Document K6dyrBeg19vQ3Kx54xZYgMyGw
FILE NAME Brakes BRK
DATE 1978
DOC BRK068
DOCUMENT DESCRIPTION Journal Article - Dark Electron Microscopy and Chrysotile Asbestos
'
ENVIRONMENTAL RESEARCH 16 383 392 1978
On the Utility of Field Electron Microscopy in the
|
Determination of the Degree of Deformation In
Chrysotile Asbestos An Environmental Research
seat
Application
ATE
K. SESHAN
Department of Materials Science and Engineering Materials and Molecular Research Division Lawrence Berkeley Laboratory University of California Berkeley California 94720 Received June 21 1977
The degree of microcrystalline deformation in fibers of chrysotile asbestos may be distin-
guished using high resolution field electron microscopy This is demonstrated by com-
paring undeformed chrysotile with Union Internationale Contre le Cancer UICC standard
reference samples The UICC samples are shown to be partially deformed as a result of
milling in the mixing process Samples of used and unused brake shoe lining dust were examined using this technique it is shown that chrysotile asbestos in various stages of
deformation undeformed to heavily deformed in automobile brake
drum dust Such dark images can serve to identify the source of asbestos found in
environmental pollution samples
INTRODUCTION
There is a controversy in the literature whether or not fibers of chrysotile
z
asbestos survive in automobile brake drum dust two studies Rohl et al 1976
PE
Alste et al 1976 report that the fibers do survive and earlier work Lynch 1968
Hickish and Knight 1970 reports that they do not The latter claim that the
sotile is converted to forsterite under the high temperatures attained in the
braking process
As high resolution dark electron microscope images are sensitive to the degree of deformation they can be used to distinguish between deformed and undeformed fibers and thus to resolve these two differing sets of results It is shown using this technique that chrysotile asbestos fibers in various states of
deformation undamaged to heavily deformed and recrystallized
in automobile brake drum dust
SAMPLE SELECTION AND PREPARATION
Z
Four samples were selected A undeformed chrysotile ore samples from ser-
pentine outcrop of Calaveras County California B slightly deformed UICC reference standards of Canadian chrysotile milled during preparation to reduce
fiber size Timbrell et al 1969 C unused brake lining dust collected during
burnishing prior to installation of new brake shoes and D brake drum dust
collected from the front and rear brake drums of a State vehicle obtained during brake shoe service Seshan and Smith 1977
Samples were transferred directly to Formvar electron microscope grids
6 and coated with carbon on both sides :
eaertsLeang
Tha 2
elas8
Calle 1/17/83 46 Calle
Calle
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0013-9351 1613-0383 1613-0383
Copyright '1978 by Academic Press Inc.
All rights of reproduction in any form reserved
:
1/17/83
1/17/83
384
K. SHAN
EXPERIMENTAL
As the high resolution dark field method is described in great detail elsewhere Hirsch et al 1969 only a very brief description is included here An electron
beam striking a polycrystalline specimen with grains of different orientation e.g.
A and in Fig ) is diffracted into cones causing the typical polycrystalline ring
pattern The resolution field method consists oftilting the incident beam
so that the part of the diffracted ring passes through the optic axis of the micro-
et, scope Fig 1b The tilting is accomplished with the electronic beam tilt device Then an aperture collects intensity only from those crystallites diffracting into this
Coe
part of the ring e.g. B Fig 1c
Various factors involved in the interpretation of the diffraction patterns of
chrysotile asbestos fiber bundles are shown in Fig 2. The actual lattice of
chrysotile is a defected scrolled crystal with fiber axis along a Yada 1967 The
reciprocal lattice of this crystal should be some form of a spiral equispaced along the a axis Zvyagin 1967 and Whittaker 1966 have studied diffraction effects
from concentric cylinders How deformation and shear will affect the diffraction
patterns has not to the author's knowledge been studied and is under study here
The simpler case of an undeformed defect chrysotile fiber where the fiber
is idealized as a series of concentric cylinders as first proposed by Whittaker
1969 is shown in Fig 2i The reciprocal lattice then consists of a series of
concentric rings shown in Fig 2ii only the two rings in the 2kl layer are drawn
The electron diffraction pattern represents the intersection of the reflecting or
Ewald sphere ES Fig 2 with these rings Hirsch et al 1969 This ought to
result in a series of spots as shown in the -2kl layer line Streaked patterns are
tt
however obtained from single fibers of chrysotile Yada 1967 Seshan and Smith
1977
othov The explanation for the streaking probably lies in refraction effects and the fiber
shape Yada 1969 it could also result from the various faults produced during the
FIG 2 Illustration of t idealized as a senes of co 1967 The reciprocal latte " axis as in the 2k Lays produced as shown on the bly from the spiral shape c fiber bundle fibers of diff typical arcuate pattern
growth of the crystal
their influence on def When bundles of fi
and 3b showing a
arcuate patterns of
dark image obta 3b should yield unife to be expected only i the experimental obs
y
b
c
Fig 1 Hustration of the high resolution dark method a The bright image from a selected area of poly crystal illustrated with two grains A and B b The situation after gun tilt only a portion of the diffracted intensity is collected by placing the objective aperture as shown c The resulting resolution dark image with only favorably oriented grains g B showing dif-
fracted intensity or lighting up
Bright and dark Fig 3. The dark field as explained above
an undeformed cryst
The striking featur
hollow canals and thi
be explained on the F
DEFORMATION OF CHRYSOTILE ASBESTOS
385 385 385
t
a
kl Ikl
I i
i
.
