Land reflection seismic, hydrogeological and magnetic study of an area prone to quick-clay landslides in southwest Sweden

SND-ID: snd1079-1. Version: 2. DOI: https://doi.org/10.57804/hxj1-8b75

Citation

Creator/Principal investigator(s)

Silvia Salas Romero - Uppsala University, Geosciences orcid

Alireza Malehmir - Uppsala University, Geosciences orcid

Ian Snowball - Uppsala University, Geosciences orcid

Benoît Dessirier - Uppsala University, Geosciences orcid

Research principal

Uppsala University - Department of Earth Sciences rorId

Description

Quick-clay landslides are common geohazards in Nordic countries and Canada. The presence of potential quick clays is confirmed using geotechnical investigations, but near-surface geophysical methods, such as seismic and resistivity surveys, can also help identifying coarse-grained materials associated to the development of quick clays.

We present the results of four reflection seismic profiles next to the Göta River in Sweden, along which many quick-clay landslide scars exist. An extensive coarse-grained layer exists in the sedimentary sequence and is interpreted and modeled in a regional context. Hydrological modeling of the coarse-grained layer is performed. Magnetic data are also studied within this investigation.

Four reflection seismic profiles collected in 2013 (line 5 has two parts, cabled geophones and wireless stations).

Data contains personal data

No

Language

Method and outcome

Time period(s) investigated

2018-01-01 – 2018-03-05

Data format / data structure

Data collection
Geographic coverage

Geographic spread

Geographic location: Sweden, Västra Götaland County

Administrative information

Responsible department/unit

Department of Earth Sciences

Topic and keywords

Research area

Earth and related environmental sciences (Standard för svensk indelning av forskningsämnen 2011)

Geoscientific information (INSPIRE topic categories)

Publications

Salas-Romero, S., Malehmir, A., Snowball, I., & Dessirier, B. (2019). Subsurface characterization of a quick-clay vulnerable area using near-surface geophysics and hydrological modelling. Solid Earth, 10(5), 1685–1705.
DOI: https://doi.org/10.5194/se-10-1685-2019

Versions

Version 2. 2025-01-17

Version 2: 2025-01-17

DOI: https://doi.org/10.57804/hxj1-8b75

Data merged: Data from: https://doi.org/10.5878/acbv-h350; https://doi.org/10.5878/md19-qw71; https://doi.org/10.5878/r1kq-0f98; https://doi.org/10.5878/a8xn-fc97

Version 1.0. 2019-01-14

Version 1.0: 2019-01-14

DOI: https://doi.org/10.5878/acbv-h350

Published: 2025-01-17