Wakefieldite
| Wakefieldite | |
|---|---|
_,_Hausmannite_-_Grube_Gl%C3%BCcksstern,_Gottlob,_Th%C3%BCringen.jpg) Wakefieldite-(La) on hausmannite | |
| General | |
| Category | Rare earth mineral |
| Formula (repeating unit) | ((La,Ce,Nd,Y)VO4) |
| Strunz classification | 08.AD.35 |
| Crystal system | Tetragonal |
| Space group | Tetragonal ditetragonal dipyramidal H-M symbol: (4/m 2/m 2/m) Space group: I 41/amd |
| Identification | |
| Color | Canary-yellow, pale tan (Wakefieldite-(Y)); Dark red to coal-black, pale yellow to bluish gray (Wakefieldite-(Ce)); Light pink, brown (Wakefieldite-(La) |
| Crystal habit | Prismatic crystals, pulverulent masses |
| Cleavage | Good on {100} |
| Tenacity | Very brittle |
| Mohs scale hardness | 4-5 |
| Diaphaneity | Translucent to opaque |
| Specific gravity | 4.25 (calculated Wakefieldite-(Y)); 4.74 (meas. Wakefieldite-(Ce) |
| Optical properties | Uniaxial (+) |
| Refractive index | nω = 2.000 nε = 2.140 |
Wakefieldite ((La,Ce,Nd,Y)VO4) is an uncommon rare earth element vanadate mineral. There are four main types of wakefieldite- wakefieldite-(La), wakefieldite-(Ce), wakefieldite-(Nd), and wakefieldite-(Y), depending upon the dominant rare earth metal ion present. Wakefieldite has a Mohs hardness ranging from 4-5.[1] Wakefieldite forms crystals of tetragonal structure. In terms of crystal structure, it is the vanadate analog of the rare earth phosphate mineral xenotime. Unlike xenotime, it is more favorable for wakefieldite to contain the lighter rare earth elements over the heavier ones. Due to the lanthanide contraction, the heavier rare earths have smaller ionic radii than the lighter ones. When the phosphate anion is replaced by the larger vanadate anion, the tetragonal crystal system preferentially accommodates the larger light rare earth elements.[2]
Wakefieldite was first described for an occurrence in the Evans Lou mine, St. Pierre de Wakefield, Quebec, Canada[3] and later designated Wakefieldite-(Y).[4]
Wakefieldite-(Ce) was first described as kusuite for its type locality in the Kusu deposit, 85 km SW of Kinshasa, Zaire. It was renamed in 1977 as the Ce analog of wakefieldite-Y.[5]
Wakefieldite-(La) was first described in 2008 for an occurrence in the Glücksstern mine, Gottlob Hill, Friedrichroda, Thuringia, Germany.[6]
Wakefieldite-(Nd) was first described in 2008 at the Arase mine, Kami city, Kochi Prefecture, Shikoku Island, Japan.[7][8]
References
- ^ The Mineral and Locality Database, Wakefieldite-(La).
- ^ Miyawaki R., and I. Nakai. (1996). "Crystal Chemical Aspects of Rare Earth Minerals." Ed. Andrian P. Jones, Frances Wall, and C. Terry Williams. Rare Earth Minerals: Chemistry, Origin and Ore Deposits. London: Chapman & Hall. (p 29-30).
- ^ Miles, Norman M., et al., Wakefieldite, Yttrium Vanadate, a New Mineral From Quebec, American Mineralogist, Vol 56, Mar.-Apr. 1971 http://www.minsocam.org/ammin/AM56/AM56_395.pdf
- ^ http://www.mindat.org/min-4234.html Mindat, Wakefieldite-(Y)
- ^ http://rruff.geo.arizona.edu/doclib/hom/wakefielditece.pdf Handbook of Mineralogy, Wakefieldite-(Ce)
- ^ http://www.webmineral.com/data/Wakefieldite-(La).shtml Webmineral data, Wakefieldite-(La)
- ^ http://www.mindat.org/min-38894.html Wakefieldite-(Nd)
- ^ Discovery of wakefieldite-(Nd), a new rare earth mineral, Moriyama,T., et al., http://unit.aist.go.jp/georesenv/english/result-e/ten-big-news/2008/2008-1-2.pdf