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Neodymium, a rare earth metal, is present in Misch metal to the extent of about 18%. The metal has a bright, silvery metallic luster, however, as one of the more reactive rare earth metals, it quickly tarnishes in air. The tarnishing forms an oxide layer that falls off, which exposes the metal to further oxidation. Although it belongs to "rare earth metals," neodymium is not rare at all. It constitutes 38 ppm of Earth’s crust.
Neodymium glass (Nd:Glass) is produced by the inclusion of neodymium oxide (Nd2O3) in the glass melt. In daylight or incandescent light neodymium glass appears lavender, but it appears pale blue under fluorescent lighting.
Neodymium glass solid-state lasers are used in extremely high power (terawatt scale), high energy (megajoules) multiple beam systems for inertial confinement fusion. Nd:Glass lasers are usually frequency tripled to the third harmonic at 351 nm in laser fusion devices.
Neodymium glass is becoming widely used in incandescent light bulbs, to provide a more "natural" light.
Neodymium glass has been patented for use in automobile rear-view mirrors, to reduce the glare at night.
The first commercial use of purified neodymium was in glass coloration, starting with experiments by Leo Moser in November 1927. The resulting "Alexandrite" glass remains a signature color of the Moser glassworks to this day. Neodymium glass was widely emulated in the early 1930's by American glasshouses, most notably Heisey, Fostoria ("wisteria"), Cambridge ("heatherbloom"), and Steuben ("wisteria"), and elsewhere (e.g. Lalique, in France, or Murano). Tiffin's "twilight" remained in production from about 1950 to about 1980. Current sources include glassmakers in the Czech Republic, the USA, and China; Caithness Glass in Scotland has also used the colorant extensively. The sharp absorption bands of neodymium cause the glass color to change under different lighting conditions, being reddish-purple under daylight or yellow incandescent light, but blue under white fluorescent lighting, or greenish under trichromatic lighting. This color-change phenomenon is highly prized by collectors. Neodymium in combination with praseodymium gave Moser's "Heliolite" glass. In combination with gold or selenium, beautiful red colors result, such as Moser's "Royalite" or Tiffin's "Wistaria" or some of the colors achieved by Fenton. Since neodymium coloration depends upon "forbidden" f-f transitions deep within the atom, there is relatively little influence on the color from the chemical environment, so the color is impervious to the thermal history of the glass. However, for the best color, iron-containing impurities need to be minimized in the silica used to make the glass. The same "forbiddenness" of the f-f transitions makes rare earth colorants less intense than those provided by most d-transition elements, so more has to be used in a glass to achieve the desired color intensity. The original Moser recipe used about 5% of neodymium oxide in the glass melt, a sufficient quantity such that Moser referred to these as being "Rare Earth Doped" glasses. Being a strong base, that level of neodymium would have affected the melting properties of the glass, and the lime content of the glass might have had to be adjusted accordingly.
Neodymium was discovered by Baron Carl Auer von Welsbach, an Austrian chemist, in Vienna in 1885. He separated neodymium, as well as the element praseodymium, from a material known as didymium by means of fractional crystallization of the double ammonium nitrate tetrahydrates from nitric acid, while following the separation by spectroscopic analysis; however, it was not isolated in relatively pure form until 1925. The name neodymium is derived from the Greek words neos, new, and didymos, twin. Neodymium is frequently misspelled as neodynium.
Double nitrate crystallization was the means of commercial neodymium purification until the 1950's. The Lindsay Chemical Division of American Potash and Chemical Corporation, at one time the largest producer of rare earths in the world, offered neodymium oxide purified in this manner in grades of 65%, 85% and 95% purity, at prices ranging from approximately 2 to 20 dollars per pound (in 1960 dollars). Lindsay was the first to commercialize large-scale ion-exchange purification of neodymium, using the technology developed by Frank Spedding at Iowa State University/Ames Laboratory; one pound of their 99% oxide was priced at $35 in 1960; their 99.9% grade only cost 5 dollars more. Starting in the 1950's, high purity (e.g. 99+%) neodymium was primarily obtained through an ion exchange process from monazite sand ((Ce,La,Th,Nd,Y)PO4), a material rich in rare earth elements. The metal itself is obtained through electrolysis of its halide salts. Currently, most neodymium is extracted from bastnaesite, (Ce,La,Nd,Pr)CO3F, and purified by solvent extraction. Ion-exchange purification is reserved for preparing the highest purities (typically >4N). (When Molycorp first introduced their 98% grade of neodymium oxide in 1965, made by solvent extraction from Mountain Pass California bastnaesite, it was priced at 5 dollars per pound, for small quantities. Lindsay soon discontinued operations.) The evolving technology, and improved purity of commercially available neodymium oxide was reflected in the appearance of neodymium glass made therefrom, that resides in collections today. Early Moser pieces, and other neodymium glass made in the 1930's, have a more reddish or orange tinge than modern versions, which are more cleanly purple, due to the difficulties in removing the last traces of praseodymium, when the fractional crystallization technology had to be relied on.
Neodymium is never found in nature as the free element; rather, it occurs in ores such as monazite sand ((Ce,La,Th,Nd,Y)PO4) and bastnäsite ((Ce,La,Th,Nd,Y)(CO3)F) that contain small amounts of all the rare earth metals. Neodymium can also be found in Misch metal; it is difficult to separate it from other rare earth elements.
Neodymium compounds include
Naturally occurring Neodymium is composed of 5 stable isotopes, 142Nd, 143Nd, 145Nd, 146Nd and 148Nd, with 142Nd being the most abundant (27.2% natural abundance), and 2 radioisotopes, 144Nd and 150Nd. In all, 31 radioisotopes of Neodymium have been characterized up to now, with the most stable being naturally occurring isotopes 144Nd (alpha decay, a half-life (T½) of 2.29×1015 years) and 150Nd (double beta decay, T½ of 7×1018 years). All of the remaining radioactive isotopes have half-lives that are less than 11 days, and the majority of these have half-lives that are less than 70 seconds. This element also has 13 known meta states with the most stable being 139mNd (T½ 5.5 hours), 135mNd (T½ 5.5 minutes) and 133m1Nd (T½ ~70 seconds).
The primary decay modes before the most abundant stable isotope, 142Nd, are electron capture and positron decay, and the primary mode after is beta minus decay. The primary decay products before 142Nd are element Pr (praseodymium) isotopes and the primary products after are element Pm (promethium) isotopes.
Neodymium metal dust is a combustion and explosion hazard.
Neodymium compounds, like all rare earth metals, are of low to moderate toxicity; however its toxicity has not been thoroughly investigated. Neodymium dust and salts are very irritating to the eyes and mucous membranes, and moderately irritating to skin. Breathing the dust can cause lung embolisms, and accumulated exposure damages the liver. Neodymium also acts as an anticoagulant, especially when given intravenously.
Neodymium magnets have been tested for medical uses such as magnetic braces and bone repair, but biocompatibility issues have prevented widespread application.
Neodymium magnet (NIB or Nd2Fe14B)
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Neodymium". A list of authors is available in Wikipedia.|