Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.

International audience Geophysical survey by of the Pierrelaye-Bessancourt area revealed conductive polygon patterns of 20-30 m diameter detected between 0.5 and 1.7 m depth. The patterns are formed by greenish glauconite and carbonated sand hollows where clay-rich pedological horizons bend downward...

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Published in:Geomorphology
Main Authors: Thiry, Médard, van Oort, Fok, Thiesson, Julien, van Vliet-Lanoë, Brigitte
Other Authors: Centre de Géosciences (GEOSCIENCES), Mines Paris - PSL (École nationale supérieure des mines de Paris), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), Physicochimie et Ecotoxicologie des SolS d'Agrosystèmes Contaminés (PESSAC), Institut National de la Recherche Agronomique (INRA), UFR 918 Terre - environnement - Biodiversité, Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE), Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris), Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE), Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Domaines Océaniques (LDO), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS), Conseil Régional de l'Ile-de-France (CRIdF), Conseil Général du Val d'Oise (CG95), Agence de l'Eau de Seine-Normandie (AESN), Syndicat Interdépartemental pour l'Assainissement de l'Agglomération Parisienne (SIAAP)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
Ice
Online Access:https://minesparis-psl.hal.science/hal-00818938
https://minesparis-psl.hal.science/hal-00818938/document
https://minesparis-psl.hal.science/hal-00818938/file/Thiry_al_Pierrelaye_Geomorphology_preprint.pdf
https://doi.org/10.1016/j.geomorph.2013.04.027
id ftecolephe:oai:HAL:hal-00818938v1
record_format openpolar
institution Open Polar
collection EPHE (Ecole pratique des hautes études, Paris): HAL
op_collection_id ftecolephe
language English
topic periglacial
cryoturbation
soils
geophysical method
electrical mapping
pollution
micromorphology
pedology
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle periglacial
cryoturbation
soils
geophysical method
electrical mapping
pollution
micromorphology
pedology
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Thiry, Médard
van Oort, Fok
Thiesson, Julien
van Vliet-Lanoë, Brigitte
Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.
topic_facet periglacial
cryoturbation
soils
geophysical method
electrical mapping
pollution
micromorphology
pedology
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience Geophysical survey by of the Pierrelaye-Bessancourt area revealed conductive polygon patterns of 20-30 m diameter detected between 0.5 and 1.7 m depth. The patterns are formed by greenish glauconite and carbonated sand hollows where clay-rich pedological horizons bend downward, forming narrow tongs extending up to 2-3 m depth. Such structures were interpreted as a buried polygonal ice-wedge network. Geometrical relationships between the lithological units allowed the identification of successive landscape events and a landscape chronology. The sequence started during the Saalian glaciation with (1) development of patterned grounds by thermokarstic cryoturbation; (2) consecutive deflation/erosion during post-permafrost aridity; (3) loess and eolian sand deposits; (4) weathering of the former deposits with development of pedogenic horizons during the Eemian interglacial; (5) recurrent cryoturbation and thermal cracking leading to infolding of the pedogenic horizons during the Pleniglacial optimum (Weichselian); (5) finally erosion that levelled the periglacial microreliefs, leading to the modern landscape. In this agricultural area, urban waste water has been spread and has led to high levels of metal pollution in the surface horizons of the soils. The polygonal cryogenic structures have major impacts on soil hydrology and dispersion/distribution of heavy metals toward the geological substrate.
author2 Centre de Géosciences (GEOSCIENCES)
Mines Paris - PSL (École nationale supérieure des mines de Paris)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
Physicochimie et Ecotoxicologie des SolS d'Agrosystèmes Contaminés (PESSAC)
Institut National de la Recherche Agronomique (INRA)
UFR 918 Terre - environnement - Biodiversité
Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE)
Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris)
Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE)
Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)
Domaines Océaniques (LDO)
Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS)
Conseil Régional de l'Ile-de-France (CRIdF), Conseil Général du Val d'Oise (CG95), Agence de l'Eau de Seine-Normandie (AESN), Syndicat Interdépartemental pour l'Assainissement de l'Agglomération Parisienne (SIAAP)
format Article in Journal/Newspaper
author Thiry, Médard
van Oort, Fok
Thiesson, Julien
van Vliet-Lanoë, Brigitte
author_facet Thiry, Médard
van Oort, Fok
Thiesson, Julien
van Vliet-Lanoë, Brigitte
author_sort Thiry, Médard
title Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.
title_short Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.
title_full Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.
title_fullStr Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.
title_full_unstemmed Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution.
title_sort periglacial morphogenesis in the paris basin: insight from geophysical survey and consequences for the fate of soil pollution.
