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Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : The Seine estuary (France)

Identifieur interne : 000222 ( PascalFrancis/Curation ); précédent : 000221; suivant : 000223

Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : The Seine estuary (France)

Auteurs : Antoine Cuvilliez [France] ; Julien Deloffre [France] ; Robert Lafite [France] ; Christophe Bessineton [France]

Source :

RBID : Pascal:09-0393913

Descripteurs français

English descriptors

Abstract

Since 1834 the Seine estuary (France) has been the site of numerous construction projects with the aim to accommodate and secure boat traffic. Since 1978, the increasing of the activities of Le Havre port, located at the mouth of the estuary, has accelerated the construction work rate. Several dykes, a bridge, and new port facilities have been constructed in rapid succession, modifying considerably the hydrodynamic conditions which sustain a partially vegetated sandy-muddy tidal flat located in the North bank of the estuary between the new port of Le Havre and the Normandy bridge achieved in 1995. The present study deals with the morphological evolution of this zone from 1978 to 2005. 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 corresponding to a loss 1250000 m3 of fine-grained sediment. At the same time, the general sanding up in the channel of the zone has caused a loss of more than 31% of the tidal prism, more than three quarters of which occurred during the last three years. 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. This delay is explained by a rapid succession of construction works which may occult the effect of a single installation. Except in the case of a dyke built perpendicular to ebb and flood currents, the impacts of these installations reach a hydro-sedimentary equilibrium on the level between 1 and 7 years after their completion.
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A11 01  1    @1 CUVILLIEZ (Antoine)
A11 02  1    @1 DELOFFRE (Julien)
A11 03  1    @1 LAFITE (Robert)
A11 04  1    @1 BESSINETON (Christophe)
A14 01      @1 Labomtoire de Morphodynamique Continentale et Côdère, Université de Rouen, UMR CNRS 6143 M2C @2 76821 Mont St. Aignan @3 FRA @Z 1 aut. @Z 2 aut. @Z 3 aut.
A14 02      @1 Université du Havre, FST @2 76058 Le Havre @3 FRA @Z 1 aut.
A14 03      @1 Maison de l'estuaire de la Seine (Center of Scientific culture and Technique of the Estuary) @2 76600 Le Havre @3 FRA @Z 4 aut.
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C01 01    ENG  @0 Since 1834 the Seine estuary (France) has been the site of numerous construction projects with the aim to accommodate and secure boat traffic. Since 1978, the increasing of the activities of Le Havre port, located at the mouth of the estuary, has accelerated the construction work rate. Several dykes, a bridge, and new port facilities have been constructed in rapid succession, modifying considerably the hydrodynamic conditions which sustain a partially vegetated sandy-muddy tidal flat located in the North bank of the estuary between the new port of Le Havre and the Normandy bridge achieved in 1995. The present study deals with the morphological evolution of this zone from 1978 to 2005. 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 corresponding to a loss 1250000 m3 of fine-grained sediment. At the same time, the general sanding up in the channel of the zone has caused a loss of more than 31% of the tidal prism, more than three quarters of which occurred during the last three years. 