1
loo.
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t
.
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OXI IX -2kl
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Lf rc
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og J
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F2 F2 Illustration of the real and reciprocal lattice of a defect chrysotile fiber i and u
idealized as a series of concentric cylinders The actual structure is a defected spiral sheet Yada
1967 The reciprocal lattice of the ideal fiber is then a series of equispaced concentric rings along the
-
AXIS as the 2kl layer when these rings intersect the Ewald sphere ES spots ought to be
p died as shown the -2kl layer line However streaks are observed Yada 1967 arising proba-
p's from the spiral shape of the fiber defects and strains formed during the scrolling process When
fibe bundle fibers of different orientations is imaged the layer lines are smeared out yielding a
typical arcuate pattern as Fig 36
growth of the crystal The influence of these faults on the diffraction patterns and their influence on deformation needs further study
When bundles of fibers are involved the streaks are replaced by arcs Figs 2iv and 3b showing a strong tendency toward a texture and yielding the typical arcuate patterns observed by several researchers e.g. Rohl et al 1976 The
image obtained by imaging any part of the arc as shown in Figs 1 and
:
35. should yield uniform intensity if the crystal is homogeneous This is the case to be expected only in the case of the undeformed fibers is consistent with the the experimental experimental observations in Figs 3a and 3b
RESULTS
Bright and field images of naturally occurring chrysotile A are shown in
Fig 3 The dark field is obtained by imaging a portion of the diffracted intensity
as explained above The result is a uniform contrast as would be expected from
aada) an undeformed crystal The striking feature of the dark images is the great intensity along the
per
hollow canals and this needs further investigation The intensity difference cannot
'
be explained on the basis of differences in absorption alone it appears that some
386
K. SESHAN
Ty abe
condenser the fib Fig 3a precaution focused and the b
A natural chrysotile a and b Dark and diffraction pattern Notice the
Fic 3 Sample
and undeformed A faint
unusually bright and undamaged internal canals the crystal is homogeneous
outline of the objective aperture is seen in the diffraction pattern of Fig 3b c Illustrates the blistering
as a result of exposure to the beam
are operative Notice that the canals are sometimes bright
diffraction processes
the intensity is uniform
and sometimes dark In the crystalline part however
and it is clear that these fibers are free of gross deformation
fibers like most sheet silicates are sensitive to 100 elec-
Chrysotile
trons Langer et al
1974 Seshan
1975 Precaution must therefore be exercised
because
focusing the
while obtaining the high resolution field images
upon
FIG 4 Sir a
that illustrate that th
polycrystal polycrystal The spa
different set st*
obtained
Pe _
aad
DE FORMATION OF
CHRYSOTILE ASBESTOS
387
condenser the fibers tend to become blistered In the dark image shown in Fig 3a precaution was taken to prevent any beam damage the condenser was not
focused and the beam was tilted in the dark field mode The condenser was then
0)
A
reste
weet shake care
sot
y
Notice Notice the the . faint
BlisterinBlistgering
FIG 4 Sample B UICC Standard Reference Canadian chrysotile a and b Dark images that illustrate that the ball milling during the mixing step converts the chrysotile into a grained polycrystal The aperture is moved from one part of the ring to another resulting in an entirely different set of grains lighting up c The bright image from which little information can be
obtained
388
K. SESHAN
focused to obtain the diffraction pattern shown in Fig 3b The resulting beam damage is shown in Fig 3c The use of beam sensitivity to distinguish chrysotile from other sensitive materials e.g. the amphiboles has been discussed by Langer et al 1974
Dark and bright images of deformed UICC standards B are shown in Figs 4c The effects of deformation are clearly seen in the dark images 4a and 4b and in the electron diffraction patterns but not in the bright
images 4c The
there appear small microdomains of
strongly textured changed to those
structural nature ( effect of translatir
in Figs 4a and 4b
or show diffracted To isolate the e
shoe burnishing d B is not inform
internal canals s
FIG 5. Sample C Burnishing dust from an automobile brake drum prior to installation a Dark field b diffraction pattern and c bright field Notice the preserved canal which shows up the dark image in a indicated by the arrow and arrowhead This and the well preserved diffraction pattern b shows that the fibers are not as deformed as the UICC samples conclusion that cannot
