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Magnetite

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Magnetite
Magnetite exposed on the ground. The mineral is black and irregularly smooth. Individual chunks jut at angles characteristic of the crystal habit.
Magnetite and pyrite from Piedmont, Italy
General
CategoryOxide minerals
Spinel group
Spinel structural group
Formula
(repeating unit)		iron(II,III) oxide, Fe2+Fe3+2O4
Strunz classification04.BB.05
Crystal systemIsometric Hexoctahedral
Space groupIsometric 4/m 3 2/m
Unit cella = 8.397 Å; Z=8
Identification
ColorBlack, gray with brownish tint in reflected sun
Crystal habitOctahedral, fine granular to massive
TwinningOn {Ill} as both twin and composition plane, the spinel law, as contact twins
CleavageIndistinct, parting on {Ill}, very good
FractureUneven
TenacityBrittle
Mohs scale hardness5.5–6.5
LusterMetallic
StreakBlack
DiaphaneityOpaque
Specific gravity5.17–5.18
SolubilityDissolves slowly in hydrochloric acid
References[1][2][3][4]
Major varieties
LodestoneMagnetic with definite north and south poles

Magnetite is a mineral, one of the three common naturally occurring iron oxides (chemical formula Fe3O4) and a member of the spinel group. Magnetite is the most magnetic of all the naturally occurring minerals on Earth.[5] Naturally magnetized pieces of magnetite, called lodestone, will attract small pieces of iron, and this was how ancient people first noticed the property of magnetism.

Small grains of magnetite occur in almost all igneous and metamorphic rocks. Magnetite is black or brownish-black with a metallic luster, has a Mohs hardness of 5–6 and a black streak.

The chemical IUPAC name is iron(II,III) oxide and the common chemical name is ferrous-ferric oxide.

Properties

Lodestones were used as an early form of magnetic compass. Magnetite typically carries the dominant magnetic signature in rocks, and so it has been a critical tool in paleomagnetism, a science important in understanding plate tectonics and as historic data for magnetohydrodynamics and other scientific fields. The relationships between magnetite and other iron-rich oxide minerals such as ilmenite, hematite, and ulvospinel have been much studied; the reactions between these minerals and oxygen influence how and when magnetite preserves a record of the Earth's magnetic field.

Magnetite has been very important in understanding the conditions under which rocks form. Magnetite reacts with oxygen to produce hematite, and the mineral pair forms a buffer that can control oxygen fugacity. Commonly, igneous rocks contain grains of two solid solutions, one of magnetite and ulvospinel and the other of ilmenite and hematite. Compositions of the mineral pairs are used to calculate how oxidizing was the magma (i.e., the oxygen fugacity of the magma): a range of oxidizing conditions are found in magmas and the oxidation state helps to determine how the magmas might evolve by fractional crystallization.

Magnetite also occurs in many sedimentary rocks, including banded iron formations. In many igneous rocks, magnetite-rich and ilmenite-rich grains occur that precipitated together in magma. Magnetite also is produced from peridotites and dunites by serpentinization.

The Curie temperature of magnetite is 858 K (585 °C; 1,085 °F).

Distribution of deposits

A fine textured sample, ~5cm across
Magnetite and other heavy minerals (dark) in a quartz beach sand (Chennai, India).

Magnetite is sometimes found in large quantities in beach sand. Such black sands (mineral sands or iron sands) are found in various places, such as California and the west coast of the North Island of New Zealand.[6] The magnetite is carried to the beach via rivers from erosion and is concentrated via wave action and currents.

Huge deposits have been found in banded iron formations. These sedimentary rocks have been used to infer changes in the oxygen content of the atmosphere of the Earth.

Large deposits of magnetite are also found in the Atacama region of Chile, Valentines region of Uruguay, Kiruna, Sweden, the Pilbara, Midwest and Northern Goldfields regions in Western Australia, New South Wales in the Tallawang Region, and in the Adirondack region of New York in the United States. Kediet ej Jill, the highest mountain of Mauritania, is made entirely of the mineral.[7] Deposits are also found in Norway, Germany, Italy, Switzerland, South Africa, India, Indonesia, Mexico, and in Oregon, New Jersey, Pennsylvania, North Carolina, West Virginia, Virginia, New Mexico, Utah, and Colorado in the United States. In 2005, an exploration company, Cardero Resources, discovered a vast deposit of magnetite-bearing sand dunes in Peru. The dune field covers 250 square kilometers (100 sq mi), with the highest dune at over 2,000 meters (6,560 ft) above the desert floor. The sand contains 10% magnetite.[8]

