TECHNICAL PAPERS
Sep 1, 1993

Creep Behavior of Saline Fine‐Grained Frozen Soil

Publication: Journal of Cold Regions Engineering
Volume 7, Issue 3

Abstract

Creep tests were conducted on a fine‐grained frozen soil at different salinities ranging from 0 to 20 ppt (parts per thousand), at temperatures between −5°C and −17°C and at two total water contents of around 34% and 52%. The test results indicated that the presence of salinity in the pore water considerably increases the creep strain rates of the frozen soil. This type of behavior is more prominent under high creep‐stress conditions. Unique relationships are found to exist between secondary strain rate and time, initial strain rate and relative creep load (creep stress to peak strength ratio), and initial strain and relative creep load. The relationships developed are not affected by the different salinity, temperature, and total water content conditions of the frozen soil. Similar creep behavior was observed when the frozen soil was subjected to similar relative creep loads under various temperature and salinity conditions. The results obtained in this study suggest a possible way of generalizing the creep characteristics of a frozen soil subjected to changing salinities and temperatures.

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References

1.
Hivon, E. G., and Sego, D. C. (1991). “Distribution of saline permafrost in the Northwest Territories.” 44th Canadian Geotech. Conf., Canadian Geotechnical Society, Calgary, Alberta, Canada, 1(38) 1–10.
2.
Jessberger, J. L., Ebel, W., and Jordan, P. (1985). “Temperature dependent strength and creep behavior of frozen saline sand.” 4th Int. Symp. on Ground Freezing, Balkema Publishers, Rotterdam, The Netherlands.
3.
Mellor, M., and Cole, D. M. (1982). “Deformation and failure of ice under constant stress or constant strain rate.” Cold Sci. and Technol., 5, 201–219.
4.
Nixon, J. F., and Lem, G. (1984). “Creep and strength testing of frozen saline fine‐grained soils.” Can. Geotech. J., 21, 518–529.
5.
Ogata, N., Yasuda, M., and Kataoka, T. (1983). “Effects of salt concentration on strength and deformation behavior of artificially frozen soils.” Cold Regions Sci. and Technol., 8(2), 139–153.
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Ting, J. M. (1983). “On the nature of the minimum creep rate‐time correlation for soil, ice and frozen soil.” Can. Geotech. J., 20, 176–182.
7.
Wijeweera, H. (1990). “Creep and strength behavior of fine‐grained frozen soils,” PhD thesis, University of Calgary, Alberta, Canada.
8.
Wijeweera, H., and Joshi, R. C. (1992). “Temperature‐independent relationships for frozen soils.” J. Cold Regions Engrg., ASCE, 6(1), 1–21.

Information & Authors

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Published In

Go to Journal of Cold Regions Engineering
Journal of Cold Regions Engineering
Volume 7Issue 3September 1993
Pages: 77 - 89

History

Received: Jun 8, 1992
Published online: Sep 1, 1993
Published in print: Sep 1993

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Authors

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H. Wijeweera
Res. Assoc., Dept. of Civ. Engrg., Univ. of Calgary, Alberta, Canada T2N 1N4
R. C. Joshi, Fellow, ASCE
Prof., Dept. of Civ. Engrg., Univ. of Calgary, Alberta, Canada, T2N 1N4

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