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 54:1060-1067 (1990)
© 1990 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Chartres, C. J.
Right arrow Articles by Raupach, M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Chartres, C. J.
Right arrow Articles by Raupach, M.
Agricola
Right arrow Articles by Chartres, C. J.
Right arrow Articles by Raupach, M.

Poorly Ordered Silica and Aluminosilicates as Temporary Cementing Agents in Hard-Setting Soils

C. J. Chartres* and J. M. Kirby

CSIRO Division of Soils, G.P.O. Box 639, Canberra, A.C.T., Australia 2601

M. Raupach

CSIRO Division of Soils, Adelaide, South Australia

*Corresponding author.

ABSTRACT

Hard-setting is an important but poorly understood phenomenon in seasonally wetting and drying soils. This study was conducted to determine the role, if any, of chemical cementing agents in a hard-setting soil. Undisturbed cores from the E horizon of an Aeric Albaqualf were leached in the laboratory with distilled water, 0.15 M ammonium oxalate (pH 3.0 in darkness) and 2 M NaOH/ethylene glycol. The leachates were analyzed for Si, Al, and Fe and the residual materials by infrared spectroscopy. After drying at 40 °C, tensile, shear, and compressive strengths of the cores were determined. All three reagents caused a total loss of tensile strength and decreased shear strength, but had little effect on compressive strength. Amorphous silica is probably the major cementing agent, but the results also indicate that an imogolite-like aluminosilicate, a feldspathoid mineral, and possibly silica-Fe complexes may play some part in cementation.


NOTES

Contribution from CSIRO Division of Soils.

Received for publication July 6, 1989.


This article has been cited by other articles:


Home page
Soil Sci.Home page
K. J. Kendrick and R. C. Graham
Pedogenic Silica Accumulation in Chronosequence Soils, Southern California
Soil Sci. Soc. Am. J., July 1, 2004; 68(4): 1295 - 1303.
[Abstract] [Full Text] [PDF]




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 © 1990 by the Soil Science Society of America.