Biological occurrences

Biomagnetism is usually related to the presence of biogenic crystals of magnetite, which occur widely in organisms.[9] These organisms range from bacteria (e.g., Magnetospirillum magnetotacticum) to animals, where these crystals are found in the brain, including those of humans.[10] Biomagnetites account for the effects of weak magnetic fields on biological systems.[11] It has been proposed the magnetite in the brain contributes to long-term memory.[12]

Magnetite crystals are involved in magnetoreception in several species,[13] the ability to sense the polarity, field lines [14] or the inclination [15] of the Earth's magnetic field, as an aid in navigation, and there is some evidence that it also exists in humans. [16]

Chitons have teeth made of magnetite on their denticles.[17]

Applications

Magnetic recording

Audio recording using magnetic acetate tape was developed in the 1930s. The German magnetophon utilized magnetite powder as the recording medium.[18] Following World War II the 3M company continued work on the German design. In 1946 the 3M researchers found they could improve the magnetite based tape, which utilized powders of cubic crystals, by replacing the magnetite with needle shaped particles of gamma ferric oxide (γ-Fe2O3).[18]

Catalysis

Magnetite is the catalyst for the industrial synthesis of ammonia.[19]

Arsenic sorbent

Magnetite powder efficiently removes arsenic(III) and arsenic(V) from water, the efficiency of which increases ~200 times when the magnetite particle size decreases from 300 to 12 nm.[20] Arsenic-contaminated drinking water is a major problem around the world, which can be solved using magnetite as a sorbent.

Other

Because of its stability at high temperatures, it is used for coating industrial watertube steam boilers. The magnetite layer is formed after a chemical treatment (e.g. by using hydrazine).

Iron-metabolizing bacteria can trigger redox reactions in microscopic magnetite particles. Using light, magnetite can reduce chromium (VI) (its toxic form), converting it to less toxic chromium (III), which can then be incorporated into a harmless magnetite crystal. Phototrophic Rhodopseudomonas palustris oxidized the magnetite, while Geobacter sulfurreducens reduced it, readying it for another cycle.[21]

  • Octahedral crystals of magnetite up to 1.8 cm across, on cream colored feldspar crystals, locality: Cerro Huañaquino, Potosí Department, Bolivia (size: 8.4 x 5.2 x 3.2 cm)
    Octahedral crystals of magnetite up to 1.8 cm across, on cream colored feldspar crystals, locality: Cerro Huañaquino, Potosí Department, Bolivia (size: 8.4 x 5.2 x 3.2 cm)
  • Red gem-like crystals of chondrodite with magnetite, Tilly Foster mine, Brewster, New York (size 2.8 x 2.6 x 2.1 cm)
    Red gem-like crystals of chondrodite with magnetite, Tilly Foster mine, Brewster, New York (size 2.8 x 2.6 x 2.1 cm)
  • Metallic, jet black, complex cubes of magnetite, from the Balmat-Edwards district, St. Lawrence County, New York (field of view, about 4 cm)
    Metallic, jet black, complex cubes of magnetite, from the Balmat-Edwards district, St. Lawrence County, New York (field of view, about 4 cm)

