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 />
150<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 />
The most abundant form <strong>of</strong> <strong>the</strong> trioctahedral<br />
serpentine minerals. It crystallizes as flat<br />
platelets. Variable amounts <strong>of</strong> Al substitute for<br />
both Mg <strong>and</strong> Si in <strong>the</strong> ideal serpentine formula<br />
<strong>of</strong> Mg3Si2O5(OH) 4 to create a better lateral<br />
fit between <strong>the</strong> component octahedral <strong>and</strong><br />
tetrahedral sheets than found in antigorite <strong>and</strong><br />
chrysotile. Several polytypes exist: rhombohedral,<br />
trigonal, hexagonal, or monoclinic.<br />
Lizardite A trigonal <strong>and</strong> hexagonal mineral,<br />
Mg3Si2O5(OH) 4; kaolinite-serpentine<br />
group; polymorphous with<br />
antigorite, clinochrysotile, orthochrysotile,<br />
<strong>and</strong> parachrysotile;<br />
forms a series with nepouite; in<br />
platy masses as an alteration product<br />
<strong>of</strong> ultramafic rocks; <strong>the</strong> most<br />
abundant serpentine mineral.<br />
A white, yellowish, or pinkish orthorhombic<br />
zeolite mineral: (Na •<br />
2,Ca,K2)Al2Si10O24 7H2O.<br />
Mordenite A white, yellowish, or pinkish<br />
member <strong>of</strong> <strong>the</strong> zeolite group<br />
<strong>of</strong> minerals with <strong>the</strong> formula<br />
(Ca,Na2K2)Al2Si10O24.7H2O. (a) A white, grayish, yellowish, or<br />
grayish-green chain-structure clay<br />
mineral: (Mg,Al) 2Si4O10(OH) •4H2O. It crystallizes in several monoclinic<br />
<strong>and</strong> orthorhombic polytypes.<br />
(b) A group name for monoclinic<br />
minerals with an analogous composition,<br />
but with Mg replaced by Mn or Na,<br />
<strong>and</strong> AL replaced by Fe3+ or Mn3+ .<br />
Palygorskite 1. A monoclinic <strong>and</strong><br />
orthorhombic mineral,<br />
(OH) •<br />
2(Mg,Al) 4(Si,Al) 8O20 8H2O;<br />
fibrous; in desert soils.<br />
2. A general name for lightweight<br />
fibrous clay minerals showing<br />
significant substitution <strong>of</strong> aluminum<br />
for magnesium; characterized<br />
by distinctive rodlike shapes<br />
under an electron microscope.<br />
See footnotes at end <strong>of</strong> table. (Continued)<br />
NIOSH CIB 62 • <strong>Asbestos</strong>