Geological Hazards in the UK: Their Occurrence, Monitoring and Mitigation – Engineering Group Working Party Report
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The UK is perhaps unique globally in that it presents the full spectrum of geological time, stratigraphy and associated lithologies within its boundaries. With this wide range of geological assemblages comes a wide range of geological hazards, whether they be geophysical (earthquakes, effects of volcanic eruptions, tsunami, landslides), geotechnical (collapsible, compressible, liquefiable, shearing, swelling and shrinking soils), geochemical (dissolution, radon and methane gas hazards) or georesource related (coal, chalk and other mineral extraction). An awareness of these hazards and the risks that they pose is a key requirement of the engineering geologist.
The Geological Society considered that a Working Party Report would help to put the study and assessment of geohazards into the wider social context, helping the engineering geologist to better communicate the issues concerning geohazards in the UK to the client and the public. This volume sets out to define and explain these geohazards, to detail their detection, monitoring and management and to provide a basis for further research and understanding.
Chapter 7 Quick clay behaviour in sensitive Quaternary marine clays – a UK perspective
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Published:June 09, 2020
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CiteCitation
David Peter Giles, 2020. "Chapter 7 Quick clay behaviour in sensitive Quaternary marine clays – a UK perspective", Geological Hazards in the UK: Their Occurrence, Monitoring and Mitigation – Engineering Group Working Party Report, D. P. Giles, J. S. Griffiths
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Abstract
The term quick clay has been used to denote the behaviour of highly sensitive Quaternary marine clays that, due to post depositional processes, have the tendency to change from a relatively stiff condition to a liquid mass when disturbed. On failure these marine clays can rapidly mobilise into high velocity flow slides and spreads often completely liquefying in the process. For a clay to be defined as potentially behaving as a quick clay in terms of its geotechnical parameters it must have a sensitivity (the ratio of undisturbed to remoulded shear strength) of greater than 30 together with a remoulded shear strength of less than 0.5 kPa. The presence of quick clays in the UK is unclear, but the Quaternary history of the British islands suggests that the precursor conditions for their formation could be present and should be considered when undertaking construction in the coastal zone.
- Cenozoic
- engineering properties
- Europe
- failures
- flocculation
- geologic hazards
- Glasgow Scotland
- Great Britain
- Holocene
- landslides
- marine sediments
- mass movements
- mechanical properties
- mitigation
- natural hazards
- Quaternary
- quick clay
- risk management
- Scotland
- sediments
- sensitive clays
- soil mechanics
- United Kingdom
- Western Europe
- Grangemouth Scotland
- Clyde Sea Loch