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Rare Earth Elements: A Review of Production, Processing ...

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<strong>Rare</strong> <strong>Earth</strong> <strong>Elements</strong> <strong>Review</strong> Section 2 – Introduction to <strong>Rare</strong> <strong>Earth</strong> <strong>Elements</strong><br />

2. Introduction to <strong>Rare</strong> <strong>Earth</strong> <strong>Elements</strong><br />

For the purposes <strong>of</strong> this report, the series <strong>of</strong> 15 lanthanide metals, plus scandium and yttrium, have been<br />

designated as REEs; however, it should be noted that other elements also are sometimes referred to as REEs.<br />

<strong>Rare</strong> earth oxides (REOs), and rare earth metals (REMs). While these elements are widely dispersed and<br />

generally common in nature, minable concentrations <strong>of</strong> REEs are less common than for most other metal ores.<br />

<strong>Rare</strong> earths have become important in modern commercial and industrial processing and products. Metallurgical<br />

processing, alloying, and electronics applications (e.g., cell phones, computer components, electric motors,<br />

specialty glass and lenses) represent the most significant uses <strong>of</strong> REEs. In addition, due to the dependence on<br />

several <strong>of</strong> these elements for military applications, REEs are considered a national strategic resource. Analysis <strong>of</strong><br />

the future supply and demand for each <strong>of</strong> the REEs indicates that, by 2014, global demand could exceed 200,000<br />

tons per year, which would exceed current production by over 75,000 tons per year. It is reported that if the new<br />

mines under development are able to meet their projected production levels, world-wide demand for REEs will be<br />

met from these new sources.<br />

The International Union <strong>of</strong> Pure and Applied Chemistry, an organization devoted to maintaining<br />

international consistency for chemical nomenclature, has identified the15 transition metals from the<br />

periodic table <strong>of</strong> the elements with atomic numbers 57 (lanthanum) through 71 (lutetium) as lanthanides<br />

or lanthanoids. These 15 elements share common physiochemical properties and are listed below:<br />

� Lanthanum (57La) � Samarium (62Sm) � Holmium (67Ho)<br />

� Cerium (58Ce) � Europium (63Eu) � Erbium (68Er)<br />

� Praseodymium (59Pr) � Gadolinium (64Gd) � Thulium (69Tm)<br />

� Neodymium (60Nd) � Terbium (65Tb) � Ytterbium (70Yb)<br />

� Promethium (61Pm) � Dysprosium (66Dy) � Lutetium (71Lu).<br />

Due to their similar physiochemistry, these lanthanides <strong>of</strong>ten occur together as elemental constituents <strong>of</strong><br />

their host minerals. Two other metals commonly found in association with lanthanides in the same<br />

mineral assemblages are the following:<br />

� Scandium (21Sc)<br />

� Yttrium (39Y).<br />

These two metals also have physiochemical characteristics that are very similar to the lanthanides.<br />

2.1 Abundance <strong>of</strong> REEs in <strong>Earth</strong>’s Crust<br />

Together, the lanthanides, yttrium, and scandium are commonly referred to as REEs or REMs, although<br />

this is a misnomer since most <strong>of</strong> the REEs are common mineral constituents as compared with other metal<br />

elements. The term “rare” is a carryover from metallurgical chemists from around the 1940s (Gupta and<br />

Krishnamurthy, 2004). The metallurgical processes needed to isolate the individual metal species are<br />

complex, and early technology prevented commodity-level production. As a result, lanthanide metals or<br />

metal oxides (i.e., REOs) were difficult to obtain and thus are considered rare. The abundance <strong>of</strong> REEs in<br />

the earth’s crust relative to other common metals is presented in Table 2-1; these abundances from<br />

Wedephol (1995) are only one <strong>of</strong> several interpretations, but those presented here are generally<br />

representative. As shown in the comparison, the content <strong>of</strong> lanthanides relative to other REEs in rockforming<br />

minerals is not rare at all.<br />

2-1

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