be inferred from the bright image c
FIG 6 Sample D Although the bright fition patterns are rema this can happen for a
Ne
a
Ge : f
ae
ee
re
- By
rah
i FAS
ae
ee
mn
Bape
DEFORMATION OF CHRYSO ASBESTOS
389
images 4c The clear internal canals of the undeformed sample A are destroyed there appear small submicron 100 ^ areas which light up as if they were grains or microdomains of different orientations consistent with this observation the
strongly textured diffraction patterns of the undeformed fibers Fig 3 are changed to those of a polycrystal At the present the crystallographic and microstructural nature of the deformation is not clear and warrants further study The
effect of translating the aperture to a different part of the diffracted ring is shown in Figs 4a and 4b The result is that grains in a different orientation light up or show diffracted intensity signifying that this is truly a diffraction effect
To isolate the effects of deformation during the braking process unused brake
shoe burnishing dust C was examined Figs 5a and 5b The bright image B is not informative whereas the dark image clearly shows some intact internal canals see arrow and arrowhead Fig 5a resembling the undeformed
hy
ag FIG 6 Sample D Brake drum dust after use in a state vehicle a Bright field and b dark field
SORE
Although the bright field is not distinctive the resolution dark field and the selected area diffrac-
rene
tion patterns are remarkably different The crystal is quite inhomogeneous with very large grain sizes
this can happen for a variety of reasons see text
ee
RIT
oR
390
K. SHAN
a also small deformation domains which clearly re-
chrysotile Fig 3 There are
therefore deformed less
semble the UICC standard B samples These fibers are
than the UICC standard samples Fig 4 as some intact internal canals can still be
to derive this conclusion from the bright range
seen It is impossible
fiber found in brake drum dust are
Samples of of heavily deformed chrysotile
shown in Fig 6 in the bright and dark field Whereas the effects of deformation are
the difference difference in the field image is quite
not evident in the bright image
is reflected in the electron diffraction
striking The crystal is inhomogeneous This This 6c The mottled contrast of black
pattern now showing a number of spots ( Fig
severe surface deforma-
and bright areas could arise from one of secvoenravlercsaiuosnes or grain growth under
tion leading to uneven crystal thickness
or transformation of local areas
heat and deformation to large grain polycrystal
forsterite Further investigation into carefully
into a new crystallineisphraeqsueiree.dg.to decide which it is It is however quite clear
found in the
deformed chrysotile that these identifying effects are associated only with the samples
used brake drum dust
also found in the brake drum dust
Undeformed and unaltered chrysotile is
after use sample D Fig 7 This was confirmed by electron diffraction
collected
was calibrated using a
which were indexed after the camera constant
patterns
deposited gold standard with the following results
Used brake dust Yada 1967
diameter ^ diameter ^
hhl
2.62 2.60
130
2.34 2.30 220
1.49 1.46 005
clear dark evidence that not all the fibers are deformed
There is also
found in the brake drum
Figure 7 shows the dark- and bright images of fibers
asbestos B
dust the field image resembles that of the UICC chrysotile
4 and those in the unused brake lining C. shown Fig 5 the grain
shown in Fig
Based upon this observation it is
sizes being the same as in the UICC samples
concluded that a variety of products ranging from almost undeformed to com-
pletely transformed chrysotile products exist in brake drum dust
DISCUSSION AND CONCLUSIONS
resolution field electron microscopy can dis-
It is demonstrated that resolution
asbestos fibers In particular it
tinguish the degrteheatofUdIeCfCorsmtaatnidoanrdinchrcyhrsyostotiilleecchhrryyssootitlielehas undergone microdeformation then
has been shown
The dark method may
of ball milling in the preparation step
as a result
trace the origins of asbestos fibers
be used by environmental researchers to
in the micro-
The dark images suggest that there are significant chaanngdesmicrostructural
structure of chrysotile upon deformation the cystallographic
details of which are complex and are worthy of further study
to the beam sensitivity of chrysotile Yada 1967
There are several references
effect to distinguish sotile from
et al 1974 The utility of using this
Lotahnegrersensitive materials could be of value to environmental pollution
research
7
FIG
Sample
shows that relative
field images a are indicating little det
This prelimi chrysotile asbe
deformation e
thank G R
problem to my att
Walter John and
by the
US Ener
AlsteJ aks
pop 10 Hatch D 1970 Hickish E.
