pyrolusite

Share on Facebook Share on Twitter Email
Top
('rō-lū'sīt) pronunciation
n.
A soft, black to dark gray mineral, MnO2, the commonest and most important secondary ore of manganese.

[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.


Top
pyrolusite ('rōlūzīt), naturally occurring manganese dioxide, MnO2, a black mineral that crystallizes in the tetragonal system but is usually found in earthy or massive deposits. It is the principal source of manganese and its compounds, and it is extensively used in steel smelting and in the manufacture of dry-cell batteries. The main producing countries are Russia, Brazil, South Africa, Gabon, India, China, and Australia.



MnO
Tetragonal -- Ditetragonal bipyramidal

Environment

Secondary manganese deposits and secondary veins.

Crystal description

Rarely 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 properties

Steel 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.

Composition

Manganese dioxide (63.2% Mn, 36.8% O), often with a small amount of water, heavy metals, phosphorus, and other elements.

Tests

Infusible 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 characteristics

The 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.

Occurrence

Pyrolusite 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.



Random House Word Menu:

categories related to 'pyrolusite'

Top
Random House Word Menu by Stephen Glazier
For a list of words related to pyrolusite, see:

Top
Pyrolusite

Pyrolusite mineral with dendrite (height of sample ~ 9 cm).
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]

Contents

Occurrence

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]

Use

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.

Variations in crystal habit

See also

Other manganese oxides:

References

 This article incorporates text from a publication now in the public domainChisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press. 


Post a question - any question - to the WikiAnswers community:

Copyrights:

Mentioned in

ramsdellite (mineralogy)