Nickel–Strunz classification

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Nickel–Strunz classification is a scheme for categorizing minerals based upon their chemical composition, introduced by German mineralogist Karl Hugo Strunz (24 February 1910 – 19 April 2006) in his Mineralogische Tabellen (1941). [1] The 4th and the 5th edition was also edited by Christel Tennyson (1966). It was followed by A.S. Povarennykh with a modified classification (1966 in Russian, 1972 in English).

Contents

As curator of the Mineralogical Museum of Friedrich-Wilhelms-Universität (now known as the Humboldt University of Berlin), Strunz had been tasked with sorting the museum's geological collection according to crystal-chemical properties. [1] His book Mineralogical Tables, has been through a number of modifications; the most recent edition, published in 2001, is the ninth (Mineralogical Tables by Hugo Strunz and Ernest H. Nickel (31 August 1925 – 18 July 2009)). [2] [3] James A. Ferraiolo was responsible for it at Mindat.org. [4] The IMA/CNMNC supports the Nickel–Strunz database. [5]

Classifications

Nickel–Strunz code scheme:NN.XY.##x
Nickel–Strunz mineral classes

The current scheme divides minerals into ten classes, which are further divided into divisions, families and groups according to chemical composition and crystal structure. [4]

  1. elements
  2. sulfides and sulfosalts
  3. halides
  4. oxides, hydroxides and arsenites
  5. carbonates and nitrates
  6. borates
  7. sulfates, chromates, molybdates and tungstates
  8. phosphates, arsenates and vanadates
  9. silicates
  10. organic compounds
IMA/CNMNC mineral classes

IMA/CNMNC proposes a new hierarchical scheme ( Mills et al. 2009 ), using the Nickel–Strunz classes (10 ed) this gives:

See also

Notes

  1. 1 2 Knobloch, Eberhard (2003). The shoulders on which We stand/Wegbereiter der Wissenschaft (in German and English). Springer. pp. 170–173. ISBN   3-540-20557-8.
  2. Mills et al. 2009.
  3. Allan Pring and William D. Birch (October 2009). "Obituary: Ernest Henry Nickel 1925–2009". Mineralogical Magazine. 73 (5): 891–892. doi:10.1017/S0026461X00032965 (inactive 24 August 2020).
  4. 1 2 Strunz Classification
  5. Ernest H. Nickel and Monte C. Nichols (22 May 2008). "IMA/CNMNC List of Mineral Name based on the database MINERAL, which Materials Data, Inc. (MDI) makes available" (PDF). Archived from the original (PDF) on 20 March 2009. Retrieved 31 January 2011.

Related Research Articles

Mineral Element or chemical compound that is normally crystalline, formed as a result of geological processes

In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid chemical compound with a fairly well-defined chemical composition and a specific crystal structure, that occurs naturally in pure form..

Sulfide mineral Nickel–Strunz 9 ed mineral class number 2

The sulfide minerals are a class of minerals containing sulfide (S2−) or persulfide (S22−) as the major anion. Some sulfide minerals are economically important as metal ores. The sulfide class also includes the selenides, the tellurides, the arsenides, the antimonides, the bismuthinides, the sulfarsenides and the sulfosalts. Sulfide minerals are inorganic compounds.

Borate mineral Nickel–Strunz 9 ed mineral class number 6

The borate minerals are minerals which contain a borate anion group. The borate (BO3) units may be polymerised similar to the SiO4 unit of the silicate mineral class. This results in B2O5, B3O6, B2O4 anions as well as more complex structures which include hydroxide or halogen anions. The [B(O,OH)4] anion exists as well.

Carbonate mineral Nickel–Strunz 9 ed mineral class number 5

Carbonate minerals are those minerals containing the carbonate ion, CO32−.

Sulfosalt mineral sulfosalt minerals, broad sense; after Moëlo, Y et al. (2008)

Sulfosalt minerals are those complex sulfide minerals with the general formula: AmBnSp; where A represents a metal such as copper, lead, silver, iron, and rarely mercury, zinc, vanadium; B usually represents semi-metal such as arsenic, antimony, bismuth, and rarely germanium, or metals like tin and rarely vanadium; and S is sulfur or rarely selenium or/and tellurium. The Strunz classification includes the sulfosalts in a sulfides and sulfosalts superclass. A group which have a similar appearing formulas are the sulfarsenides. In sulfarsenides the arsenic substitutes for sulfur whereas in the sulfosalts the arsenic substitutes for a metal cation.

