Philip Morris
Epa Study of Biological Effects of Asbestos - Like Mineral Fibers
Fields
- Author
- Coffin, D.L.
- Palekar, L.D.
- Type
- SCRT, REPORT, SCIENTIFIC
- ABST, ABSTRACT
- CHAR, CHART, GRAPH, TABLE, MAPS
- FOOT, FOOTNOTES
- PHOT, PHOTOGRAPH
- ABST, ABSTRACT
- Area
- SOLANA,RICHARD/CENTRAL FILES
- Litigation
- Fali/Produced
- Characteristic
- EXTR, EXTRA
- Site
- R545
- Named Organization
- Natl Bureau of Mines
- Reserve Mining
- Second Advisory Comm
- Uicc
- Workshop on Asbestos
- Duluth Gabbro
- Epa, Environmental Protection Agency
- Il Inst of Technology
- Il Inst of Technology Research Inst
- Reserve Mining
- Author (Organization)
- Environmental Sciences Group
- Epa, Environmental Protection Agency
- Health Effects Research Lab
- Northrop Services
- Epa, Environmental Protection Agency
- Named Person
- Ames
- Bleifuss, R.
- Cooper, C.
- Gross, P.
- Langer, A.
- Mitchell, P.
- Nicholson, W.
- Nord, G.
- Palekar, L.D.
- Ross, M.
- Smith, B.
- Walia, D.
- Wiley, A.
- Bleifuss, R.
- Master ID
- 2063104795/5283
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- Date Loaded
- 20 Sep 1999
- UCSF Legacy ID
- hbp52d00
Document Images
CS
National Bureau of Standards Special Publication 506. Proceedings of the Workshop on
Asbestos: Definitions and Measurement Methods held at NBS, Gaithersburg, MD, July 18-20,
1977. (Issued November 1978)
EPA STUDY OF BIOLOGICAL EFFECTS OF ASBESTOS-LIKE MINERAL FIBERS
D. L. Coffin
EPA Health Effects Research Laboratory
Research Triangle Park, North Carolina 27709
and
L. D. Palekar
Health Effects Research Laboratory
Northrop Services, Inc.
Environmental Sciences Group
Research Triangle.Park, North Carolina 27709
Abstract
A large amount of the earth's crust is composed of rock containing
mineral fibers which resemble asbestos to varying degrees in their
physical and chemical properties. Consequently, such materials are
likely to be encountered inadvertently during the extraction of various
ores, the extraction of rock for commercial purposes, and even from rock
moving operations encountered during highway construction, and the like.
Because the air and water may become contaminated by these fibers,
it is of interest from the standpoint of environmental protection to know
how the biological effect of such material compares with that of
asbestos. Consequently, a study has been instituted by EPA to
investigate the relative biological potency of such materials. The
project is being approached on both in vivo and in vitro levels. The
minerals being studied at the outset are fibrous ampriboles from a
taconite mine, but it is the intent to broaden these studies as soon as
possible. The animal studies are being conducted in pathogen-free rats
by intratracheal instillation (with and without interacting organic
carcinogens) and by intrapleural injections. The end points are tumor
induction and other chronic diseases. Attention is also being given to
early pathogenic sequences.
The in vitro studies consist of red cell lysis, pulmonary macrophage
systems, and~various biological and chemical studies connected with the
influence of these agents on cell membranes and interaction with mutagens
and carcinogens. The prime objective is to compare the biological effect
of the minerals studied to the corresponding asbestos species to
determine the comparative influence of such co-variables as fiber
length, trace element content, surface area, zeta potential, and the
like, on the biological outcome. Thus, the study will relate biological
activity to mineralogical characterization so that generalization can be
made on the basis of such factors.
Key Words: Alveolar macrophages; hemolysis; intrapleural injections;
intratracheal instillation; multinucleated giant cell; PMP I; PMP II;
Polyp.
Preceding page blank
163
L

