|Nature & Property of Asbestos
Nature & Property of Asbestos
Origin and Classifications of Asbestos
There are six types of asbestos: chrysotile, crocidolite, amosite, anthophyllite, tremolite and actinolite. They can be group into two distinctive groups according to their physical and chemical properties as well as mineralogical difference.
The Serpentine Group
Chrysotile is the sole mineral of this group. It is found in ultrabasic rock formations located in many places in the world. Chrysotile accounts for only a small percentage of the minerals found in these rock types, the rest being its variations forms. Chrysotile fibers are formed as a result of metamorphism and are found as veins in serpentines, in serpentinized ultramafic rocks, and in serpentinized dolomitic marbles.
It°Įs believed that the ultrabasic rocks, containing olivine, Mg-rich pyroxenes, and amphiboles are first altered by hydrothermal processes to form the serpentine minerals; in a later metamorphic event, the serpentines are partially re-dissolved and crystallized as chrysotile fibers, and this view is supported by the fact that chrysotile is commonly found with remnants of serpentine even in industrialized products.
Clearly, the genesis of each chrysotile deposit must have involved specific features related to the composition of the precursor minerals, the stress and deformations in the host matrix, the water content, the temperature cycles, etc. As a result, it is generally observed that the chemical composition of the fibrous phase is closely related to that of the surrounding rock matrix.
The Amphibole Group
This group is made up of crocidolite, amosite, anthophyllite, tremolite and actinolite, and is widely found throughout the earth's crust. Their chemical composition can vary widely.
Of the amphiboles, only a few varieties have an asbestiform habit and occur in relatively low quantities. The geological origin of amphibole asbestos fibers appears to be quite varied. In the case of the crocidolite deposit of South Africa (Transvaal), the amphibole fibers formed during secondary chemical reactions that took place as the banded ironstone host rock consolidated from a gel of iron hydroxide and colloidal silica. Crocidolite fiber veins formed, presumably with magnetite particles acting as nucleating agents. The presence of mechanical stress appears to be necessary for the formation of crocidolite. It appears that fibers form in places where there is shearing (slip fibers) or rock dialatium (cross fiber). It°Įs not expect that fibers will form in rock that is not mechanically disturbed. The amosite deposit found in similar rock formations is the result of a high temperature metamorphic process.
Mineral Characteristics of Asbestos
Most common type of chrysotile deposit grow with the fibers at right angles to the walls of cracks (cross-vein) in massive serpentine formations. In some occurrences, the relative motions (slipping) of blocks in the host rock, during or after fiber growth, lead to veins in which the fibers are inclined or parallel to the vein axes (slip fibers). In still other local conditions, dispersed aggregates of fibers are found with no preferential orientation but with high fiber content, up to 50% of the surrounding rocks. These are called mass-fiber deposits.
Most of the industrial chrysotile fibers are extracted from deposits where fiber lengths can reach several centimeters (cm), but most often do not exceed 1 cm.
Among the five asbestos fibers in the amphiboles group, only three fibers have industrial significance: crocidolite and amosite were the only amphiboles with significant industrial uses in recent years; tremolite, although having essentially no industrial application, may be found as a contaminant in other fibers or in other industrial minerals (e.g., chrysotile and talc).
The differences in microscopic and macroscopic properties of asbestos fibers stem from their intrinsic, and sometimes unique, crystalline features. As with all silicate minerals, the basic building blocks of asbestos fibers are the silicate tetrahedra which may occur as double chains (Si4O11)-6, as in the amphiboles, or in sheets (Si4O10)-4, as in chrysotile.