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. This delay is explained by a rapid succession of construction works which may occult the effect of a single installation. Except in the case of a dyke built perpendicular to ebb and flood currents, the impacts of these installations reach a hydro-sedimentary equilibrium on the level between 1 and 7 years after their completion.
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C03 01  2  FRE  @0 Erosion littorale @5 01
C03 01  2  ENG  @0 littoral erosion @5 01
C03 01  2  SPA  @0 Erosión litoral @5 01
C03 02  2  FRE  @0 Hydrodynamique @5 02
C03 02  2  ENG  @0 hydrodynamics @5 02
C03 02  2  SPA  @0 Hidrodinámica @5 02
C03 03  2  FRE  @0 Slikke @5 03
C03 03  2  ENG  @0 tidal flats @5 03
C03 03  2  SPA  @0 Marea parada @5 03
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C03 05  2  SPA  @0 Detección a distancia @5 05
C03 06  2  FRE  @0 Milieu estuaire @5 06
C03 06  2  ENG  @0 estuarine environment @5 06
C03 06  2  SPA  @0 Medio estuario @5 06
C03 07  2  FRE  @0 Action anthropique @5 07
C03 07  2  ENG  @0 human activity @5 07
C03 07  2  SPA  @0 Acción hombre @5 07
C03 08  2  FRE  @0 Végétation @5 08
C03 08  2  ENG  @0 vegetation @5 08
C03 08  2  SPA  @0 Vegetación @5 08
C03 09  2  FRE  @0 Fraction fine @5 10
C03 09  2  ENG  @0 fine-grained materials @5 10
C03 09  2  SPA  @0 Fracción fina @5 10
C03 10  2  FRE  @0 Grain @5 11
C03 10  2  ENG  @0 grains @5 11
C03 10  2  SPA  @0 Grano @5 11
C03 11  2  FRE  @0 Chenal @5 12
C03 11  2  ENG  @0 channels @5 12
C03 11  2  SPA  @0 Canal @5 12
C03 12  2  FRE  @0 Crue @5 13
C03 12  2  ENG  @0 floods @5 13
C03 12  2  SPA  @0 Crecida @5 13
C03 13  2  FRE  @0 Milieu intertidal @5 14
C03 13  2  ENG  @0 intertidal environment @5 14
C03 13  2  SPA  @0 Medio intertidal @5 14
C03 14  2  FRE  @0 Equilibre @5 15
C03 14  2  ENG  @0 equilibrium @5 15
C03 15  2  FRE  @0 Morphodynamique @5 16
C03 15  2  ENG  @0 landform evolution @5 16
C03 15  2  SPA  @0 Morfodinámica @5 16
C03 16  2  FRE  @0 Vasière @5 17
C03 16  2  ENG  @0 mud flats @5 17
C03 16  2  SPA  @0 Marisma @5 17
C03 17  2  FRE  @0 Actuel @5 18
C03 17  2  ENG  @0 modern @5 18
C03 17  2  SPA  @0 Actual @5 18
C03 18  2  FRE  @0 Photographie aérienne @5 19
C03 18  2  ENG  @0 aerial photography @5 19
C03 18  2  SPA  @0 Fotografía aérea @5 19
C03 19  2  FRE  @0 Estuaire Seine @2 NG @5 61
C03 19  2  ENG  @0 Seine Estuary @2 NG @5 61
C03 19  2  SPA  @0 Estuario Sena @2 NG @5 61
C03 20  2  FRE  @0 Seine-Maritime @2 NG @5 64
C03 20  2  ENG  @0 Seine-Maritime France @2 NG @5 64
C03 21  2  FRE  @0 Manche Mer @2 NG @5 65
C03 21  2  ENG  @0 English Channel @2 NG @5 65
C03 21  2  SPA  @0 Mancha (Canal) @2 NG @5 65
C07 01  2  FRE  @0 France @2 NG
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C07 01  2  SPA  @0 Francia @2 NG
C07 02  2  FRE  @0 Europe Ouest @2 NG
C07 02  2  ENG  @0 Western Europe @2 NG
C07 02  2  SPA  @0 Europa del Oeste @2 NG
C07 03  2  FRE  @0 Europe @2 564
C07 03  2  ENG  @0 Europe @2 564
C07 03  2  SPA  @0 Europa @2 564
C07 04  2  FRE  @0 Océan Atlantique Nord Est @2 NG
C07 04  2  ENG  @0 Northeast Atlantic @2 NG
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C07 06  2  ENG  @0 Atlantic Ocean @2 564
C07 06  2  SPA  @0 Océano Atlántico @2 564
N21       @1 285

