Morphosedimentary evolution of the Flemish coastal plain since Antiquity : contribution of georadar surveys to geoarchaeology ; Evolution morphosédimentaire de la plaine maritime flamande depuis l'Antiquité : apport des prospections géoradar à la géoarchéologie

Ground-penetrating radar (GPR) is a non-destructive geophysical prospecting tool used to image the finest discontinuities of the underground where the soil is not too conductive. GPR equipment was acquired in 2020 by the Oceanology and Geosciences Laboratory (LOG), which gave rise to bachelor's and master's internships supervised as part of this thesis, as well as academic and industrial collaborations. The first part of the results presented in this memoir is a summary of the surveys carried out on a variety of targets to test the method. GPR gives excellent results on wind-blown sands, and m... Mehr ...

Verfasser: Ouchaou, Rachid
Dokumenttyp: doctoralThesis
Erscheinungsdatum: 2023
Verlag/Hrsg.: HAL CCSD
Schlagwörter: Gpr / Sedimentary environments / Estuary / Holocene / Land reclamation / Géoradar / Environnements sédimentaire / Estuaire / Holocène / Poldérisation / [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Sprache: Französisch
Permalink: https://search.fid-benelux.de/Record/base-27477484
Datenquelle: BASE; Originalkatalog
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Link(s) : https://theses.hal.science/tel-04576242

Ground-penetrating radar (GPR) is a non-destructive geophysical prospecting tool used to image the finest discontinuities of the underground where the soil is not too conductive. GPR equipment was acquired in 2020 by the Oceanology and Geosciences Laboratory (LOG), which gave rise to bachelor's and master's internships supervised as part of this thesis, as well as academic and industrial collaborations. The first part of the results presented in this memoir is a summary of the surveys carried out on a variety of targets to test the method. GPR gives excellent results on wind-blown sands, and makes it possible to reconstruct the evolution of the coastal dunes affected by climate change. Examples of very-high resolution architectures are provided on the Slack and Pilat dunes. The combined use of different GPR antennas allows describing the mechanisms of sand erosion and deposition, from the scale of seasonal events to that of dune construction on a millennial scale. The backshore area is also explored. The Flemish coastal plain contains sandbodies of kilometer extension, partly buried under the silt of the polders, and which are strategic both for water resources and for the diversity of natural environments. One of the best known is the Ghyvelde fossil dune, an area managed by the Coastal Conservatory. The GPR profiles carried out on the Ghyvelde dune make it possible to image a few meters below the dune a sandy unit of marine or estuarine origin. The polders themselves constitute a target, against all expectations given the clayey and conductive component of these lands. By previously stripping the topsoil, the GPR signal penetrates sufficiently (4m) to image the last channels that drained the plain before it dried up. Finally, two examples show the potential of GPR in geological studies of deeper sedimentary or rocky layers. In the Brussels sands of the Leuven region (Belgium), a penetration depth of more than 30 meters was obtained with a low frequency antenna, making it possible to reconstruct the geometry of ...