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 ...
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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