreviations.
Chemical elements can be fully identified, therefore, by any one of three characteristics: their name, their chemical symbol, or their atomic number. If you know any one of these identifiers, you immediately know the other two. Saying "Na" to a chemist immediately tells that person that you are referring to sodium, element #11. Similarly, if you say "element 19," the chemist knows that you're referring to potassium, known by the symbol K.
The system of classifying elements used by chemists today is called the periodic table. The law on which the periodic table is based was first discovered almost simultaneously by German chemist Julius Lothar Meyer (1830–1895) and Russian chemist Dmitry Mendeleev (1834–1907) in about 1870. The periodic table is one of the most powerful tools in chemistry because it organizes the chemical elements in groups that have similar physical and chemical properties.
Properties of the elements
One useful way of describing the chemical elements is according to their metallic or nonmetallic character. Most metals are hard with bright, shiny surfaces, often white or grey in color. Since important exceptions to this rule exist, metals are more properly defined according to the way they behave in chemical reactions. Metals, by this definition, are elements that lose electrons to other elements. By comparison, nonmetals are elements that gain electrons from other elements in chemical reactions. (They may be gases, liquids, or solids but seldom look like a metal.) The vast majority (93) of the elements are metals; the rest are nonmetals.
A Who's Who of the Elements
|Astatine (At)||The rarest||Rarest of the naturally occurring elements|
|Boron (B)||The strongest||Highest stretch resistance|
|Californium (Cf)||The most expensive||Sold at one time for about $1 billion a gram|
|Carbon (C)||The hardest||As diamond, one of its three solid forms|
|Germanium (Ge)||The purest||Has been purified to 99.99999999 percent purity|
|Helium (He)||The lowest melting point||−271.72°C at a pressure of 26 times atmospheric pressure|
|Hydrogen (H)||The lowest density||Density 0.0000899 g/cc at atmospheric pressure and 0°C|
|Lithium (Li)||The lowest–density metal||Density 0.534g/cc|
|Osmium (Os)||The highest density||Density 22.57 g/cc|
|Radon (Rn)||The highest–density gas||Density 0.00973 g/cc at atmospheric pressure and 0°C|
|Tungsten (W)||The highest melting point||3,420°C|
The concept of a chemical element goes back more than 2,000 years. Ancient Greek philosophers conceived of the idea that some materials are more fundamental, or basic, than others. They listed obviously important materials such as earth, air, fire, and water as possibly being such "elemental" materials. These speculations belonged in the category of philosophy, however, rather than science. The Greeks had no way of testing their ideas to confirm them.
In fact, a few elements were already known long before the speculations of the Greek philosophers. No one at that time called these materials elements or thought of them as being different from the materials we call compounds today. Among the early elements used by humans were iron, copper, silver, tin, and lead. We know that early civilizations knew about and used these elements because of tools, weapons, and pieces of art that remain from the early periods of human history.
Another group of elements was discovered by the alchemists, the semimystical scholars who contributed to the early development of chemistry. These elements include antimony, arsenic, bismuth, phosphorus, and zinc.
Formation of the Elements
How were the chemical elements formed? Scientists believe the answer to that question lies in the stars and in the processes by which stars are formed. The universe is thought to have been created at some moment in time 12 to 15 billion years ago. Prior to that moment, nothing other than energy is thought to have existed. But something occurred to transform that energy into an enormous explosion: the big bang. In the seconds following the big bang, matter began to form.
According to the big bang theory, the simplest forms of matter to appear were protons and electrons. Some of these protons and electrons combined to form atoms of hydrogen. A hydrogen atom consists of one proton and one electron; it is the simplest atom that can exist. Slowly, over long periods of time, hydrogen atoms began to come together in regions of space forming dense clouds. The hydrogen in these clouds was pulled closer and closer together by gravitational forces. Eventually these clouds of hydrogen were dense enough to form stars.
A star is simply a mass of matter that generates energy by nuclear reactions. The most common of these reactions involves the combination of four hydrogen atoms to make one helium atom. As soon as stars began to form, then, helium became the second element found in the universe.
As stars grow older, they switch from hydrogen-to-helium nuclear reactions to other nuclear reactions. In another such reaction, helium atoms combine to form carbon atoms. Later carbon atoms combine to form oxygen, neon, sodium, and magnesium. Still later, neon and oxygen combine with each other to form magnesium. As these reactions continue, more and more of the chemical elements are formed.
At some point, all stars die. The nuclear reactions on which they depend for their energy come to an end. In some cases, a star's death is dramatic. It may actually blow itself apart, like an atomic bomb. The elements of which the star was made are then spread throughout the universe. They remain in space until they are drawn into the core of other stars or other astronomical bodies, such as our own Earth. If this theory is correct, then the atoms of iron, silver, and oxygen you see around you every day actually started out life in the middle of a star billions of miles away.
