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Articles | Volume 10, issue 5
Articles | Volume 10, issue 5
https://doi.org/10.5194/se-10-1685-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-10-1685-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 10, issue 5
Research article
 | 
11 Oct 2019
Research article |  | 11 Oct 2019

Subsurface characterization of a quick-clay vulnerable area using near-surface geophysics and hydrological modelling

Silvia Salas-Romero, Alireza Malehmir, Ian Snowball, and Benoît Dessirier

Supplement

https://doi.org/10.5194/se-10-1685-2019-supplement

Data sets

Land reflection seismic, hydrogeological and magnetic study of an area prone to quick-clay landslides in southwest Sweden. Swedish National Data Service. Version 1.0. (2019) Silvia Salas Romero, Alireza Malehmir, Ian Snowball, and Benoît Dessirier (Uppsala University, Department of Earth Sciences) https://doi.org/10.5878/acbv-h350

Modeled subsurface interfaces of an area prone to quick-clay landslides in southwest Sweden. Swedish National Data Service. Version 1.0. (2019) Silvia Salas Romero, Alireza Malehmir, Ian Snowball, and Benoît Dessirier (Uppsala University, Department of Earth Sciences) https://doi.org/10.5878/md19-qw71

Hydrogeological modeling of an area prone to quick-clay landslides in southwest Sweden. Swedish National Data Service. Version 2.0. (2019) Silvia Salas Romero, Alireza Malehmir, Ian Snowball, and Benoît Dessirier (Uppsala University, Department of Earth Sciences) https://doi.org/10.5878/r1kq-0f98

Magnetic study of an area prone to quick-clay landslides in southwest Sweden. Swedish National Data Service. Version 1.0. (2019) Silvia Salas Romero, Alireza Malehmir, Ian Snowball, and Benoît Dessirier (Uppsala University, Department of Earth Sciences) https://doi.org/10.5878/a8xn-fc97

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Short summary
Land–river reflection seismic, hydrogeological modelling, and magnetic investigations in an area prone to quick-clay landslides in SW Sweden provide a detailed description of the subsurface structures, such as undulating fractured bedrock, a sedimentary sequence of intercalating leached and unleached clay, and coarse-grained deposits. Hydrological properties of the coarse-grained layer help us understand its role in the leaching process that leads to the formation of quick clays in the area.
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