At A Glance: Gd

Atomic Number: 64
Atomic Symbol: Gd
Atomic Weight: 157.25
Electron Configuration: [Xe]6s24f75d1
Atomic Radius: 237 pm (Van der Waals)
Melting Point: 1313 °C
Boiling Point: 3273 °C
Oxidation States: 3
Sources: Bastnasite and monazite are the principal ores containing gadolinium.

Uses: Phosphors in television, microwave applications, heat resistant metals and alloys.

Content provided by Los Alamos National Laboratory. Used with permission.

Rare earth element - Gadolinium
Rare earth element - Gadolinium
Gadolinium Spin Video

Photos of rare earth elements used on our site are copyright of Max Whitby and Theodore Gray. Used with permission.

Gadolinium yttrium garnets are used in microwave applications and gadolinium compounds are used as phosphors in color television sets. The metal has unusual superconductive properties. As little as 1 percent gadolinium improves the workability and resistance of iron, chromium, and related alloys to high temperatures and oxidation. Gadolinium ethyl sulfate has extremely low noise characteristics and may find use in duplicating the performance of amplifiers, such as the maser.

The metal is ferromagnetic. Gadolinium is unique for its high magnetic movement and for its special Curie temperature (above which ferromagnetism vanishes) lying just at room temperature, meaning it could be used as a magnetic component that can sense hot and cold.

Gadolinium’s unique magnetic behavior allows it to be used in alloys that form the heart of magneto-optic recording technology used for handling computer data. Many such data storage devices utilize Gadolinium. Super computers contain Gadolinium based bubble-memory crystal substrates. Magnetic resonance imaging (MRI) systems use materials containing Gadolinium to enhance the resulting images. Gadolinium is also the single most efficient component used in the detection of power plant radiation leaks.


From gadolinite, a mineral named for Gadolin, a Finnish chemist. The rare earth metal is obtained from the mineral gadolinite. Gadolinia, the oxide of gadolinium, was separated by Marignac in 1880 and Lecoq de Boisbaudran independently isolated it from Mosander’s yttria in 1886.


Gadolinium is found in several other minerals, including monazite and bastnasite, both of which are commercially important. With the development of ion-exchange and solvent extraction techniques, the availability and prices of gadolinium and the other rare-earth metals have greatly improved. The metal can be prepared by the reduction of the anhydrous fluoride with metallic calcium.


Natural gadolinium is a mixture of seven isotopes, but 17 isotopes of gadolinium are now recognized. Although two of these, 155Gd and 157Gd, have excellent capture characteristics, they are only present naturally in low concentrations. As a result, gadolinium has a very fast burnout rate and has limited use as a nuclear control rod material.


As with other related rare-earth metals, gadolinium is silvery white, has a metallic luster, and is malleable and ductile. At room temperature, gadolinium crystallizes in the hexagonal, close-packed alpha form. Upon heating to 1235°C, alpha gadolinium transforms into the beta form, which has a body-centered cubic structure.

The metal is relatively stable in dry air, but tarnishes in moist air and forms a loosely adhering oxide film which falls off and exposes more surface to oxidation. The metal reacts slowly with water and is soluble in dilute acid.

Gadolinium has the highest thermal neutron capture cross-section of any known element (49,000 barns).

Sources: Los Alamos National Laboratory; Molycorp

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