Document O3Lyj3ojgYzXDn8ZKwV5G273w
Report to: Windsor Mineral Company Windsor, Vermont 05089
Technical Report MA-2401
EXAMINATION OF TALC SAMPLES FOR
WINDSOR MINERAL COMPANY
Submitted by :
Walter C. McCrone A ssociates, Inc. 493 East 31st Street Chicago, Illinois 60616
Gene R. Greiger Principal Investigator
of copie s
PLAINTIFFS EXHIBIT
CAM-305
Ian M. Stewart Manager, Electron Optics Group
21 October 1971
ITA-Ratcliff-001217
Technical Report MA-2401
EXAMINATION OF TALC SAMPLES FOR
WINDSOR MINERAL COMPANY
Summary Three talc samples, identified as 2676-55A, 2676-55B, and 2676-55C,
have been examined for the Windsor Mineral Company with particular empha sis being placed on the fiber content of the m aterials, particularly fibers of the asbestiform minerals.
Of the three samples, A and C were found to contain several fibers of unknown mineralogical types, none of which yielded electron diffraction patterns which would perm it their identification. Several of these fibers ap peared morphologically sim ilar to chrysotile, but no positive identification was possible.
Sample C showed the thinnest plates of talc and on this basis is judged to be the best talc of the three samples.
ITA-Ratcliff-001218
EXAMINATION OF TALC SAMPLES FOR
WINDSOR MINERAL COMAPNY
Introduction Three samples of talc, identified as 2676-55A, 2676-55B, and 2676-55C
were submitted by the Windsor Mineral Company, Windsor, Vermont, for examination by electron microscopy and electron diffraction techniques. In formation was sought on the fiber content of the three samples, in particular the presence of asbestiform m ineral fibers. It was further requested that we compare samples A and B with sample C. For this reason, sample C will be described first.
Results of the Examination Sample 2676-55 C This sample has a very clean appearance with extremely thin plates
of talc and very few pieces of rolled talc. In our examination of this sample we observed two fine fibers, neither of which could be positively identified since they did not yield diffraction patterns but one of which did have a m or phology sim ilar to chrysotile. It should be pointed out, however, that we observed sim ilar morphology in several m inerals. No amphibole particles were observed. The plate-size range in the portion of the sample analyzed in the transm ission electron microscope is approximately 1-3 n m.
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ITA-Ratcliff-001219
Sample 2676-55A In this sample, the talc plates appeared to be thicker, and there is a slightly higher percentage of rolled talc plates. We found four fibers, three of which could be classed as suspect on the basis of their morphology, but none of these fibers could be positively identified. Of the three suspect fibers, one has a limited sim ilarity and two have substantial sim ilarity to the morphology of chrysotile, but they could not be identified as this mineral as we were unable to obtain electron diffraction patterns from them. Again we detected no amphiboles although there is slightly more extraneous m aterial than in sample C.
Sample 2676-55B This sample appeared very clean, containing no fine fibers of any type, fewer fine talc particles and no amphiboles. There is very little extraneous m aterial present, and only on one occasion did we find any of the normal de composition products of chlorite or carbonates. The talc plates are not quite as thin as those in sample C but are thinner than those in sample A.
Observations Despite the presence of the two fine fibers in C, this sample appears
to be the best example of talc since it occurs as the thinnest plates. We would place sample B as next best on the basis of plate thickness and sample cleanliness.
The possibility that the suspect fibers found in samples A and B originate from some external source of contamination cannot be precluded.
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ITA-Ratcliff-001220
The fact that these occurred as isolated fibers would tend to indicate external rath er than internal contamination of the source m aterial; internal contamina tion would, in general, tend to yield fibrous bundles or aggregates, and it is unlikely that isolated fibers of the dimensions which we are observing, approximately 20 nm in diam eter, would occur in a natural talc body.
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