Pyrrhotine

Pyrrhotite ('' pyrrhos'' in Greek meaning "flame-coloured"'')'' is an iron sulfide mineral with the formula Fe_(1−x)S (x = 0 to 0.125). It is a nonstoichiometric variant of FeS, the mineral known as troilite.
Pyrrhotite is also called magnetic pyrite, because the color is similar to pyrite and it is weakly magnetic. The magnetism decreases as the iron content increases, and troilite is non-magnetic. Pyrrhotite is generally tabular and brassy/bronze in color with a metallic luster. The mineral occurs with mafic igneous rocks like norites, and may form from pyrite during metamorphic processes. Pyrrhotite is associated and mined with other sulfide minerals like pentlandite, pyrite, chalcopyrite, and magnetite, and has been found globally.

Structure

Pyrrhotite exists as a number of polytypes of hexagonal or monoclinic crystal symmetry; several polytypes often occur within the same specimen. Their structure is based on the NiAs unit cell. As such, Fe occupies an octahedral site and the sulfide centers occupy trigonal prismatic sites.

Peter Atkins, Tina Overton, Jonathan Rourke, Mark Weller, Fraser Armstrong

Materials with the NiAs structure often are non-stoichiometric because they lack up to 1/8th fraction of the metal ions, creating vacancies. One of such structures is pyrrhotite-4C (Fe₇S₈). Here "4" indicates that iron vacancies define a superlattice that is 4 times larger than the unit cell in the "C" direction. The C direction is conventionally chosen parallel to the main symmetry axis of the crystal; this direction usually corresponds to the largest lattice spacing. Other polytypes include: pyrrhotite-5C (Fe₉S₁₀), 6C (Fe₁₁S₁₂), 7C (Fe₉S₁₀) and 11C (Fe₁₀S₁₁). Every polytype can have monoclinic (M) or hexagonal (H) symmetry, and therefore some sources label them, for example, not as 6C, but 6H or 6M depending on the symmetry.
The monoclinic forms are stable at temperatures below 254 °C, whereas the hexagonal forms are stable above that temperature. The exception is for those with high iron content, close to the troilite composition (47 to 50% atomic percent iron) which exhibit hexagonal symmetry.

Magnetic properties

The ideal FeS lattice, such as that of troilite, is non-magnetic. Magnetic properties vary with Fe content. More Fe-rich, hexagonal pyrrhotites are antiferromagnetic. However, the Fe-deficient, monoclinic Fe₇S₈ is ferrimagnetic. The ferromagnetism which is widely observed in pyrrhotite is therefore attributed to the presence of relatively large concentrations of iron vacancies (up to 20%) in the crystal structure. Vacancies lower the crystal symmetry. Therefore, monoclinic forms of pyrrhotite are in general more defect-rich than the more symmetrical hexagonal forms, and thus are more magnetic. Monoclinic pyrrhotite undergoes a magnetic transition known as the Besnus transition at 30 K that leads to a loss of magnetic remanence. The saturation magnetization of pyrrhotite is 0.12 tesla.

Identification

Physical properties

Pyrrhotite is brassy, bronze, or dark brown in color with a metallic luster and uneven or subconchoidal fracture. Pyrrhotite may be confused with other brassy sulfide minerals like pyrite, chalcopyrite, or pentlandite. Certain diagnostic characteristics can be used for identification in hand samples. Unlike other common brassy-colored sulfide minerals, pyrrhotite is typically magnetic (varies inversely with iron content). On the Mohs hardness scale, pyrrhotite ranges from 3.5 to 4, compared to 6 to 6.5 for pyrite. Streak can be used when properties between pyrrhotite and other sulfide minerals are similar. Pyrrhotite displays a dark grey to black streak. Pyrite will display a greenish black to brownish black streak, chalcopyrite will display a greenish black streak, and pentlandite leaves a pale bronze-brown streak. Pyrrhotite generally displays massive to granular crystal habit, and may show tabular/prismatic or hexagonal crystals which are sometimes iridescent.

Diagnostic characteristics in hand sample include: brassy/bronze color with a grey/black streak, tabular or hexagonal crystals which show iridescence, subconchoidal fracture, metallic luster, and magnetic.

Optical properties

Pyrrhotite is an opaque mineral and will therefore not transmit light. As a result, pyrrhotite will display extinction when viewed under plane polarized light and cross polarized light, making identification with petrographic polarizing light microscopes difficult. Pyrrhotite, and other opaque minerals can be identified optically using a reflected light ore microscope. The following optical propertiesSpry, P. G., & Gedlinske, B. (1987). ''Tables for the determination of common opaque minerals''. Economic Geology Pub. are representative of polished/puck sections using ore microscopy:

Pyrrhotite typically appears as anhedral, granular aggregates and is cream-pink to brownish in color. Weak to strong reflection pleochroism which may be seen along grain boundaries. Pyrrhotite has similar polishing hardness to pentlandite (medium), is softer than pyrite, and harder than chalcopyrite. Pyrrhotite will not display twinning or internal reflections, and its strong anisotropy from yellow to greenish-gray or grayish-blue is characteristic.

