Abstract is: The lanthanide (/ˈlænθənaɪd/) or lanthanoid (/ˈlænθənɔɪd/) series of chemical elements comprises the 15 metallic chemical elements with atomic numbers 57–71, from lanthanum through lutetium. These elements, along with the chemically similar elements scandium and yttrium, are often collectively known as the rare-earth elements or rare-earth metals. The informal chemical symbol Ln is used in general discussions of lanthanide chemistry to refer to any lanthanide. All but one of the lanthanides are f-block elements, corresponding to the filling of the 4f electron shell. There is some dispute on whether lanthanum or lutetium is a d-block element, but lutetium is usually considered so by those who study the matter; it is included due to its chemical similarities with the other 14. All lanthanide elements form trivalent cations, Ln3+, whose chemistry is largely determined by the ionic radius, which decreases steadily from lanthanum to lutetium. These elements are called lanthanides because the elements in the series are chemically similar to lanthanum. Since "lanthanide" means "like lanthanum", it has been argued that lanthanum cannot logically be a lanthanide, but the International Union of Pure and Applied Chemistry (IUPAC) acknowledges its inclusion based on common usage. In presentations of the periodic table, the f-block elements are customarily shown as two additional rows below the main body of the table. This convention is entirely a matter of aesthetics and formatting practicality; a rarely used wide-formatted periodic table inserts the 4f and 5f series in their proper places, as parts of the table's sixth and seventh rows (periods). The 1985 IUPAC "Red Book" (p. 45) recommends using "lanthanoid" instead of "lanthanide", as the ending "-ide" normally indicates a negative ion. However, owing to wide current use, "lanthanide" is still allowed. * v * t * eLanthanides Primordial From decay Synthetic Border shows natural occurrence of the element
Abstract is: The rare-earth elements (REE), also called the rare-earth metals or (in context) rare-earth oxides or sometimes the lanthanides (yttrium and scandium are usually included as rare earths), are a set of 17 nearly-indistinguishable lustrous silvery-white soft heavy metals. Compounds containing rare earths have diverse applications in electrical and electronic components, lasers, glass, magnetic materials, and industrial processes. Scandium and yttrium are considered rare-earth elements because they tend to occur in the same ore deposits as the lanthanides and exhibit similar chemical properties, but have different electronic and magnetic properties. These metals tarnish slowly in air at room temperature and react slowly with cold water to form hydroxides, liberating hydrogen. They react with steam to form oxides, and at elevated temperature (400°C) ignite spontaneously. These elements and their compounds have no biological function other than in several specialized enzymes, such as in lanthanide-dependent methanol dehydrogenases in bacteria. The water-soluble compounds are mildly to moderately toxic, but the insoluble ones are not. Despite their name, rare-earth elements are relatively plentiful in Earth's crust, with cerium being the 25th most abundant element at 68 parts per million, more abundant than copper. All isotopes of promethium are radioactive, and it does not occur naturally in the earth's crust, except for a trace amount generated by spontaneous fission of Uranium-238. They are often found in minerals with thorium, and less commonly uranium. Because of their geochemical properties, rare-earth elements are typically dispersed and not often found concentrated in rare-earth minerals. Consequently, economically exploitable ore deposits are sparse (i.e. "rare"). The first rare-earth mineral discovered (1787) was gadolinite, a black mineral composed of cerium, yttrium, iron, silicon, and other elements. This mineral was extracted from a mine in the village of Ytterby in Sweden; four of the rare-earth elements bear names derived from this single location.
rare earth element | Q190444 |
period 6 | Q239813 |
lithophile | Q1130479 |
P1343 | described by source | Armenian Soviet Encyclopedia, vol. 4 | Q124737630 |
P246 | element symbol | Ln | |
P527 | has part(s) | cerium | Q1385 |
praseodymium | Q1386 | ||
neodymium | Q1388 | ||
europium | Q1396 | ||
promethium | Q1809 | ||
terbium | Q1838 | ||
gadolinium | Q1832 | ||
dysprosium | Q1843 | ||
holmium | Q1846 | ||
ytterbium | Q1855 | ||
samarium | Q1819 | ||
lutetium | Q1857 | ||
erbium | Q1849 | ||
thulium | Q1853 | ||
P138 | named after | lanthanum | Q1801 |
P5008 | on focus list of Wikimedia project | Wikipedia:Vital articles/Level/4 | Q6173448 |
P910 | topic's main category | Category:Lanthanides | Q6657575 |