SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 45:568-573 (1981)
© 1981 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Bresson, L.-M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Bresson, L.-M.
Agricola
Right arrow Articles by Bresson, L.-M.

Ion Micromilling Applied to the Ultramicroscopic Study of Soils1

L.-M. Bresson2

ABSTRACT

The electron transmission microscopic (TEM) study of undisturbed soil materials requires the preparation of thin sections of about 1,000Ä thick. This seems to be possible only by ion micromilling.

This thinning technique necessitates particular precautions due to the fragility of permeated soil materials. The resins generally used for the making of thin sections are suitable as long as their polymerization is very good. Handling of the sample must be done under a stereomicrosocope with great care. It may prove useful before bombardment to glue the sample (3 mm in diam, 30 µm in thickness) between two electron microscope grids with a single central hole. The required thickness is reached when small holes appear in the sample. The thickness of the ultrathin sections can be irregular because the thinning rate of the sample varies considerably with its chemical composition, the type of its crystal lattice, and the state of its surface. Therefore, the only areas visible with a TEM appear as halos around holes. Artifacts induced by ion bombardment seem to be negligible compared with those that appear during observation by TEM. The ultrathin sections thus obtained allow the morphology of soil constituents and their ultramicroorganization to be studied at very high magnifications; hence, they are extremely useful for studies of mineral weathering, microstructures, and microfabrics.


NOTES

1 Contribution from the Département des Sols, Faculté des Sciences de l'Agriculture et de l'Alimentation, Université Laval, Québec, G1K 7P4 (Canada). This work was aided by the Comité de Coordination pour la Recherche of this Faculty; special research fund 1-1-04-41-31-20-10.

2 Visiting Professor, now Maitre-Assistant, Département des Sols, Institut National Agronomique Paris-Grignon, 78850 Thiverval-Grignon (France).

Received for publication July 29, 1979. Accepted for publication November 20, 1980.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1981 by the Soil Science Society of America.