Arsenate minerals usually refer to the naturally occurring orthoarsenates, possessing the (AsO4)3− anion group and, more rarely, other arsenates with anions like AsO3(OH)2− (also written HAsO42−) (example: pharmacolite Ca(AsO3OH).2H2O) or (very rarely) [AsO2(OH)2] (example: andyrobertsite). Arsenite minerals are much less common. Both the Dana and the Strunz mineral classifications place the arsenates in with the phosphate minerals.

Adelite arsenate mineral

The rare mineral adelite, is a calcium, magnesium, arsenate with chemical formula CaMgAsO4OH. It forms a solid solution series with the vanadium-bearing mineral gottlobite. Various transition metals substitute for magnesium and lead replaces calcium leading to a variety of similar minerals in the adelite - duftite group.

Oxide mineral Nickel–Strunz 9 ed mineral class number 4

The oxide mineral class includes those minerals in which the oxide anion (O2−) is bonded to one or more metal alloys. The hydroxide-bearing minerals are typically included in the oxide class. The minerals with complex anion groups such as the silicates, sulfates, carbonates and phosphates are classed separately.

Halide mineral Nickel–Strunz 9 ed mineral class number 3

Halide minerals are those minerals with a dominant halide anion. Complex halide minerals may also have polyatomic anions.

Arsenite minerals are very rare oxygen-bearing arsenic minerals. Classical world localities where such minerals occur include the complex skarn manganese deposit at Långban (Sweden) and the polymetallic Tsumeb deposit (Namibia). The most often reported arsenite anion in minerals is the AsO33− anion, present for example in reinerite Zn3(AsO3)2. Unique diarsenite anions occur i. e. in leiteite Zn[As2O4] and paulmooreite Pb[As2O5]. More complex arsenites include schneiderhöhnite Fe2+Fe3+3[As5O13] and ludlockite PbFe3+4As10O22.

Sulfate mineral Nickel–Strunz 9 ed mineral class number 7 (isolated tetrahedral units, mainly)

The sulfate minerals are a class of minerals that include the sulfate ion (SO42−) within their structure. The sulfate minerals occur commonly in primary evaporite depositional environments, as gangue minerals in hydrothermal veins and as secondary minerals in the oxidizing zone of sulfide mineral deposits. The chromate and manganate minerals have a similar structure and are often included with the sulfates in mineral classification systems.

Native element mineral Nickel–Strunz 9 ed mineral class number 1

Native element minerals are those elements that occur in nature in uncombined form with a distinct mineral structure. The elemental class includes metals and intermetallic elements, naturally occurring alloys, semi-metals and non-metals. The Nickel–Strunz classification system also includes the naturally occurring phosphides, silicides, nitrides and carbides and arsenides.

Georgius Agricola is considered the 'father of mineralogy'. Nicolas Steno founded the stratigraphy, the geology characterizes the rocks in each layer and the mineralogy characterizes the minerals in each rock. The chemical elements were discovered in identified minerals and with the help of the identified elements the mineral crystal structure could be described. One milestone was the discovery of the geometrical law of crystallization by René Just Haüy, a further development of the work by Nicolas Steno and Jean-Baptiste L. Romé de l'Isle. Important contributions came from some Saxon "Bergraths"/ Freiberg Mining Academy: Johann F. Henckel, Abraham Gottlob Werner and his students. Other milestones were the notion that metals are elements too and the periodic table of the elements by Dmitri Ivanovich Mendeleev. The overview of the organic bonds by Kekulé was necessary to understand the silicates, first refinements described by Bragg and Machatschki; and it was only possibly to understand a crystal structure with Dalton's atomic theory, the notion of atomic orbital and Goldschmidt's explanations. Specific gravity, streak and X-ray powder diffraction are quite specific for a Nickel-Strunz identifier. Nowadays, non-destructive electron microprobe analysis is used to get the empirical formula of a mineral. Finally, the International Zeolite Association (IZA) took care of the zeolite frameworks.

Letovicite sulfate mineral

Letovicite is an ammonium sulfate mineral with composition (NH4)3H(SO4)2 (IUPAC: triammonium sulfate hydrogensulfate, Nickel–Strunz classification 07.AD.20).

References