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Gadolinium (revised)


Note: This article, originally published in 1998, was updated in 2006 for the eBook edition.


Gadolinium was named for Finnish chemist Johan Gadolin (1760-1852). Gadolin served for many years as professor of chemistry at the University of Åbo in Finland. He was the first person to study an unusual black stone discovered near the town of Ytterby, Sweden, in 1787. The stone was an unusually important discovery. Chemists isolated nine new elements from the stone, one of which was gadolinium.




rare earth metal)


Gadolinium is in Row 6 of the periodic table. The periodic table is a chart that shows how chemical elements are related to each other. The elements in Row 6 are called rare earth elements. They really aren't rare, but they are difficult to separate. For this reason, scientists know less about the rare earth elements than they do about most other elements. The rare earth metals are also called lanthanides. That name comes from the first element in Row 6, lanthanum.

Discovery and naming

Two unusual rocks were discovered in Sweden near the end of the eighteenth century. The rocks were unusual because they both contained a complex mixture of substances. Chemists worked for nearly a century to separate the mixtures and find out what they were. All fifteen rare earth elements were first discovered in the two Swedish rocks.

One rock contained a mineral that had never been seen before, cerite. Cerite was first discovered in 1803. The last new element found in cerite was not identified until almost a century later, in 1901. In 1880, French chemist Jean-Charles Galissard de Marignac (1817-94) was studying a new material found in cerite called samaria. Earlier chemists had identified samaria as a new element.

Marignac found that samaria was not a pure element. Instead, it consisted of two parts, which he called samaria and gadolinia. He believed each was a new element. He was right about gadolinia, but wrong about samaria.

Physical properties

Gadolinium has a shiny metallic luster with a slight yellowish tint. It is both ductile and malleable. Ductile means capable of being made into wires. Malleable means capable of being hammered or rolled into thin sheets. It has a melting point of 1,312°C (2,394°F) and a boiling point of about 3,000°C (5,400°F). Its density is 7.87 grams per cubic centimeter.

Few elements are as strongly magnetic as gadolinium. It also has the highest neutron-absorbing ability of any element. A piece of gadolinium stops neutrons better than any other element.

Chemical properties

Gadolinium metal is not especially reactive. It dissolves in acids and reacts slowly with cold water. It also reacts with oxygen at high temperatures.

Occurrence in nature

The abundance of gadolinium in the Earth's surface is estimated at about 4.5 to 6.4 parts per million. That would make it one of the most abundant of the rare earth elements. It ranks above bromine and uranium, but just below lead and boron in order of abundance. Some minerals in which it occurs are monazite, bastnasite, samarskite, gadolinite, and xenotime.


Seven naturally occurring isotopes of gadolinium are known. They are gadolinium-152, gadolinium-154, gadolinium-155, gadolinium-156, gadolinium-157, gadolinium-158, and gadolinium-160. Isotopes are two or more forms of an element. Isotopes differ from each other according to their mass number. The number written to the right of the element's name is the mass number. The mass number represents the number of protons plus neutrons in the nucleus of an atom of the element. The number of protons determines the element, but the number of neutrons in the atom of any one element can vary. Each variation is an isotope. One of gadolinium's naturally occurring isotopes is radioactivegadolinium-152. A radioactive isotope is one that breaks apart and gives off some form of radiation.

Radioactive isotopes can also be produced artificially when very small particles are fired at atoms. These particles stick in the atoms and make them radioactive. At least eleven artificial radioactive isotopes have been produced. Some of these are used in medicine. For example, gadolinium-153 is used to study the composition of bones. The radiation it gives off acts like X rays, penetrating the bones to reveal the minerals present.

Gadolinium is also used in another X-ray-like technique called neutron radiography. In this technique, neutrons are fired through a sample of material. The neutrons act somewhat like X rays. They show the structure of the material. Adding gadolinium to the back side of the material makes the neutron image easier to read. Neutron radiography is especially useful because one can look for damage inside a piece of metal without having to take the material apart.


The method for obtaining gadolinium from its ores is similar to that for other rare earth elements. The ore is converted into gadolinium chloride (GdCl3) or gadolinium fluoride (GdF3). Passing an electric current through the first compound releases pure gadolinium:

Nine new elements, including gadolinium, came from an unusual black stone found in Ytterby, Sweden, in 1787.

Adding calcium to the second compound also releases pure gadolinium:

Uses and compounds

Gadolinium is used in control rods in nuclear power plants. Energy produced during nuclear fission is used to generate electricity. Nuclear fission is the process in which large atoms (usually uranium or plutonium ) break apart, releasing energy. The smaller atoms produced are called fission products and are radioactive.

Neutrons are also produced in the reaction. In order for a nuclear power plant to work properly, the number of neutrons must be carefully controlled. Rods containing gadolinium are raised out of or lowered into the reactor. This allows more or fewer neutrons to remain in the reaction.

Gadolinium also has medical uses. It is used to locate the presence of tumors in the inner ear. Gadolinium is injected into the blood stream. It then goes to any tumor that happens to be present in the ear. The tumor appears darker when seen with X rays.

Gadolinium is used to locate tumors in the inner ear.

Gadolinium compounds are used as phosphors in television tubes. A phosphor is a material that shines when struck by electrons. The color of the phosphor depends on the elements of which it is made.

Gadolinium is also found in alloys and special minerals known as yttrium garnets. An alloy is made by melting and mixing two or more metals. The mixture has properties different from those of the individual metals. Gadolinium alloys are easier to work with than alloys without gadolinium. Gadolinium yttrium garnets are used in microwave ovens to produce the microwaves.

What on Earth is an "Earth"?

B ooks on the chemical elements sometimes talk about gadolinium and gadolinia; about erbium and sometimes erbia; sometimes about samarium and sometimes samaria. Is the -ium ending any different from the -ia ending?