See also

References

  1. ^ Handbook of Mineralogy
  2. ^ Mindat.org Mindat.org
  3. ^ Webmineral data
  4. ^ Hurlbut, Cornelius S.; Klein, Cornelis (1985). Manual of Mineralogy (20th ed.). Wiley. ISBN 0-471-80580-7.
  5. ^ Harrison, R. J.; Dunin-Borkowski, RE; Putnis, A (2002). "Direct imaging of nanoscale magnetic interactions in minerals" (free-download pdf). Proceedings of the National Academy of Sciences. 99 (26): 16556–16561. Bibcode:2002PNAS...9916556H. doi:10.1073/pnas.262514499. PMC 139182. PMID 12482930.
  6. ^ Templeton, Fleur. "1. Iron – an abundant resource - Iron and steel". Te Ara Encyclopedia of New Zealand. Retrieved 4 January 2013.
  7. ^ Kediet ej Jill
  8. ^ Ferrous Nonsnotus
  9. ^ Kirschvink, J L; Walker, M M; Diebel, C E (2001). "Magnetite-based magnetoreception". Current opinion in neurobiology. 11 (4): 462–7. PMID 11502393.
  10. ^ Kirschvink, Joseph; et al. (1992). "Magnetite biomineralization in the human brain". Proceedings of the National Academy of Sciences of the USA. 89 (16): 7683–7687. {{cite journal}}: Explicit use of et al. in: |last2= (help); Unknown parameter |laysource= ignored (help); Unknown parameter |laysummary= ignored (help)
  11. ^ Kirschvink, J L; Kobayashi-Kirschvink, A; Diaz-Ricci, J C; Kirschvink, S J (1992). "Magnetite in human tissues: a mechanism for the biological effects of weak ELF magnetic fields". Bioelectromagnetics. Suppl 1: 101–13. PMID 1285705. A simple calculation shows that magnetosomes moving in response to earth-strength ELF fields are capable of opening trans-membrane ion channels, in a fashion similar to those predicted by ionic resonance models. Hence, the presence of trace levels of biogenic magnetite in virtually all human tissues examined suggests that similar biophysical processes may explain a variety of weak field ELF bioeffects. {{cite journal}}: Unknown parameter |laysummary= ignored (help)
  12. ^ Banaclocha, Marcos Arturo Martínez; Bókkon, István; Banaclocha, Helios Martínez (2010). "Long-term memory in brain magnetite". Medical hypotheses. 74 (2): 254–7. doi:10.1016/j.mehy.2009.09.024. PMID 19815351.
  13. ^ Kishkinev, D A; Chernetsov, N S (2014). "[Magnetoreception systems in birds: a review of current research]". Zhurnal obshcheĭ biologii. 75 (2): 104–23. There are good reasons to believe that this visual magnetoreceptor processes compass magnetic information which is necessary for migratory orientation. {{cite journal}}: Unknown parameter |laysummary= ignored (help)
  14. ^ Wiltschko, Roswitha; Wiltschko, Wolfgang (2014). "Sensing magnetic directions in birds: radical pair processes involving cryptochrome". Biosensors. 4 (3): 221–42. doi:10.3390/bios4030221. Birds can use the geomagnetic field for compass orientation. Behavioral experiments, mostly with migrating passerines, revealed three characteristics of the avian magnetic compass: (1) it works spontaneously only in a narrow functional window around the intensity of the ambient magnetic field, but can adapt to other intensities, (2) it is an "inclination compass", not based on the polarity of the magnetic field, but the axial course of the field lines, and (3) it requires short-wavelength light from UV to 565 nm Green. {{cite journal}}: Unknown parameter |laysummary= ignored (help)CS1 maint: unflagged free DOI (link)
  15. ^ Wiltschko, Roswitha; Stapput, Katrin; Thalau, Peter; Wiltschko, Wolfgang (2010). "Directional orientation of birds by the magnetic field under different light conditions". Journal of the Royal Society, Interface / the Royal Society. 7 (Suppl 2): S163–77. doi:10.1098/rsif.2009.0367.focus. PMID 19864263. {{cite journal}}: Unknown parameter |laysource= ignored (help); Unknown parameter |laysummary= ignored (help)
  16. ^ Baker, R R (1988). "Human magnetoreception for navigation". Progress in clinical and biological research. 257: 63–80. PMID 3344279.
  17. ^ Lowenstam, H A (1967). "Lepidocrocite, an apatite mineral, and magnetic in teeth of chitons (Polyplacophora)". Science. 156 (3780): 1373–1375. PMID 5610118. X-ray diffraction patterns show that the mature denticles of three extant chiton species are composed of the mineral lepidocrocite and an apatite mineral, probably francolite, in addition to magnetite.
  18. ^ a b Schoenherr, Steven, 2002, The History of Magnetic Recording, Audio Engineering Society
  19. ^ Max Appl "Ammonia, 2. Production Processes" in Ullmann's Encyclopedia of Industrial Chemistry 2011, Wiley-VCH. doi:10.1002/14356007.o02_o11
  20. ^ Mayo, J.T.; et al. (2007). "The effect of nanocrystalline magnetite size on arsenic removal". Sci. Technol. Adv. Mater. 8: 71–75. Bibcode:2007STAdM...8...71M. doi:10.1016/j.stam.2006.10.005.
  21. ^ "How bacteria can use magnetic particles to create a 'natural battery'". KurzweilAI. March 30, 2015. Retrieved April 2015. {{cite news}}: Check date values in: |accessdate= (help)

Further reading


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