Laboratory simulation of periglacial solifluction: Significance of porewater pressures, moisture contents and undrained shear strengths during soil thawing

Charles Harris, Michael C. R. Davies and Jean‐Pierre Coutard

Permafrost and Periglacial Processes, 1995, vol. 6, issue 4, 293-311

Abstract: Laboratory simulation of periglacial solifluction in two natural soils, one a sandy silt, the other a gravelly silty sand, was undertaken on a 12° slope in a thermally controlled 5 m square chamber. Soil freezing and thawing took place from the top downwards in an open hydraulic system. Frost heaving and surface downslope movements were much greater in the silt‐rich soil than in the sandy soil. In both cases, solifluction took place during the thaw period. At any given depth, porewater pressures rose rapidly immediately following soil thaw, and were generally positive for several days, though not in excess of hydrostatic pressure. Soil moisture contents following thaw exceeded the liquid limit and measured in situ undrained shear strengths were low, ranging between 0.8 kPa near the surface and 9.0 kPa at depth. Conventional slope stability analyses based on total stress and effective stress conditions indicated that the thawing slope was not susceptible to rapid failure. It was concluded that the observed soil displacements represent post‐thaw strain when soil moisture contents were high and Theological properties were intermediate between those of a viscous fluid and a plastic creeping solid. Des expériences de solifluxion périglaciaire ont été réalisées avec deux sols naturels, un de limon sableux et l'autre de sable limoneux et graveleux. Elles ont été entreprises sur une pente de 12°, dans une chambre climatique carrée de 5 m de cǒté. Les gels et les dégels se sont propagés depuis la surface dans des conditions de système hydraulique ouvert. Le soulèvement dǔ au gel et les mouvements de solifluxion ont été beaucoup plus importants dans le sol riche en limon que dans le sol sableux. Dans les deux cas, la solifluxion s'est produite pendant la période de dégel. A toutes les profondeurs, la pression d'eau dans les pores a augmenté rapidement immédiatement après le dégel et est restée positive pendant

Date: 1995
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Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:6:y:1995:i:4:p:293-311

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