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Examination of rock surfaces with the scanning electron microscope

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Publisher’s version / Version de l'éditeur:

Journal of Microscopy, 91 Pt. 3, pp. 203-205, 1970-11-01

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Examination of rock surfaces with the scanning electron microscope

Gillott, J. E.

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0 Journal of Microscopy, Vol. 91, Pt 3, June 1970, pp. 203-205 Received 8 December 1969; revision received 12 January 1970

Short Technical Note

Examination of rock surfaces with the scanning electron

microscope

by J. E. G I L L o TT, Materials Section, Division of Building Research, Nationul Research Coulzcil of Canada, Ottawa

S U M M A R Y

A fracture surface of rock (greywaclze) was examined with the scanning electron microscope prior to, and after, surface etching for successively increasing time intervals in 2 M NaOH at 38°C (100°F). T h e same area of rock was successfully relocated in the microscope so that the effect of the alkali upon minerals and micro- structure could be observed by direct comparison of micrographs. Layer-structure silicates showed exfoliation.

A fracture surface of rock (greywacke) was examined with the scanning electron microscope, prior to, and following successively increasing time intervals in 2 M NaOH at 38°C (100°F). As rock is non-conducting, a thin metal coating is

required to prevent the build-up, on the surface, of an electric charge that would otherwise cause a serious loss inresolution. Aluminium coating was used because it is rapidly removed by the alkali exposing the bare rock to attack. I n other experiments the rock was not coated and the microscope was operated at a low voltage to minimize charge build-up. Results were generally -less satisfactory with non-coated samples.

A magnification of x 230 was used and a mosaic constructed that covered an area of 3 or 4 mm by 1+ or 2 mm of sample surface. One or more photographs at x 2300 magnification were taken in each frame of the mosaic as well as a small number of photographs at higher magnification in order to study the effect on the

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fabric of the rock of increasing periods of time in alkali (Gillott, 1969). This could

be accomplished most directly by observing the same area of sample before and after it had been immersed in 2 M NaOH.

I

I n the first experiments two orthogonal lines were scratched on the sample sur- face. T h e etching action of the alkali tended to obscure these markings, however, and in later experiments a piece of gold leaf was attached to the sample. Modified sample holders were made. T h e side of the stub was threaded and a screw-on cap constructed with a rim that overlapped the outermost portion of the sample. When the cap was screwed down over the sample the rim held both the gold leaf and sample in place. The cap and sample holder stub were made of stainless steel

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J.

E. Gillott

unit. After a specified time this unit was removed from alkali and the sample was re-examined on the microscope; the same area of sample could be relocated with- out too much difficulty.

Fig. 1 presents views of a fracture surface of untreated rock and views of the same area after 1 month in 2 M NaOH at 38°C (100°F). Fig. l(a and b) represent one frame each of the respective mosaics; Fig. l(c and d) are enlargements of the central portion of each. I n the lower-power magnification there are feldspars,

quartz and mica-type minerals. Comparison shows that many of the minerals are L

b

relatively unaffected by the alkali after 1 month though the layer-structure silicates show exfoliation. This is most clearly seen in the views taken at higher v magnification (c and d). T h e significance of this work to the understanding of the mechanism of alkali-aggregate reaction involving greywackes and phyllites (Duncan & Swenson, 1969) will be described in detail elsewhere.

Fig. 1. Scanning electron micrographs of selected area of greywacke be- fore and after treatment with alkali, talcen at 20 kV accelerating potential on a Cambridge Stereoscan Mk I1 scanning electron microscope. (a, c) Untreated; (b, d) 1 month 2 M NaOH at 38°C.

A C K N O W L E D G M E N T S

T h e author wishes to express sincere thanks to G. Seibel and A. Rezanowich, Pulp and Paper Research Institute of Canada, for technical help and suggestions. This paper is a contribution from the Division of Building Research, National Research Council of Canada, and is published with the approval of the Director of the Division.

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SEM of rock sztrfaces

References

Duncan, M.A.G. & Swenson, E.G. (1969) Investigation of concrete expansion in Nova Scotia.

J . Ass. Prof. Engrs Nova Scotia, 10, 16.

Gillott, J.E. (1969) Study of the fabric of fine-grained sediments with the scanning electron microscope. J. sedim. Petrol. 39, 90.

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Figure

Fig.  1 presents  views  of  a fracture  surface  of  untreated  rock  and views  of the  same area after  1 month in  2  M  NaOH at 38°C (100°F)

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