The modern definition of an element was first provided by English chemist Robert Boyle (1627–1691). Boyle defined elements as "certain primitive and simple, or perfectly unmingled bodies; which not being made of any other bodies, or of one another, are the ingredients of which all those call'd perfectly mixed bodies are immediately compounded, and into which they are ultimately resolved." For all practical purposes, Boyle's definition of an element has remained the standard working definition for a chemical element ever since.
By the year 1800, no more than about 25 true elements had been discovered. During the next hundred years, however, that situation changed rapidly. By the end of the century, 80 elements were known. The rapid pace of discovery during the 1800s can be attributed to the development of chemistry as a science, to the improved tools of analysis available to chemists, and to the new predictive power provided by the periodic law of 1870.
During the twentieth century, the last remaining handful of naturally occurring elements were discovered and the synthetic elements were first manufactured.
"Element, Chemical." UXL Encyclopedia of Science. . Encyclopedia.com. (December 10, 2017). http://www.encyclopedia.com/science/encyclopedias-almanacs-transcripts-and-maps/element-chemical-1
"Element, Chemical." UXL Encyclopedia of Science. . Retrieved December 10, 2017 from Encyclopedia.com: http://www.encyclopedia.com/science/encyclopedias-almanacs-transcripts-and-maps/element-chemical-1
By the end of the nineteenth century, the elements and matter comprising all things could no long be viewed as immutable. The dramatic rise of scientific methodology and experimentation during the later half of the eighteenth century set the stage for the fundamental advances in chemistry and physics made during the nineteenth century. In less than a century, European society moved from an understanding of the chemical elements grounded in mysticism to an understanding of the relationships between elements found in a modern periodic table . During the eighteenth century, there was a steady march of discovery with regard to the chemical elements. Isolations of hydrogen and oxygen allowed for the formation of water from its elemental components. Nineteenth century scientists built experiments on new-found familiarity with elements such as nitrogen, beryllium, chromium and titanium.
By the mid-nineteenth century, chemistry was in need of organization. New elements were being discovered at an increasing pace. Accordingly, the challenge for chemists and physicists was to find a key to understand the increasing volume of experimental evidence regarding the properties of the elements. In 1869, the independent development of the periodic law and tables by the Russian chemist Dmitry Mendeleev (1834–1907) and German chemist Julius Meyer (1830–95) brought long sought order and understanding to the elements.
Mendeleev and Meyer did not work in a vacuum. English chemist J.A.R. Newlands (1837–1898) had already published several works that ventured relationships among families of elements, including his "law of octaves" hypothesis. Mendeleev's periodic chart of elements, however, spurred important discoveries and isolation of chemical elements. Most importantly, Mendeleev's table provided for the successful prediction of the existence of new elements and these predictions proved true with the discovery of gallium (1875), scandium (1879) and germanium (1885).
By the end of the nineteenth century, the organization of the elements was so complete that British physicists Lord Rayleigh (born John William Strutt, 1842–1919) and William Ramsay (1852–1916) were able to expand the periodic table and to predict the existence and properties of the noble gases argon and neon.
Nineteenth century advances were, however, not limited to mere identification and isolation of the elements. By 1845, German chemist Adolph Kolbe (1818–84) synthesized an organic compound and, in 1861, another German chemist Friedrich Kekule (1829–1896) related the properties of molecules to their geometric shape. These advances led to the development of wholly new materials (e.g., plastics, celluloids) that had a dramatic impact on a society in midst of industrial revolution.
The most revolutionary development with regard to the elucidation of the elements during the nineteenth century came in the waning years of the century. In 1895, Wilhelm Röntgen (1845–1923) published a paper titled: "On a New Kind of Rays." Röntgen's work offered the first description of x rays and offered compelling photographs of photographs of a human hand. The scientific world quickly grasped the importance of Röntgen's discovery. At a meeting of the French Academy of Science, Henri Becquerel (1852–1908) observed the pictures taken by Röntgen of bones in the hand. Within months Becquerel presented two important reports concerning "uranium rays" back to the Academy. Becquerel, who was initially working with phosphorescence, described the phenomena that later came to be understood as radioactivity . Less than two years later, two other French scientists, Pierre (1859–1906) and Marie Curie (born in Poland, 1867–1934) announced the discovery of the radioactive elements polonium and radium. Marie Curie then set out on a systematic search for radioactive elements and was able, eventually, to document the discovery of radioactivity in uranium and thorium minerals .
