22.02.2013 Views

Asbestos Fibers and Other Elongate Mineral Particles: State of the ...

Asbestos Fibers and Other Elongate Mineral Particles: State of the ...

Asbestos Fibers and Other Elongate Mineral Particles: State of the ...

SHOW MORE
SHOW LESS
  • No tags were found...

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Table 2. Definitions <strong>of</strong> specific minerals (Continued)<br />

Glossary <strong>of</strong> Geology, 5th ed.<br />

[American Geological Institute 2005] Leake et al. [1997] NIOSH [1990a]<br />

Dictionary <strong>of</strong> Mining,<br />

<strong>Mineral</strong>, <strong>and</strong> Related Terms<br />

[U.S. Bureau <strong>of</strong> Mines 1996]<br />

[Note: Footnotes identify <strong>the</strong> Primary<br />

Source Citation for <strong>the</strong> definition]<br />

Term<br />

NIOSH CIB 62 • <strong>Asbestos</strong><br />

Anthophyllite can occur in<br />

both <strong>the</strong> asbestiform <strong>and</strong><br />

nonasbestiform mineral<br />

habits. The asbestiform<br />

variety is <strong>of</strong>ten referred to<br />

as anthophyllite asbestos.<br />

An orthorhombic Mg-Fe-Mn-<br />

Li amphibole: Mg7Si8O22(OH) 2;<br />

may also contain divalent<br />

iron but with Mg/(Mg+Fe2+ )<br />

≥ 0.50 (o<strong>the</strong>rwise ferroanthophyllite),<br />

<strong>and</strong> with Si ><br />

7.00 (o<strong>the</strong>rwise it is gedrite).<br />

A clove-brown to colorless orthorhombic<br />

mineral <strong>of</strong> <strong>the</strong> amphibole group: (Mg,<br />

Fe2+ ) 2(Mg,Fe2+ ) 5Si8O22(OH) 2. It is dimorphous<br />

with cummingtonite; with increase in aluminum<br />

it grades into gedrite. Anthophyllite occurs<br />

in metamorphosed ultrabasic rocks, typically<br />

with olivine or talc or in monominerallic<br />

aggregates <strong>of</strong> parallel or radiating asbestiform<br />

fibers. It has been mined for asbestos.<br />

Anthophyllite An orthorhombic mineral,<br />

4[Mg,Fe) 7Si8O22(OH) 2];<br />

amphibole group; commonly<br />

lamellar or fibrous, green to<br />

clove-brown; in schists from<br />

metamorphosed ultramafic rocks;<br />

a nonspinning grade <strong>of</strong> asbestos.<br />

palygorskite<br />

Attapulgite A light-green, magnesiumrich<br />

clay mineral, named from<br />

its occurrence at Attapulgus,<br />

GA, where it is quarried as<br />

fuller’s earth. Crystallizes in<br />

<strong>the</strong> monoclinic system.<br />

An olive-green asbestiform variety<br />

<strong>of</strong> tremolite-actinolite.<br />

Byssolite An olive-green asbestiform<br />

variety <strong>of</strong> tremolite-actinolite.<br />

A group name for a monoclinic zeolite<br />

mineral with <strong>the</strong> general formula:<br />

A •<br />

2-3(Si,Al) 18O36 11H2O, where A = Na, K, or Ca.<br />

Clinoptilolite A monoclinic mineral, (Na,<br />

K,Ca) 2Al3(Al,Si) 2Si13O36.12 H2O; <strong>of</strong> <strong>the</strong> zeolite group.<br />

Chrysotile generally occurs segregated<br />

as parallel fibers in veins<br />

or veinlets <strong>and</strong> can easily separate<br />

into individual fibers or bundles.<br />

Often referred to as “white asbestos,”<br />

it is used commercially for its<br />

good spinnability in <strong>the</strong> making <strong>of</strong><br />

textile products, <strong>and</strong> as an additive<br />

in cement’ or friction products.<br />

A white, gray, or greenish orthorhombic<br />

or monoclinic mineral <strong>of</strong> <strong>the</strong> serpentine<br />

group: Mg3(OH) 4Si2O5. It is a highly<br />

fibrous, silky variety <strong>of</strong> serpentine, <strong>and</strong><br />

constitutes <strong>the</strong> most important type <strong>of</strong><br />

asbestos. Not to be confused chrysolite.<br />

Chrysotile A monoclinic mineral (clinochrysotile),<br />

or orthorhombic mineral<br />

(orthochrysotile, parachrysotile),<br />

[Mg6(OH) 8Si4O10]; serpentine<br />

group; forms s<strong>of</strong>t, silky white, yellow,<br />

green, or gray flexible fibers as<br />

veins in altered ultramafic rocks;<br />

<strong>the</strong> chief asbestos minerals. (Not<br />

to be confused with chrysolite.)<br />

See footnotes at end <strong>of</strong> table. (Continued)<br />

147

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!