The hazards for human health associated with the extraction and handling of various
members of the commercial asbestos series are now well known. However, a new issue has
recently come to the forefront of environmental toxicology concerning the possible health
hazard from inhalation or ingestion of fibrous silicate minerals, not asbestos per se,
that contaminate the air and water. Such silicate materials are ubiquitous in the earth's
crust where amphibole-bearing rocks may serve as a potential source for a number of
mineral species, for example, fibers from the cummingtonite-grunerite series, hornblende,
etc.
When the above-mentioned facts became known, there was a tendency to class all of
these materials as "asbestos" and to try to make inferences concerning their potential
health effects in man merely on the basis of supposed analogy to commercial asbestos. We
know now, however, that there is an enormous variation in these materials; some closely
resemble the corresponding asbestos, and others do not. It would be folly, therefore, to
base the threat to human health solely on such a crude determinant. This is particularly
true since, despite the great number of epidemiological and biological studies carried out
with asbestos, much remains to be learned concerning the exact causal mechanisms of the
various lesions attributed to such exposure. For instance, one cannot safely postulate a
common etiological mechanism for the usual lesions of asbestos exposure such as pulmonary
fibrosis, carcinoma of the lung, and mesothelioma, and the possible role of asbestos for
tumors in other locations which at this time is largely unexplored.
Because of these issues, the Environmental Protection Agency (EPA) has taken the
initiative to study these matters to determine if a threat to health exists from non-
asbestos minerals, and if it does, by means of its quantification, to determine how best
to control it on the basis of health benefit versus cost. EPA is conducting a study of
the relative pathogenic potential of such minerals compared to asbestos, silica, and other
particulate substances of known toxicity. The prime purpose of these experiments is to
relate biological effects to the physiochemical properties of the minerals. Beginning
with the convening of an advisory committee, the following approach evolved, which
includes mineralogical as well as biological studies.
Mineralogical Studies
Intensive study was made from 50 large rock specimens removed from a taconite mine.
After preliminary lithological examinations, two of these were selected for employment in
biological experiments, which are designated as PMP I and PMP II. Fibers were separated
from the rock by such means as mechanical vibration, hand cobbing, air jet milling,
spinning, and riffling. The final specimens were subjected to a detailed analysis by
means of optical and electron microscopy, x-ray emission spectroscopy, and x-ray
diffraction. Computations of surface area and determination of extractable organics were
made. Comparisons were also made an the basis of the above parameters with UICC amosite
(fibrous grunerite) and airborne material collected in the vicinity of the mine and the
ore processing plant. On the basis of the above measurements, a decision was made to
prepare a large amount of this material suitable for biological experimentation.
Figures 1 through 8 and Tables I-III illustrate various mineralogical characteristics
of the samples chosen from the mine for biological studies, as well as samples from the
airborne material in the vicinity of the mine and ore-processing area. Figures 1 and 2
represent electron micrographs of air samples from mine and processing areas respectively.
The chemical analysis of air samples revealed that in addition to magnetite and
quartz particles there were predominantly two other types of minerals in both areas. The
electron microscope x-ray analysis revealed the presence of Mg, Si, Ca, Mn, and Fe in one
sample (fig. 3), whereas the second sample contained only Mg, Si, and Fe (fig. 4). Data
from a careful analysis of size distribution of the air samples are presented in Table 1,
showing two samples from each of the processing and mine areas. The majority of the
particles in both areas were found to be less than 5 pm in length and less than 1 pm in
diameter. A small percentage of particles were between 5 and 10 pm in length, with
varying diameters. Air samples from the processing areas contained 66 to 70 percent
fibers with diameters less than 0.5 pm as compared to 52 to 55 percent in the mine area.
This may suggest that further fibrillation of the rock occurs during the processing.
164

.
Figure 1. Air sample from mine area
showing long and straight
fibers (10,000x).
Figure 2. Air sample from the area
of processing plants also
showing long and straight
fibers (10,000x).
z /z
®
®
En 00170 Ca Q17O3!
165
Figure 3. Electron microscope x-ray
spectra of air sample
indicating the presence
of Mg, Si, Ca, Mn, and Fe.

Figure 4. Electron microscope x-ray spectra of air sample
indicating the presence of Mg. Si, and Fe.
Table 1. Sumnary data of size distribution of mineral fibers in ambient air samples.
- - - - - - - - - Lengths by Percent Number in Microns - - - - - - - - -
<1 1-5 5-10 >10 Total
Air Sample No. 1
<0.50 9 71 5 0
0.51-1.00 0 12 2 0
>1.00 1 0 0 0
Total 10 83 7 0 100
-93% 7%
+ -
Air Sample No. 2
<0.50 8 66 2 1
0.51-1.00 0 13 1 0
>1.00 0 2 6 1
Total 8 81 9 2 100
89% . 11% 1
f .
Air Sample No. 3
<0.50 5 55 2 0
0.51-1.00 0 21 4 0
>1.00 0 4 8 1
Total 5 80 14 1 100
85% . 15%
Air Sample No. 4
<0.50 9 52 5 0
0.51-1.00 0 21 3 0
>1.00 0 3 5 2
Total 9 76 13 2 100
85% 15%
Below 5 um
Diameter by Percent Number in Microns
166
Above 5 Wn

