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Identifying landslide preconditions in Swedish quick clays—insights from integration of surface geophysical, core sample- and downhole property measurements

Salas-Romero, Silvia (författare)
Uppsala universitet,Uppsala University,Geofysik
Malehmir, Alireza (författare)
Uppsala universitet,Uppsala University,Geofysik
Snowball, Ian (författare)
Uppsala universitet,Uppsala University,Geofysik,Naturresurser och hållbar utveckling
visa fler...
Lougheed, Bryan C. (författare)
Uppsala universitet,Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science,Naturresurser och hållbar utveckling
Hellqvist, Magnus (författare)
Uppsala universitet,Uppsala University,Paleobiologi
visa färre...
 (creator_code:org_t)
2015-09-24
2016
Engelska 19 s.
Ingår i: Landslides. - : Springer Science and Business Media LLC. - 1612-510X .- 1612-5118. ; 13:5, s. 905-923
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Quick-clay landslides are a serious geohazard in Canada, Norway and Sweden. Identification and mapping of quick clays are essential endeavours because the damage caused by an individual landslide can be large and costly, with potentially fatal consequences. We collected geophysical borehole and soil core data from an area prone to quick-clay landslides in southwestern Sweden. Methodologies included in situ and laboratory measurements, providing information about natural gamma radiation, sonic velocities, electrical conductivity, pH, physical grain size, elemental and mineral composition, magnetic properties, cation exchange capacity and fossil content. A stratigraphic thickness of almost 60 m enables us to study quick clays and their host environment in Sweden at unusually high resolution. Results identify the origin and location of reflections in nearby seismic lines and assign physico-chemical properties to the geological units present in the area. We show that coarse-grained layers are sandwiched between marine clays (some of which are quick clays). These layers function as a conduit for relatively fresh water that infiltrates the marine clays and chemically destabilizes them by leaching out their salts. The salinity distribution in the boreholes indicate that the groundwater movement is downwards, through the coarse-grained layer and towards the Göta river. The presence of these materials is important for the development of quick clays, although not a prerequisite. With the help of surface geophysical methods, the location of the coarse-grained layers can be known faster and more economically, which could be relevant for studying the potential for quick-clay landslide occurrence over large areas.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)

Nyckelord

Correlation
Downhole geophysics
Landslide
Physico-chemical properties
Quick clay
Southwestern Sweden
Landslide; Quick clay; Southwestern Sweden; Correlation; Downhole geophysics; Physico-chemical properties

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