Diagnostic characteristics in polished section include: anhedral aggregates, cream-pink to brown in color and strong anisotropy.

Occurrence

Pyrrhotite is a rather common trace constituent of mafic igneous rocks especially norites. It occurs as segregation deposits in layered intrusions associated with pentlandite, chalcopyrite and other sulfides. It is an important constituent of the Sudbury intrusion (1.85 Ga old meteorite impact crater in Ontario, Canada) where it occurs in masses associated with copper and nickel mineralisation. It also occurs in pegmatites and in contact metamorphic zones. Pyrrhotite is often accompanied by pyrite, marcasite and magnetite.

Formation

Pyrrhotite requires both iron and sulfur to form. Iron is the fourth most abundant element in the Earth's continental crust (average abundance of 5.63 % or 56,300 mg/kg in the crust),"Abundance of Elements in the Earth’s Crust and in the Sea," in CRC Handbook of Chemistry and Physics, 103rd Edition (Internet Version 2022), John R. Rumble, ed., CRC Press/Taylor & Francis, Boca Raton, FL. and so the majority of rocks have sufficient iron abundance to form pyrrhotite. However, because sulfur is less abundant (average abundance of 0.035 % or 350 mg/kg in the crust), the formation of pyrrhotite is generally controlled by sulfur abundance. Also, the mineral pyrite is both the most common and most abundant sulfide mineral in the Earth's crust. If rocks containing pyrite undergo metamorphism, there is a gradual release of volatile components like water and sulfur from pyrite. The loss of sulfur causes pyrite to recrystallize into pyrrhotite.

Pyrite also decomposes into pyrrhotite in hot reductive technogenic environments, such as blast furnaces and direct coal liquefaction (in which it is an important catalyst).

Pyrrhotite can also form near black smoker hydrothermal vents. Black smokers release high sulfur concentrations onto the sea floor, and when the surrounding rocks are metamorphosed, pyrrhotite can crystallize. Later tectonic processes uplift the metamorphic rocks and expose pyrrhotite to the Earth's surface.

Distribution

United States

Pyrrhotite occurs in a variety of locations in the United States. In the eastern United States, pyrrhotite occurs in highly metamorphosed rock that forms a belt along the Appalachian Mountains. Pyrrhotite-bearing rocks are generally unseen in the central United States as the area is unmetamorphosed and underlain by sedimentary rocks which do not contain pyrrhotite. Discontinuous belts that contain pyrrhotite are present in the western United States along the Sierra Nevada mountain range and Cascade Range extending into the northwestern United States. Pyrrhotite may also be found west and south of Lake Superior.

Mining locations worldwide

The following are some of the locations worldwide where pyrrhotite has been reported during mining:

Canada

US

Australia

Brazil

Italy

Kosovo

Etymology and history

Named in 1847 by Ours-Pierre-Armand Petit-Dufrénoy. "Pyrrhotite" is derived from the Greek word πυρρός, "'' pyrrhos"'', meaning flame-colored.

Issues

If pyrrhotite-containing rocks are crushed and used as aggregate within concrete, then the pyrrhotite creates a problem in the production of concrete. Pyrrhotite has been linked to crumbling concrete basements in Quebec, Massachusetts and Connecticut when local quarries included it in their concrete mixtures. Many houses in Ireland, particularly in County Donegal, have also been affected by inclusion of rocks containing pyrrhotite in concrete blocks. The iron sulfide it contains can naturally react with oxygen and water, and over time pyrrhotite breaks down into sulfuric acid and secondary minerals like ettringite, thaumasite and gypsum. These secondary products occupy a larger volume than pyrrhotite, which expands and cracks the concrete leading to home foundation or block failure.

Uses

Other than a source of sulfur, pyrrhotite does not have specific applications.Haldar, S. K. (2017). ''Platinum-nickel-chromium deposits : geology, exploration and reserve base''. Elsevier. p.24. ISBN 978-0-12-802041-8. It is generally not a valuable mineral unless significant nickel, copper, or other metals are present.Kolahdoozan, M. & Yen, W.T.. (2002)
Pyrrhotite – An Important Gangue and a Source for Environmental Pollution
Green Processing 2002 – Proceedings: International Conference on the Sustainable Proceesing of Minerals. 245–249. Iron is seldom extracted from pyrrhotite due to a complicated metallurgical process It is mined primarily because it is associated with pentlandite, a sulfide mineral that can contain significant amounts of nickel and cobalt. When found in mafic and ultramafic rocks, pyrrhotite can be a good indicator of economic nickel deposits.

Mineral abbreviations

Synonyms

References

External links

* {{Cite EB1911 , last=Spencer , first=Leonard James , authorlink=Leonard James Spencer , wstitle=Pyrrhotite , short=x

Sulfide minerals
Iron minerals
Monoclinic minerals
Minerals in space group 15
Magnetic minerals