CS
Figure 5. Electron micrograph of PMP I
showing long and straight
fibers with acicular
particles (1000x).
Figure 6. Electron micrograph ~of PMP II
indicating long and straight
fibers and particles (1000x).
The electron microscope x-ray emission spectra of the fibers collected from the two
rock samples revealed the presence of Mg, Si, Ca, Mn, and Fe on PMP I (fig. 7); and Mg,
Si, and Fe on PMP II (fig. 8). The size distribution of the samples is given in Tables 2
and 3. The data indicate that the majority of the fibers are less than 5 pm in length and
less than 0.5 pm in diameters in both samples.
Figure 7. Electron microscope x-ray
spectra of PMP I showing
the presence of Mg, Si,
Ca, Mn, and Fe.
N
Q
a
167 ~
g
~
w

Figure 8. Electron microscope x-ray
spectra of PMP II showing
the presence of Mg. Si,
and Fe.
Table 2. Size distribution of PMP I sample.
- - - - - - - - - - - - - Lengths in Microns (lun) -------------
0.00 - 0.50 0.51 - 1.00' 1.01 - 5.00 5.01 - 10.00 10.01 - 25.00 Total
0.00 - 0.50 1.47 8.09 68.38 2.94 0.73 81.61
0.51 - 1.00 0.00 0.00 5.88 2.94 0.00 8.82
1.01 - 2.00 0.00 0.00 4.41 0.73 0.73 5.87
2.01 - 5.00 0.00 0.00 0.00 0.00 2.94 2.94
5.01 - 10.00 0.00 0.00 0.00 0.00 0.73 0.73
88.23 -- 11.74 99.97
Below 5 um Above 5 ym
Diameter by Percent Number in Microns
Table 3. Size distribution of PMP-2 sample.
Lengths by Percent Number in Microns
<1 1- 5 5- 10 10 - 15
0.00 - 0.50 27.06 41.53 0 0
0.51 - 1.00 0 18.01 5.50 1.80
>1.00 - 10 0 0.80 3.90 1.80
27.06 60.34 9.40 3.60
.-- 87% -. «-~ 13% -+
Be1ow 5 um Above 5 1¢a
Diameter by Percent Number in Microns
168

Figure 9. Fibrous grunerite (UICC amosite)
showing the general shape of the
particle which is long and
straight (1000x).
Sim-e-the air samples and the rock samples seem to be representative of the grunerite
Tamiiy, a fibrous grunerite, namely UICC standard reference amosite, with known biological
properties, was selected as a possible control for the studies, and characterized. The
electron microscope x-ray analysis of amosite indicates the presence of Mg, Si, and Fe
(fig. 10). Size distribution data for this material are presented in Table 4. Eighty-
seven percent of the fibers were found to be less than 5 Nm in length and 1.5 Nm in
diameter.
I
V
Figure 10. Electron microscope x-ray
spectra of fibrous grunerite
(UICC amosite) indicating the
presence of Mg, 51, and Fe.
En Qi.IU Ca =7Q39
Table 4. Size distribution data of UICC amosite by IITRI method.
- - - - - - - Lengths Distribution (by percent number), in Microns - - - - - - -
0.2-0.5 0.5-1 1-2 2-5 5-10 10-25 25-50 50-100 100-200 Total
0.00-1.10 15.90 3.48 1.64 1.80 0.57 0.20 -- -- -- 23.39
0.10-0.40 8.69 13.49 18.24 16.40 5.16 1.68 0.41 0.20 0.01 64.28
0.40-1.50 -- -- 2.54 4.75 1.31 1.84 2.69 0.20 -- 12.93
87% 7%
Diameter by Percent Number in Microns
169
~
6%