As the nineteenth century drew to a close, Ernest Rutherford (1871–1937), using an electrometer, identified two types of radioactivity, which he labeled alpha radiation and beta radiation. Rutherford actually thought he had discovered a new type of x ray. Subsequently alpha and beta radiation were understood to be particles. Alpha radiation is composed of alpha particles (the nucleus of helium). Because alpha radiation is easily stopped, alpha radiation-emitting elements are usually not dangerous to biological organisms (e.g., humans) unless the emitting element actually enters the organism. Beta radiation is composed of a stream of electrons (electrons were discovered by J. J. Thomson in 1897) or positively charged particles called positrons.
The impact of the discovery of radioactive elements produced immediate and dramatic impacts upon society. Within a few years, high-energy electromagnetic radiation in the form of x rays, made possible by the discovery of radioactive elements, was used by physicians to diagnose injury. More importantly, the rapid incorporation of x rays into technology established a precedent increasingly followed throughout the twentieth century. Although the composition and nature of radioactive elements was not fully understood, the practical benefits to be derived by society outweighed scientific prudence.
Italian scientist Alessandro Volta's (1745–1827) discovery, in 1800, of a battery using discs of silver and zinc gave rise to the voltaic pile or the first true batteries. Building on Volta's concepts, English chemist Humphry Davy (1778–1829) first produced sodium from the electrolysis of molten sodium hydroxide in 1807. Subsequently, Davy isolated potassium, another alkali metal, from potassium hydroxide in the same year. Lithium was discovered in 1817.
Studies of the spectra of elements and compounds spawned further discoveries. German chemist Robert Bunsen's (1811–1999) invention of the famous laboratory burner that bears his name allowed for the development of new methods for the analysis of the elemental structure of compounds. Working with Russian-born scientist Gustav Kirchhoff (1824–1887) Bunsen's advances made possible flame analysis (a technique now commonly known as atomic emission spectroscopy [AES]) and established the fundamental principles and techniques of spectroscopy. Bunsen examined the spectra (i.e., component colors), emitted when a substance was subjected to intense flame. Bunsen's keen observation that flamed elements that emit light only at specific wavelengths—and that each element produces a characteristic spectra—along with Kirchhoff's work on black body radiation set the stage for subsequent development of quantum theory . Using his own spectroscopic techniques, Bunsen discovered the elements cesium and rubidium.
Using the spectroscopic techniques pioneered by Bunsen, other nineteenth century scientists began to deduce the chemical composition of stars. These discoveries were of profound philosophical importance to society because they proved that Earth did not lie in a privileged or unique portion of the universe. Indeed, the elements found on Earth, particularly those associated with life, were found to be commonplace in the cosmos. In 1868, French astronomer P.J.C. Janssen (1824–1907) and English astronomer, Norman Lockyer (1836–1920), used spectroscopic analysis to identify helium on the Sun . For the first time an element was first discovered outside the confines of Earth.
See also Atomic mass and weight; Atomic number; Big Bang theory; Stellar life cycle
"Chemical Elements." World of Earth Science. . Encyclopedia.com. (December 10, 2017). http://www.encyclopedia.com/science/encyclopedias-almanacs-transcripts-and-maps/chemical-elements
"Chemical Elements." World of Earth Science. . Retrieved December 10, 2017 from Encyclopedia.com: http://www.encyclopedia.com/science/encyclopedias-almanacs-transcripts-and-maps/chemical-elements
Relative atomic mass1
Valency point °C
Melting point °C
Boiling Point °C
Date of discovery
1 Relative atomic mass: values given in parentheses are for radioactive elements whose relative atomic mass cannot be given precisely without knowledge of origin, and is the atomic mass number of the isotope of longest known half-life
2 Also called hahnium, nielsbohrium, rutherfordium, or element 105
3 Also called unnilquadium (Unq) or element 104
4 Also called wolfram
3, 4, 5, 6
1, 3, 5, 7
1, 3, 5, 7
1, 3, 5, 7
2, 3, 6
1, 3, 5, 7
2, 3, 4, 6, 7
3, 4, 6
4, 5, 6
2, 3, 4, 8
2, 4, 6
3, 4, 5, 6
3, 4, 6, 8
2, 4, 6
2, 4, 6
2, 4, 6
"chemical elements." World Encyclopedia. . Encyclopedia.com. (December 10, 2017). http://www.encyclopedia.com/environment/encyclopedias-almanacs-transcripts-and-maps/chemical-elements
"chemical elements." World Encyclopedia. . Retrieved December 10, 2017 from Encyclopedia.com: http://www.encyclopedia.com/environment/encyclopedias-almanacs-transcripts-and-maps/chemical-elements