The answer is yes. Almost all metal names end in -ium or just -um, like sodium, potassium, magnesium, aluminum, and gadolinium. The ending -ia or just -a, on the other hand, stands for the form in which an element occurs in the earth. When miners take gadolinium out of the earth, it is called gadolinia.

The natural form of the element is often called an "earth." Gadolinium is the element that comes from the earth, gadolinia. Earths are compounds of the element and one or more other element. Two common combining elements are oxygen and sulfur. For example, gadolinia contains gadolinium oxide (Gd2O3).

These terms can be confusing when reading the history of chemical elements. Many elements were first discovered not in their pure form, but as compoundsas earths.

Health effects

Not many details of the health effects of gadolinium are known. It is usually handled as if it were very toxic.

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melting point: 1,311°C
boiling point: 3,233.0 °C
density: 7.89 g cm 3
most common ion: Gd 3+

Gadolinium is a chemical element. Its ground state electronic configuration is [Xe]4f75d6s2. Monazite and bastnasite are the principal gadolinium ores, in which gadolinium occurs together with other members of the rare earth elements or the lanthanides . It can be separated from the other rare earths by ion exchange or solvent extraction techniques. Gadolinia, the oxide of gadolinium, was first extracted from the mineral gadolinite by Jean-Charles-Galissard de Marignac in 1880. (Gadolinite is named after the Finnish chemist Johan Gadolin.) In 1886 Paul-Émile Lecoq de Boisbaudran independently separated the oxide of gadolinium from Carl Mosander's "yttria" (impure yttrium oxide).

Gadolinium is a silver-white, malleable, and ductile metal . Gadolinium metal is ferromagnetic just below room temperature. Gadolinium chemistry is dominated by the trivalent gadolinium(III) ion, Gd3+. This ion forms ionic bonds with ligands containing an oxygen or nitrogen donor atom. The ground state electronic configuration of Gd3+ is [Xe]4f7. In spectroscopic

analysis there are no absorption bands in the visible region of the electromagnetic spectrum, and gadolinium compounds are colorless.

Gadolinium(III) chelates are used as contrast reagents in magnetic resonance imaging (MRI). Due to the high magnetic moment of the paramagnetic Gd3+ ion (with its seven unpaired electrons), the relaxation time of water molecules in the proximity of Gd3+ ions is greatly reduced and signal intensity is thereby enhanced. MRI is a medical diagnostic technique that depends on the proton nuclear magnetic resonance (NMR) signal from water in its creation of a proton density map. Gadolinium is a major component of x-ray phosphors, such as Gd2O2S:Tb3+, within which it dilutes the active emitter (Tb3+) to avoid concentration quenching. Because gadolinium effectively absorbs neutrons, this element has found some use in control rods for nuclear reactors.

see also Cerium; Dysprosium; Erbium; Europium; Gadolin, Johan; Holmium; Lanthanides; Lanthanum; Lutetium; Neodymium; Praseodymium; Promethium; Samarium; Terbium; Ytterbium.

Koen Binnemans


Bünzli, Jean-Claude G., and Choppin, Gregory R., eds. (1989). Lanthanide Probes in Life, Chemical and Earth Sciences. New York: Elsevier.

Cotton, Simon (1991). Lanthanides and Actinides. New York: Oxford University Press.

Kaltsoyannis, Nikolas, and Scott, Peter (1999). The f Elements. New York: Oxford University Press.

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gadolinium (gădəlĬn´ēəm), metallic chemical element; symbol Gd; at. no. 64; at. wt. 157.25; m.p. 1,312°C; b.p. 3,233°C; sp. gr. 7.898 at 25°C; valence +3. Gadolinium is a malleable, ductile, lustrous silver-white metal with a hexagonal close-packed crystalline structure at room temperature. It is a rare-earth metal found in Group 3 of the periodic table. Although the metal does not tarnish in dry air, in moist air an oxide film forms; the film flakes off, exposing more metal to oxidation. Gadolinium reacts slowly with water and dissolves in dilute mineral acids. It occurs in nature in its salts and especially as the oxide, gadolinia, a rare earth. It is a component of the minerals gadolinite, monazite, and bastnasite. Naturally occurring gadolinium is a mixture of seven isotopes; ten additional isotopes are known. Although gadolinium absorbs neutrons more effectively than does any other known substance, this property is caused by two isotopes that are present only to a limited extent in natural gadolinium. Gadolinium has found some use in control rods for nuclear reactors; it has also been used as a "poison" in nuclear fuels, added to control the initial rapid reaction and "burning out" as the reaction proceeds. Gadolinium metal can be prepared by reduction of anhydrous gadolinium fluoride with calcium metal. Gadolinium has unusual magnetic properties. At room temperature the metal is paramagnetic, but it becomes strongly ferromagnetic when cooled. Gadolinium compounds are used as phosphors in the manufacture of color-television picture tubes. Gadolinia, the oxide, was extracted from the mineral gadolinite [for J. Gadolin, a Finnish chemist] in 1880 by J. C. G. de Marignac; in 1886, P. E. Lecoq de Boisbaudran independently isolated the oxide from Mosander's "yttria."

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gadolinium (symbol Gd) Silvery white metallic element of the lanthanide series. Chief ores are gadolinite, monazite and bastnaesite. Its uses include neutron absorption and the manufacture of certain alloys. Properties: 64; r.a.m. 157.25; r.d. 7.898; m.p. 1311°C (2392°F); b.p. 3233°C (5851°F); most common isotope Gd158 (24.87%).

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gad·o·lin·i·um / ˌgadlˈinēəm/ • n. the chemical element of atomic number 64, a soft silvery-white metal of the lanthanide series. (Symbol: Gd)

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