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Thermal stress weathering and the spalling of Antarctic rocks

Authors :
Lamp, J. L.
Marchant, D. R.
Mackay, S. L.
Head, J. W.
Source :
Journal of Geophysical Research - Earth Surface; January 2017, Vol. 122 Issue: 1 p3-24, 22p
Publication Year :
2017

Abstract

Using in situ field measurements, laboratory analyses, and numerical modeling, we test the potential efficacy of thermal stress weathering in the flaking of millimeter‐thick alteration rinds observed on cobbles and boulders of Ferrar Dolerite on Mullins Glacier, McMurdo Dry Valleys (MDV). In particular, we examine whether low‐magnitude stresses, arising from temperature variations over time, result in thermal fatigue weathering, yielding slow crack propagation along existing cracks and ultimate flake detachment. Our field results show that during summer months clasts of Ferrar Dolerite experience large‐temperature gradients across partially detached alteration rinds (>4.7°C mm−1) and abrupt fluctuations in surface temperature (up to 12°C min−1); the latter are likely due to the combined effects of changing solar irradiation and cooling from episodic winds. The results of our thermal stress model, coupled with subcritical crack growth theory, suggest that thermal stresses induced at the base of thin alteration rinds ~2 mm thick, common on rocks exposed for ~105years, may be sufficient to cause existing cracks to propagate under present‐day meteorological forcing, eventually leading to rind detachment. The increase in porosity observed within alteration rinds relative to unaltered rock interiors, as well as predicted decreases in rind strength based on allied weathering studies, likely facilitates thermal stress crack propagation through a reduction of fracture toughness. We conclude that thermal stress weathering may be an active, though undervalued, weathering process in hyperarid, terrestrial polar deserts such as the stable upland region of the MDV. Antarctic dolerite clasts experience large temperature gradients and fast fluctuations in surface temperatureThermal fatigue weathering likely contributes to the spalling and flaking of dolerite boulders in AntarcticaAlteration rinds on dolerite clasts allow for local weakening and subcritical crack propagation under thermal stress

Details

Language :
English
ISSN :
21699003 and 21699011
Volume :
122
Issue :
1
Database :
Supplemental Index
Journal :
Journal of Geophysical Research - Earth Surface
Publication Type :
Periodical
Accession number :
ejs42564920
Full Text :
https://doi.org/10.1002/2016JF003992