
[German Pyrolusit : Greek puro-, pyro- + Greek lousis, a washing (from louein, to wash).]
A mineral having composition MnO2. Well-developed crystals (polianite) arerare; it is usually in radiating fibers or reniform coatings. The hardness is 1–2 on the Mohs scale (often soiling the fingers) and the specific gravity is 4.75. The luster is metallicand the color iron-black. It frequently forms pseudomorphs after other manganese minerals, notably manganite.
Pyrolusite is extensively mined as a manganese ore in many countries, chiefly in Russia, Ghana, India, the Republic of South Africa, Morocco, Brazil, and Cuba. See also Manganese; Manganite.
Environment
Secondary manganese deposits and secondary veins.
Crystal descriptionRarely in prismatic or stubby well-formed crystals. Sometimes in fibrous crystals and usually in fibrous masses that are pseudomorphous after other manganese oxides. Also massive, fibrous; and as black powdery to granular masses.
Physical propertiesSteel gray to iron black. Luster metallic; hardness 6-6Ɖ (for crystals) to as little as 2 (for massive material), specific gravity 4.4-5.0; streak black (soft material blackens the fingers); fracture uneven; cleavage prismatic. Brittle.
CompositionManganese dioxide (63.2% Mn, 36.8% O), often with a small amount of water, heavy metals, phosphorus, and other elements.
TestsInfusible on charcoal; dissolves in hydrochloric acid with the evolution of acrid chlorine gas. Borax bead test is easy, showing in the oxidizing flame a fine amethystine color. (Avoid getting too much and having a black bead.)
Distinguishing characteristicsThe sooty black character of the streak and the manganese tests prove presence of manganese, but it is virtually impossible to tell one manganese oxide mineral from another without distinct crystals, except by x-ray tests. Pyrolusite is a safe name for any fibrous-looking mass of black manganese oxide needles or for the black powdery alterations of other manganese minerals.
OccurrencePyrolusite is the most common and most important secondary ore of manganese. It forms under conditions of oxidation, either from primary manganese minerals such as the carbonate rhodochrosite, the silicate rhodonite, and the numerous manganese phosphates or as direct deposits from cold ground water in bogs and on the sea floor. It is usually the mineral responsible for fernlike markings commonly observed along rock fissures. These are known as dendrites and are often mistaken for fossil ferns. The mineral is extremely widespread; good specimens are found in some of the Minnesota and Michigan iron ores.
| Pyrolusite | |
|---|---|
Pyrolusite mineral with dendrite (height of sample ~ 9 cm). |
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| General | |
| Category | Oxide minerals |
| Chemical formula | MnO2 |
| Strunz classification | 04.DB.05 |
| Identification | |
| Color | Darkish, black to lighter grey, somethimes bluish |
| Crystal habit | Granular to massive: botryoidal and dendritic. Crystals rare |
| Crystal system | Tetragonal |
| Twinning | {031}, {032} may be polysynthetic |
| Cleavage | Perfect on 110 |
| Fracture | Brittle |
| Mohs scale hardness | 6–6.5, 2 when massive |
| Luster | Metallic, dull to earthy |
| Streak | Black to bluish-black |
| Specific gravity | 4.4–5.06 |
| Refractive index | Opaque |
| References | [1][2][3] |
| Major varieties | |
| Polianite | pseudomorphic after manganite[4] |
Pyrolusite is a mineral consisting essentially of manganese dioxide (MnO2) and is important as an ore of manganese. It is a black, amorphous appearing mineral, often with a granular, fibrous or columnar structure, sometimes forming reniform crusts. It has a metallic luster, a black or bluish-black streak, and readily soils the fingers. The specific gravity is about 4.8. Its name is from the Greek for fire and to wash, in reference to its use as a way to remove tints from glass.[3]
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Contents
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Pyrolusite and romanechite are among the most common manganese minerals. Pyrolusite occurs associated with manganite, hollandite, hausmannite, braunite, chalcophanite, goethite and hematite under oxidizing conditions in hydrothermal deposits. It also occurs in bogs and often results from alteration of manganite.[3]
The metal is obtained by reduction of the oxide with sodium, magnesium, aluminium, or by electrolysis. Pyrolusite is extensively used for the manufacture of spiegeleisen and ferromanganese and of various alloys such as manganese-bronze. As an oxidizing agent it is used in the preparation of chlorine; indeed, chlorine gas itself was first described by Karl Scheele in 1774 from the reaction products of pyrolusite and hydrochloric acid. Natural pyrolusite has been used in batteries, but high-quality batteries requires synthetic products. Pyrolusite is also used to prepare disinfectants (permanganates) and for decolorizing glass. When mixed with molten glass it oxidizes the ferrous iron to ferric iron, and so discharges the green and brown tints (making it classically useful to glassmakers as a decolorizer). As a coloring material, it is used in calico printing and dyeing; for imparting violet, amber, and black colors to glass, pottery, and bricks; and in the manufacture of green and violet paints.
Acicular radiating
Other manganese oxides:
This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press.
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