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Pascal:09-0393913

Le document en format XML

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<div type="abstract" xml:lang="en">Since 1834 the Seine estuary (France) has been the site of numerous construction projects with the aim to accommodate and secure boat traffic. Since 1978, the increasing of the activities of Le Havre port, located at the mouth of the estuary, has accelerated the construction work rate. Several dykes, a bridge, and new port facilities have been constructed in rapid succession, modifying considerably the hydrodynamic conditions which sustain a partially vegetated sandy-muddy tidal flat located in the North bank of the estuary between the new port of Le Havre and the Normandy bridge achieved in 1995. The present study deals with the morphological evolution of this zone from 1978 to 2005. 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 corresponding to a loss 1250000 m
<sup>3</sup>
of fine-grained sediment. At the same time, the general sanding up in the channel of the zone has caused a loss of more than 31% of the tidal prism, more than three quarters of which occurred during the last three years. 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. This delay is explained by a rapid succession of construction works which may occult the effect of a single installation. Except in the case of a dyke built perpendicular to ebb and flood currents, the impacts of these installations reach a hydro-sedimentary equilibrium on the level between 1 and 7 years after their completion.</div>
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<fC01 i1="01" l="ENG">
<s0>Since 1834 the Seine estuary (France) has been the site of numerous construction projects with the aim to accommodate and secure boat traffic. Since 1978, the increasing of the activities of Le Havre port, located at the mouth of the estuary, has accelerated the construction work rate. Several dykes, a bridge, and new port facilities have been constructed in rapid succession, modifying considerably the hydrodynamic conditions which sustain a partially vegetated sandy-muddy tidal flat located in the North bank of the estuary between the new port of Le Havre and the Normandy bridge achieved in 1995. The present study deals with the morphological evolution of this zone from 1978 to 2005. 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 corresponding to a loss 1250000 m
<sup>3</sup>
of fine-grained sediment. At the same time, the general sanding up in the channel of the zone has caused a loss of more than 31% of the tidal prism, more than three quarters of which occurred during the last three years. 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. This delay is explained by a rapid succession of construction works which may occult the effect of a single installation. Except in the case of a dyke built perpendicular to ebb and flood currents, the impacts of these installations reach a hydro-sedimentary equilibrium on the level between 1 and 7 years after their completion.</s0>
</fC01>
<fC02 i1="01" i2="2">
<s0>001E01P02</s0>
</fC02>
<fC02 i1="02" i2="2">
<s0>001E01P01</s0>
</fC02>
<fC02 i1="03" i2="2">
<s0>001E01M04</s0>
</fC02>
<fC02 i1="04" i2="2">
<s0>226C02</s0>
</fC02>
<fC02 i1="05" i2="2">
<s0>226C01</s0>
</fC02>
<fC02 i1="06" i2="2">
<s0>225B04</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE">
<s0>Erosion littorale</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG">
<s0>littoral erosion</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA">
<s0>Erosión litoral</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE">
<s0>Hydrodynamique</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG">
<s0>hydrodynamics</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA">
<s0>Hidrodinámica</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE">
<s0>Slikke</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG">
<s0>tidal flats</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA">
<s0>Marea parada</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE">
<s0>Altitude</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG">
<s0>altitude</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA">
<s0>Altitud</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE">
<s0>Télédétection</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG">
<s0>remote sensing</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA">
<s0>Detección a distancia</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE">
<s0>Milieu estuaire</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG">
<s0>estuarine environment</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA">
<s0>Medio estuario</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE">
<s0>Action anthropique</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG">
<s0>human activity</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA">
<s0>Acción hombre</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE">
<s0>Végétation</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG">
<s0>vegetation</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA">
<s0>Vegetación</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE">
<s0>Fraction fine</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG">
<s0>fine-grained materials</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA">
<s0>Fracción fina</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE">
<s0>Grain</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG">
<s0>grains</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA">
<s0>Grano</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE">
<s0>Chenal</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG">
<s0>channels</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA">
<s0>Canal</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE">
<s0>Crue</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG">
<s0>floods</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA">
<s0>Crecida</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE">
<s0>Milieu intertidal</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG">
<s0>intertidal environment</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA">
<s0>Medio intertidal</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE">
<s0>Equilibre</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG">
<s0>equilibrium</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE">
<s0>Morphodynamique</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG">
<s0>landform evolution</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA">
<s0>Morfodinámica</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE">
<s0>Vasière</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG">
<s0>mud flats</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA">
<s0>Marisma</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE">
<s0>Actuel</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG">
<s0>modern</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA">
<s0>Actual</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE">
<s0>Photographie aérienne</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG">
<s0>aerial photography</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA">
<s0>Fotografía aérea</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE">
<s0>Estuaire Seine</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG">
<s0>Seine Estuary</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA">
<s0>Estuario Sena</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE">
<s0>Seine-Maritime</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG">
<s0>Seine-Maritime France</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE">
<s0>Manche Mer</s0>
<s2>NG</s2>
<s5>65</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG">
<s0>English Channel</s0>
<s2>NG</s2>
<s5>65</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA">
<s0>Mancha (Canal)</s0>
<s2>NG</s2>
<s5>65</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE">
<s0>France</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG">
<s0>France</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA">
<s0>Francia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE">
<s0>Europe Ouest</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG">
<s0>Western Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA">
<s0>Europa del Oeste</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE">
<s0>Europe</s0>
<s2>564</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG">
<s0>Europe</s0>
<s2>564</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA">
<s0>Europa</s0>
<s2>564</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE">
<s0>Océan Atlantique Nord Est</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG">
<s0>Northeast Atlantic</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE">
<s0>Océan Atlantique Nord</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG">
<s0>North Atlantic</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA">
<s0>Océano Atlántico Norte</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE">
<s0>Océan Atlantique</s0>
<s2>564</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG">
<s0>Atlantic Ocean</s0>
<s2>564</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA">
<s0>Océano Atlántico</s0>
<s2>564</s2>
</fC07>
<fN21>
<s1>285</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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   |area=    LeHavreV1
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   |texte=   Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : The Seine estuary (France)
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