Erbium is a chemical element in the periodic table that has the symbol Er and atomic number 68. A rare silvery metallic lanthanide rare earth element, erbium is associated with several other rare elements in the mineral gadolinite from Ytterby in Sweden.
Notable characteristics
A
trivalent element, pure erbium
metal is malleable, soft yet stable in air and does not
oxidize as quickly as some other rare-earth metals. Its
salts are rose-colored and the element gives a characteristic sharp
absorption spectra in
visible light,
ultraviolet, and near
infrared. Otherwise it looks much like the other rare earths. Its
sesquioxide is called
erbia. Erbium's properties are to a degree dictated by the kind and amount of impurities present. Erbium does not play any known biological role but is thought by some to be able to stimulate
metabolism.
Applications
Erbium's everyday uses are varied. It is commonly used as a
photographic filter and because of its resilience it is useful as a metallurgical additive. Other uses:
History
Erbium (for
Ytterby, a town in
Sweden) was
discovered by
Carl Gustaf Mosander in
1843. Mosander separated "yttria" from the mineral
gadolinite into three fractions which he called
yttria,
erbia, and
terbia. He named the new element after the town of Ytterby where large concentrations of yttria and erbium are located. Erbia and terbia, however, were confused at this time. After
1860, terbia was renamed erbia and after
1877 what had been known as erbia was renamed terbia. Fairly pure Er
2O3 was independently isolated in
1905 by
Georges Urbain and
Charles James. Reasonably pure metal wasn't produced until
1934 when workers reduced the
anhydrous chloride with
potassium vapor.
Occurrence
Like other rare earths, this element is never found as a free element in nature but is found bound in
monazite sand ores. It has historically been very difficult and expensive to separate rare earths from each other in their ores but
ion-exchange production techniques developed in the late
20th century have greatly brought down the cost of production of all rare-earth metals and their
chemical compounds. The principal commercial sources of erbium are from the minerals
xenotime and
euxenite. Metallic erbium in dust form presents a fire and explosion hazard.
Isotopes
Naturally occurring erbium is composed of 6 stable
isotopes, Er-162, Er-164, Er-166, Er-167, Er-168, and Er-170 with Er-166 being the most abundant (33.6%
natural abundance). 23
radioisotopes have been characterized, with the most stable being Er-169 with a
half life of 9.4 days, Er-172 with a half-life of 49.3 hours, Er-160 with a half-life of 28.58 hours, Er-165 with a half-life of 10.36 hours, and Er-171 with a half life of 7.516 hours. All of the remaining
radioactive isotopes have half-lifes that are less than 3.5 hours, and the majority of these have half lifes that are less than 4 minutes. This element also has 6
meta states, with the most stable being Er-167m (t
½ 2.269 seconds).
The isotopes of erbium range in atomic weight from 144.957 amu (Er-145) to 173.944 amu (Er-174). The primary decay mode before the most abundant stable isotope, Er-166, is electron capture, and the primary mode after is beta decay. The primary decay products before Er-166 are element 67 (holmium) isotopes, and the primary products after are element 69 (thulium) isotopes.
Precautions
As with the other lanthanides, erbium compounds are of low to moderate
toxicity, although their toxicity has not been investigated in detail.
See also
References
External links
Chemical elements | Lanthanides
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