Structure of Chrysotile
In the case of chrysotile, an octahedral brucite layer having the formula (Mg6O4(OH) 4)-4 is intercalated between each silicate tetrahedra sheet. The silicate and brucite layers share oxygen atoms which would normally be separated by distances of 0.305 nm in the silicate layer and 0.342 nm in the brucite layer. This mismatch of O-O distances induces a curvature of the sheets, the ideal radius of which has been calculated as 8.8 nm. The curvature of the sheets propagates along a preferred axis leading to the formation of the tubular structure found in chrysotile. The concentric sheets forming the fibers have a curvature radius from 2.5 to 3.0 nm for the internal layers up to approximately 25 nm for the external layers, yielding unit fibers (fibrils) with external diameters ranging between 20 and 50 nm. Electron microscopy studies have also shown that, in the unit chrysotile fiber cross-section, the layers may appear in a concentric or spiral arrangement. The stacking of the tetrahedral and octahedral sheets in the chrysotile structure has been shown to yield three types of chrysotile fibers:
clino-chrysotile: monoclinic stacking of the layers, x parallel to fiber axis, most abundant
formortho-chrysotile: orthorhombic stacking of the layers, x parallel to fiber
axispara-chrysotile: two layer structure, 180°„ rotation of two-layer structures, y parallel to fiber axis
The extent of substitution of magnesium and silicon by other cations in the chrysotile structure is limited by the structural strain that would result from replacement with ions having inappropriate radii. In the octahedral layer (brucite), magnesium can be substituted by several divalent ions, Fe+2, Mn +2, or Ni+2. In the tetrahedral layer, silicon may be replaced by or Al+3 or rarely Fe+3. Most of the other elements that are rarely found in vein fiber samples, or in industrial asbestos fibers, are associated with interstitial mineral phases. Typical compositions of bulk chrysotile fibers from different locations are given in the table below:
Structure of Amphiboles
The crystalline structure common to amphibole minerals consists of two ribbons of silicate tetrahedra placed back to back.
The plane of anionic valency sites created by this double ribbon arrangement is neutralized by the metal cations. The crystal structure has sixteen cationic sites of four different types; these sites can host a large variety of metal cations without substantial disruption of the lattice.
In contrast to chrysotile fibers, the atomic crystal structure of amphiboles does not inherently lead to fiber formation. The formation of asbestiform amphiboles must result from multiple nucleation and specific growth conditions. The difference between asbestiform and massive amphibole minerals is obvious on the macroscopic scale although, the crystalline structures of the two varieties do not exhibit substantial differences. The asbestiform amphiboles tend to have a larger number of crystal defects (Wadsley defects and twinning and chain width disorder) than the nonasbestiform varieties. The frequency and width of these defects vary with amphibole type. Amphibole minerals, in general, are characterized by prismatic cleavage planes parallel to the c axis which intersect at an angle of about 56°„. Hence, in the crushing of massive, nonfibrous amphiboles, microscopic fragments are found having the appearance of asbestos fibers. However, the statistical average of their aspect ratio is considerably lower than that of the asbestiform amphiboles.
Physical Properties of Asbestos
Chrysotile fibers can be extremely thin, the unit fiber having an average diameter of approximately 25 nanometers (nm) (0.025 :m). Industrial chrysotile fibers are aggregates of these unit fibers that usually exhibit diameters from 0.1 to 100 :m; their lengths range from a fraction of a millimeter (mm) to several centimeters (cm), though most of the chrysotile fibers used are shorter than 1 cm.
Asbestos fibers used in most industrial applications consist of aggregates of smaller units (fibrils). This is most evident in chrysotile that exhibits an inherent, well-defined unit fiber. Diameters of fiber bundles in bulk industrial samples may be in the millimeter range in some cases; fiber bundle lengths may be several millimeters to 10 cm or more.
The mechanical processes employed to extract the fibers from the host matrix, or to further separate (defiberize, open) the aggregates, can impart significant morphological alterations to the resulting fibers. Typically, microscopic observations on mechanically opened fibers reveal fiber bends and kinks, partial separation of aggregates, fiber end-splitting, etc. The resulting product thus exhibits a wide variety of morphological features
(see image below).
Morphological variances occur more frequently with chrysotile than amphiboles. The crystal structure of chrysotile, its higher flexibility, and interfibril adhesion allow for a variety of intermediate shapes when fiber aggregates are subjected to mechanical shear. Amphibole fibers are generally more brittle and accommodate less morphological deformation during mechanical treatment.
Fiber Length Distribution
For industrial applications, the fiber length and length distribution are of primary importance because they are closely related to the performance of the fibers in matrix reinforcement. Various fiber classification methods have thus been devised. Representative distributions of fiber lengths and diameters can be obtained through measurement and statistical analysis of microphotographs; fiber length distributions have also been obtained from automated optical analyzers.