The air samples, ttie fibers obtained from rocks, and amosite fibers were examined by
electron microscope for their general shape. All samples contained straight and long
fibers and acicular particles (figs. 5, 6, 9). These photographs are not representative
of the size distribution.
Biological Studies
Toxicity evaluations are proceeding both in vivo and in vitro. Whole animal experi-
ments are being carried out to determine the comparative ef e~ ct of the above-mentioned
mineral fibers in inducing lesions such as pulmonary fibrosis, lung cancer, and pleural
mesothelioma. Basically, a comparison between a test amphibole of the cummingtonite-
grunerite family, UICC amosite, and an inert particle is intended. These studies are
being conducted in Fisher 344 pathogen-free rats during their life span. The particles
are administered to the animals by intratracheal instillation and intrapleural injections.
In vitro studies are conducted on sheep blood erythrocytes and rabbit alveolar
macropFages. The cytotoxicity is evaluated by quantitation of red cell hemolysis and cell
death respectively. -
In Vivo Studies
The doses for the intratracheal instillations were determined by an initial range-
finding study. Several doses of the particulates were administered to the animals and the
highest tolerated dose was determined. Two series of intratracheal studies are planned.
Innoculation of the animals in the first series is complete. The second series will be
initiated in the near future.
Chronic Intratracheal Testing of PMP Amphibole
The first series will determine whether the particles alone cause significant toxicity
to animals. The regimen for this series is as follows:
Series I: Unknown Sample - PMP I Amphibole ........600 animals
Asbestos Control - UICC Amosite..........200 animals
Negative Control - Saline and Gel ........ 200 animals
Chronic Interaction Studies by Intratracheal Instillations
The purpose of the second series is to determine whether the particles will interact
with a known carcinogen to produce a higher incidence of tumors. A knpwn amount of
benzo(a)pyrene (BaP) will be coated on the particles to compare the synergistic effect of
the carcinogen with amosite, the test amphibole, and hematite. The regimen of this series
is as follows:
Series II: PMP I Amphibole + Bap ....................300 animals
UICC Amosite + BaP .......................300 animals
Iron Oxide + BaP .........................300 animals
PMP I Amphibole ..........................200 animals
Iron Oxide ...............................200 animals
BaP ......................................200 animals
Chronic Intrapleural Testing of PMP Particles
Intrapleural studies employing 20 mg of particles injected once into the pleural
cavity are being carried out as follows:
Series III: Unknown Sample - PMP I Amphibole......... 150 animals
Asbestos Control - UICC Amosite.......... 150 animals
Negative Control - Saline ................150 animals
170

Ip addition to the lifetime experiments, exploration of the pathological sequences
induced by these materials in the lung is in progress by experiments in which sequential
sacrifices are being carried out. Figures 11 and 12 demonstrate epithelial polyps and
fiber-containing giant cells observed in the parenchyma of rats treated with 12 weekly
Injections of 1 mg of amosite or the test sample PMP I, 50 days after the last innocula-
tion. The polyps essentially consist of several multi-nucleated giant cells covered with
columnar epithelium.
Figure 11. Epithelial polyps observed in the bronchi (250x).
Figure 12. Multinucleated giant cell containing fibers (1000x).
N
~
171 W
~
~
J

In Vitro Studies
The second part of the biological studies consists of in vitro investigation to
determine cytotoxicity of the particles. Two techniques are empTed, namely, sheep
erythrocyte hemolysis and rabbit alveolar macrophage destruction. A comparison was made
between several commercial asbestos samples of known biological properties, PMP I and non-
fibrous grunerite. The data presented in figure 13 suggest that the amphiboles are not as
hemolytic as chrysotile fibers, requiring large doses to achieve 50 percent hemolysis.
Among the amphiboles, anthophyllite, PMP I, and tremolite are similar in their effect.
Crocidolite and amosite seem to be less hemolytic. In contrast, non-fibrous grunerite is
non-hemolytic. In the rabbit alveolar macrophage study, amosite and PMP I caused marked
depression of cellular viability, whereas non-fibrous grunerite showed no significant
change in cellular viability (fig. 14). The sample PMP II is not yet tested.
A second advisory committee was convened to consider further investigations to
increase our understanding of the mechanisms of mineral interactions with the biological
systems. It was the opinion of the committee that the comparative study of minerals
should be started as soon as possible. On the basis of the existing data, produced by
different laboratories throughout the world, the problem of contamination of the
environment with inorganic fibers may pose a significant health threat. Indeed, it may
shed significant light on existing problems, e.g., asbestos in potable water supplies,
asbestos released from degraded asbestos cement water pipes, natural sources, etc.
The selection of minerals and bioassays are as follows: fibrous and non-fibrous
grunerite will be collected from different geological localities and their biological
properties will be compared. The careful mineralogical analysis and bioassays may
indicate whether there is some influence in terms of the crushing process that may create
new fiber surfaces not present when communiting materials from other areas.
100
N
}
80
QJ
2
= 60
~
40
20
0
0 CHRYSOTILE CROCIDOLITE
p (RHODESIA-UICC)
TREMOLITE (INDIA)
V (S. AFRICA-UICC)
GRUNERITE
PMP (NON FIBROUS)
O ANTHOPHYLLITE
(S. AFR ICA-UICC)
AMOSITE
(S. AFRICA-UICC)
I
I
p....q_..~. ~-..q
0.01 0.02 0.05 0.10 0,20 0.50 1 2 5
CONCENTRATION (mg/ml)
10
20
Figure 13. Hemolysis of sheep erythrocytes by various minerals.
172
