Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : the Seine estuary (France)
Identifieur interne : 000103 ( PascalFrancis/Corpus ); précédent : 000102; suivant : 000104Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : the Seine estuary (France)
Auteurs : A. Cuvilliez ; J. Deloffre ; R. Lafite ; C. BessinetonSource :
- Geomorphology (Amsterdam) [ 0169-555X ] ; 2009.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
This study deals with the morphological evolution of this zone from 1978 to 2005, in particular the impact of the construction on the Northern intertidal mudflat at the mouth of the Seine estuary located between the new Le Havre port (Port 2000) and the Normandy bridge. The use of a low altitude remote sensing technique combined with traditional methods of ground survey and probes allow to demonstrate the impact of human activities on sedimentary and vegetation dynamics. The Northern mudflat of the estuary is the most affected by these human activities, which surface have reduced of 62% during the last 27 years with an intensified local erosion during the last 27 months. Results also establish that the response times of the sedimentary or topographic readjustment to an installation depend on the extent and the nature of the construction. In fact, the sedimentary readjustments to an installation can be delayed by up to 10 years in the case of the Seine estuary
Notice en format standard (ISO 2709)
Pour connaître la documentation sur le format Inist Standard.
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Format Inist (serveur)
NO : | FRANCIS 22528520 PRODIG-INTERGEO |
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ET : | Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : the Seine estuary (France) |
AU : | CUVILLIEZ (A.); DELOFFRE (J.); LAFITE (R.); BESSINETON (C.) |
AF : | Lab. de Morphodynamique Continentale et Côtière, Univ. Rouen, UMR CNRS 6143 M2C/Mont St.Aignan/France (2 aut., 3 aut.); Maison de l'estuaire de la Seine/Le Havre/France (4 aut.); Univ., FST/Le Havre/France |
DT : | Publication en série; Niveau analytique |
SO : | Geomorphology (Amsterdam); ISSN 0169-555X; Pays-Bas; Da. 2009; Vol. 104; No. 3-4; Pp. 165-174; Bibl. 1 p.; 7 fig. |
LA : | Anglais |
EA : | This study deals with the morphological evolution of this zone from 1978 to 2005, in particular the impact of the construction on the Northern intertidal mudflat at the mouth of the Seine estuary located between the new Le Havre port (Port 2000) and the Normandy bridge. The use of a low altitude remote sensing technique combined with traditional methods of ground survey and probes allow to demonstrate the impact of human activities on sedimentary and vegetation dynamics. The Northern mudflat of the estuary is the most affected by these human activities, which surface have reduced of 62% during the last 27 years with an intensified local erosion during the last 27 months. Results also establish that the response times of the sedimentary or topographic readjustment to an installation depend on the extent and the nature of the construction. In fact, the sedimentary readjustments to an installation can be delayed by up to 10 years in the case of the Seine estuary |
CC : | 53151; 531 |
FD : | Estuaire; Impact; Action anthropique; Zone intertidale; Sédimentologie; Erosion; Infrastructure portuaire; Télédétection; Années 1978-2005; France; Normandie; Seine |
ED : | Estuary; Impact; Human impact; Intertidal zone; Sedimentology; Erosion; Port infrastructure; Remote sensing; France; Normandie; Seine |
SD : | Estuario; Impacto; Acción antrópica; Zona intertidal; Sedimentología; Erosión; Infraestructura portuaria; Teledetección |
LO : | INIST-21151 |
ID : | 22528520 |
Links to Exploration step
Francis:22528520Le document en format XML
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<front><div type="abstract" xml:lang="en">This study deals with the morphological evolution of this zone from 1978 to 2005, in particular the impact of the construction on the Northern intertidal mudflat at the mouth of the Seine estuary located between the new Le Havre port (Port 2000) and the Normandy bridge. The use of a low altitude remote sensing technique combined with traditional methods of ground survey and probes allow to demonstrate the impact of human activities on sedimentary and vegetation dynamics. The Northern mudflat of the estuary is the most affected by these human activities, which surface have reduced of 62% during the last 27 years with an intensified local erosion during the last 27 months. Results also establish that the response times of the sedimentary or topographic readjustment to an installation depend on the extent and the nature of the construction. In fact, the sedimentary readjustments to an installation can be delayed by up to 10 years in the case of the Seine estuary</div>
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<ET>Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : the Seine estuary (France)</ET>
<AU>CUVILLIEZ (A.); DELOFFRE (J.); LAFITE (R.); BESSINETON (C.)</AU>
<AF>Lab. de Morphodynamique Continentale et Côtière, Univ. Rouen, UMR CNRS 6143 M2C/Mont St.Aignan/France (2 aut., 3 aut.); Maison de l'estuaire de la Seine/Le Havre/France (4 aut.); Univ., FST/Le Havre/France</AF>
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<LA>Anglais</LA>
<EA>This study deals with the morphological evolution of this zone from 1978 to 2005, in particular the impact of the construction on the Northern intertidal mudflat at the mouth of the Seine estuary located between the new Le Havre port (Port 2000) and the Normandy bridge. The use of a low altitude remote sensing technique combined with traditional methods of ground survey and probes allow to demonstrate the impact of human activities on sedimentary and vegetation dynamics. The Northern mudflat of the estuary is the most affected by these human activities, which surface have reduced of 62% during the last 27 years with an intensified local erosion during the last 27 months. Results also establish that the response times of the sedimentary or topographic readjustment to an installation depend on the extent and the nature of the construction. In fact, the sedimentary readjustments to an installation can be delayed by up to 10 years in the case of the Seine estuary</EA>
<CC>53151; 531</CC>
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