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Gelifluction and Thixotropy of Maritime Antarctic Soils: Small‐Scale Measurements with a Rotational Rheometer
Author(s) -
Sun Benhua,
Dennis Paul G.,
Newsham Kevin K.,
Hopkins David W.,
Hallett Paul D.
Publication year - 2016
Publication title -
permafrost and periglacial processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.867
H-Index - 76
eISSN - 1099-1530
pISSN - 1045-6740
DOI - 10.1002/ppp.1886
Subject(s) - geology , thixotropy , rheometer , scale (ratio) , geotechnical engineering , permafrost , geomorphology , oceanography , rheology , materials science , composite material , geography , cartography
Gelifluction, thixotropy and yield stress were measured from < 5 g soil samples taken from Signy, Alectoria, Greenwich, Wiencke and Livingston islands in the maritime Antarctic using a temperature‐controlled rotational rheometer. The small sample size that this method permitted is compatible with sampling from sensitive sample locations. An oscillating 10 Pa shear stress was applied to samples at ‐0.5 kPa water potential. Two freeze‐thaw cycles had temperature ramps from 5°C to ‐10°C over 2 h, followed by ‐10°C to 5°C over 2 h and finally at 5°C for 1 h. At freezing onset, the shear modulus, G , dropped to 4–50 per cent of thawed G , with no differences between locations. At thawing onset, G dropped to 8–32 per cent of thawed G , with significant differences between locations ( P < 0.001). Thixotropy was then measured by applying a 2 kPa oscillating shear stress for 10 min, followed by relaxation at 10 Pa for 2 h. The increased shear stress caused G to drop to less than 8 per cent of the pre‐stressed value, with no difference between locations. After 0.1 and 2 h, G was 18–65 per cent and 31–82 per cent of the pre‐stressed value, respectively. A shear ramp determined yield stresses ranging from 494–2217 Pa. These findings demonstrate the potential risk of more frequent freeze‐thaw cycles or the occurrence of thawed soil to the stability of polar soils. Gelifluction through more frequent freeze‐thaw cycles could result in increased slope movement, whereas thixotropy caused by trampling of thawed soils could exacerbate mechanical damage of surface soils. Copyright © 2016 John Wiley & Sons, Ltd.