Occup Hy Hirsch P B.H
Crystals
Langer A M asbestos fr
Lynch JR JR I
Rohl A. N. L. N. lining main
Seshan K and
DEFORMATION OF CHRYSOTILE ASBESTOS
Fit 7 Sample D Automobile brake drum dust after use a Dark field and b bright field This shows that relatively undeformed fibers survive in the brake drum dust The grain sizes in the darkfield images a are comparable to those in the burnishing dust Fig 5a or the UICC samples Fig 4a
indicating little deformation during use
This preliminary study also shows the need to study details of the growth of the
^'
chrysotile asbestos and the nature of the defects involved if all the diffraction and
a
4
4
deformation effects are to be understood
d
hee ACKNOWLEDGMENTS
ase
I thank G R Smith of the Air Industrial Hygiene Laboratory AIHL Berkeley for bringing this
J 4
wert
problem to my attention and preparing preparing the samples I acknowledge useful discussions with him and Dr
MaEt Walter John and thank Professor Washburn for encouragement This work was supported financially
cepa by the US Energy Research and Development Administration
Dow
REFERENCES
Ser
Alste J. Watson D. and Bagg J 1976 Airborne asbestos in the vicinity of a freeway Atmos
Environ 10 583
Hatch D. 1970 Possible alternatives to asbestos as a friction material Ann Occup Hyg 13. 25
Hickish D E. and Knight K. L 1970 Exposure to asbestos during brake maintenance Ann
Leys Occup Hyg 13 17
Ih
Hirsch P B. Howie A. Pashley D W. and Whelan M. J. 1965 Electron Microscopy of Thin
ep
Crystals Butterworths London
Rea
Langer A M Mackler A. D. and Pooley D. 1974 Electron microscopical investigation of
RR asbestos fibers Environ Health Perspect 9 63
Be
Lynch JR JR 1968 Brake lining decomposition products J. Air Pollut Control Assoc 18 824
ye Rohl A N. Langer A. M. Wolff M. S. and Weisman I. 1976 Asbestos exposure during brake
hate
lining maintenance and repair Environ Res 12 110
a
ty r
Seshan K. and Smith G. R. 1977 Characterization of chrysotile asbestos in automobile brake drum
K.
aa
392
K. SFSHAN
dust by transmission electron microscopy Proceedings 35th Annual Meeting of EMSA
Claitors Baton Rouge La
standard reference
Timbrell V. 1969 Characteristics of the international union against cancer
samples of asbestos Pneumoconiosis In Proceedings International Conference on
Pneumoconiosis Johannesburg p 28. In Oxford Univ Press England
Whittaker E. J. W. 1966 Diffraction contrast in electron microscopy of Chrysotile Acta Crystal-
logr 21 4616
resolution electron microscope Acta Crystal-
Yada K 1967 Study of chrysotile asbestos by a high
Zvyalgoign 2B.3 B7041967 Diffraction Analysis of Clay Mineral Structures Plenum New
York
i
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oer ED
FEY
Be
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ENVIRONMENTAL RESEARCH RESEARCH
Development Exposure
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Asbestos cement ranks first amorata amorata Leineweber P AC sheets and pipes
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to investigate the trolled laboratory de outbred LVG 1
chosen because st^/d in terms of lesion s dusts and th
chrysotile asbestos a in the exposed air coniosis and cigare and epithelial less e
hamster following following number of investiga investiga
1970 Dontenwillet Dontenwillet fiotti 1968a b 1970 Althoff and Auttan Auttan study of the re re extensively ex gens and convenier convenier 1970 and Do