publisher HAL CCSD
publishDate 2013
url https://minesparis-psl.hal.science/hal-00818938
https://minesparis-psl.hal.science/hal-00818938/document
https://minesparis-psl.hal.science/hal-00818938/file/Thiry_al_Pierrelaye_Geomorphology_preprint.pdf
https://doi.org/10.1016/j.geomorph.2013.04.027
genre Ice
permafrost
wedge*
genre_facet Ice
permafrost
wedge*
op_source ISSN: 0169-555X
Geomorphology
https://minesparis-psl.hal.science/hal-00818938
Geomorphology, 2013, 197, doi:10.1016/j.geomorph.2013.04.027. ⟨10.1016/j.geomorph.2013.04.027⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geomorph.2013.04.027
hal-00818938
https://minesparis-psl.hal.science/hal-00818938
https://minesparis-psl.hal.science/hal-00818938/document
https://minesparis-psl.hal.science/hal-00818938/file/Thiry_al_Pierrelaye_Geomorphology_preprint.pdf
doi:10.1016/j.geomorph.2013.04.027
PRODINRA: 189396
WOS: 000323990100004
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/j.geomorph.2013.04.027
container_title Geomorphology
container_volume 197
container_start_page 34
op_container_end_page 44
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spelling ftecolephe:oai:HAL:hal-00818938v1 2024-05-19T07:41:54+00:00 Periglacial morphogenesis in the Paris Basin: insight from geophysical survey and consequences for the fate of soil pollution. Thiry, Médard van Oort, Fok Thiesson, Julien van Vliet-Lanoë, Brigitte Centre de Géosciences (GEOSCIENCES) Mines Paris - PSL (École nationale supérieure des mines de Paris) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Physicochimie et Ecotoxicologie des SolS d'Agrosystèmes Contaminés (PESSAC) Institut National de la Recherche Agronomique (INRA) UFR 918 Terre - environnement - Biodiversité Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE) Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris) Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Conseil Régional de l'Ile-de-France (CRIdF), Conseil Général du Val d'Oise (CG95), Agence de l'Eau de Seine-Normandie (AESN), Syndicat Interdépartemental pour l'Assainissement de l'Agglomération Parisienne (SIAAP) 2013-06-01 https://minesparis-psl.hal.science/hal-00818938 https://minesparis-psl.hal.science/hal-00818938/document https://minesparis-psl.hal.science/hal-00818938/file/Thiry_al_Pierrelaye_Geomorphology_preprint.pdf https://doi.org/10.1016/j.geomorph.2013.04.027 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geomorph.2013.04.027 hal-00818938 https://minesparis-psl.hal.science/hal-00818938 https://minesparis-psl.hal.science/hal-00818938/document https://minesparis-psl.hal.science/hal-00818938/file/Thiry_al_Pierrelaye_Geomorphology_preprint.pdf doi:10.1016/j.geomorph.2013.04.027 PRODINRA: 189396 WOS: 000323990100004 info:eu-repo/semantics/OpenAccess ISSN: 0169-555X Geomorphology https://minesparis-psl.hal.science/hal-00818938 Geomorphology, 2013, 197, doi:10.1016/j.geomorph.2013.04.027. ⟨10.1016/j.geomorph.2013.04.027⟩ periglacial cryoturbation soils geophysical method electrical mapping pollution micromorphology pedology [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2013 ftecolephe https://doi.org/10.1016/j.geomorph.2013.04.027 2024-04-25T00:47:40Z International audience Geophysical survey by of the Pierrelaye-Bessancourt area revealed conductive polygon patterns of 20-30 m diameter detected between 0.5 and 1.7 m depth. The patterns are formed by greenish glauconite and carbonated sand hollows where clay-rich pedological horizons bend downward, forming narrow tongs extending up to 2-3 m depth. Such structures were interpreted as a buried polygonal ice-wedge network. Geometrical relationships between the lithological units allowed the identification of successive landscape events and a landscape chronology. The sequence started during the Saalian glaciation with (1) development of patterned grounds by thermokarstic cryoturbation; (2) consecutive deflation/erosion during post-permafrost aridity; (3) loess and eolian sand deposits; (4) weathering of the former deposits with development of pedogenic horizons during the Eemian interglacial; (5) recurrent cryoturbation and thermal cracking leading to infolding of the pedogenic horizons during the Pleniglacial optimum (Weichselian); (5) finally erosion that levelled the periglacial microreliefs, leading to the modern landscape. In this agricultural area, urban waste water has been spread and has led to high levels of metal pollution in the surface horizons of the soils. The polygonal cryogenic structures have major impacts on soil hydrology and dispersion/distribution of heavy metals toward the geological substrate. Article in Journal/Newspaper Ice permafrost wedge* EPHE (Ecole pratique des hautes études, Paris): HAL Geomorphology 197 34 44