Asbestos fiber minerals are hydrated silicates so their behavior as a function of temperature is related first to dehydration (or dehydroxylation) reactions. In the case of chrysotile, the crystalline structure is stable up to approximately 550°„ C (depending on the heating period), where the dehydroxylation of the brucite layer begins. This process is completed near 750°„ C and is characterized by a total weight loss of 13%. The resulting magnesium silicate recrystallizes to form forsterite and silica in the temperature range 800-850°„ C, as an exothermic process. The strongly endothermic dehydration process enhances the high temperature thermal insulation properties of chrysotile asbestos.
The behavior of amphibole fibers under continuous heating is similar to that observed with chrysotile, although the temperatures of dehydroxylation and recrystallization processes are different. The amphiboles have a lower water (hydroxyl) content and their dehydroxylation reaction begins between 400-600°„ C, depending on the amphibole type; this reaction leads to a weight loss of approximately 2%. The products resulting from the thermal decomposition of the amphiboles are pyroxenes, magnetite, hematite, and silica.
In the presence of oxygen, the thermal decomposition of amphiboles is associated with an oxidation of divalent iron to trivalent iron, which may lead to an increase in the sample weight. The oxidation process also induces an obvious color alteration: the fibers acquire the characteristic ferric oxide color.
Asbestos fibers, in particular chrysotile fibers, can undergo substantial thermal degradation during mechanical grinding. In high-energy attrition equipment, such as ball mills, the high localized impact energies can cause the crystalline structure to become amorphous. This is particularly true for dry milling or milling in organic solvents. However, milling in aqueous slurries is less detrimental, water offering some protection against high impact degradation.
The inherent tensile strength of a single asbestos fiber, based on the strength of Si-O-Si bonds in the silicate chain, should be near 10 gigapascals (GPa) (1.45 x 106 pounds per square inch [psi]). However, industrial fibers exhibit substantially lower values, because of the presence of various types of structural or chemical defects.
The measured tensile strength of chrysotile fibers has been reported in the range 1.1-4.4 GPa (160,000-640,000 psi). The accurate determination of this parameter is difficult since the measurement performed on a fiber aggregate is influenced by interfibril adhesion, discontinuities in some of the unit fibers, mineral inclusions, etc. Consequently, higher tensile strength results are obtained for measurements done on short and thin fibers. The tensile strengths of amosite and crocidolite are comparable to that of chrysotile. With amphiboles, the tensile strength is highly influenced by the iron content since iron-oxygen bonds located in the fiber axes, particularly those involving trivalent Fe, are particularly strong. The trend observed of increasing tensile strength of amphiboles from tremolite, to amosite, to crocidolite is directly related to the iron content of these fibers.
The variation in tensile strength of asbestos fibers as a function of temperature also sharply distinguishes chrysotile and amphiboles. Chrysotile retains (and even slightly increases) its tensile strength up to 500°„ C, until the dehydroxylation reaction begins; it drops sharply at higher temperatures. Amphiboles, on the other hand, exhibit a decreasing tensile strength beginning at approximately 200°„ C. For example, at 350°„ C, crocidolite has lost 50% of its initial tensile strength.
Chemical Composition of Asbestos
Chrysotile is a hydrated magnesium silicate and its stoichiometric chemical composition may be given as Mg3Si2O5(OH)4. However, the geothermal processes that yield the chrysotile fiber formations usually involve the co-deposition of various other minerals. These mineral contaminants comprise: brucite Mg(OH)2), magnetite (Fe3O4), calcite (CaCO3), dolomite ((Mg,Ca)(CO 3)2), chlorite ((Mg,Al,Fe)12Si8O20(OH)16), and talc (Mg6Si8O20(OH)4). Other iron-containing minerals may also be found in chrysotile, for example, pyroaurite, brugnatellite, and pyroxenes. In commercial fibers, dust particles from the host rock generated during the mining and milling processes are most inevitably present. Elemental analysis data for several chrysotile and amphibole samples are presented in the table below.
The chemical composition of amphiboles readily reflects the complexity of the environment in which they formed. The average chemical composition of amphibole minerals may be represented as:
A0-1, B 2C5T8O22 (OH, O, F, Cl)2
where A= Na, K B= Na, Ca, Mg, Fe+2, Mn, Li C= Al, Fe +2, Fe+3, Ti, Mg, Mn, Cr T= Si, Al A, B, C each represent cationic sites within the crystal structure.