Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : The Seine estuary (France)
Identifieur interne : 000108 ( PascalFrancis/Checkpoint ); précédent : 000107; suivant : 000109Morphological 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 :
- Geomorphology : (Amsterdam) [ 0169-555X ] ; 2009.
Descripteurs français
- Pascal (Inist)
- Wicri :
- topic : Télédétection.
English descriptors
- KwdEn :
- English Channel, Seine Estuary, Seine-Maritime France, aerial photography, altitude, channels, equilibrium, estuarine environment, fine-grained materials, floods, grains, human activity, hydrodynamics, intertidal environment, landform evolution, littoral erosion, modern, mud flats, remote sensing, tidal flats, vegetation.
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.
Affiliations:
- France
- Haute-Normandie, Région Normandie
- Le Havre, Mont St. Aignan
- Université de Rouen, Université du Havre
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activity</term><term>hydrodynamics</term><term>intertidal environment</term><term>landform evolution</term><term>littoral erosion</term><term>modern</term><term>mud flats</term><term>remote sensing</term><term>tidal flats</term><term>vegetation</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Erosion littorale</term><term>Hydrodynamique</term><term>Slikke</term><term>Altitude</term><term>Télédétection</term><term>Milieu estuaire</term><term>Action anthropique</term><term>Végétation</term><term>Fraction fine</term><term>Grain</term><term>Chenal</term><term>Crue</term><term>Milieu intertidal</term><term>Equilibre</term><term>Morphodynamique</term><term>Vasière</term><term>Actuel</term><term>Photographie aérienne</term><term>Estuaire Seine</term><term>Seine-Maritime</term><term>Manche Mer</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Télédétection</term></keywords></textClass></profileDesc></teiHeader><front><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></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0169-555X</s0></fA01><fA03 i2="1"><s0>Geomorphology : (Amst.)</s0></fA03><fA05><s2>104</s2></fA05><fA06><s2>3-4</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Morphological responses of an estuarine intertidal mudflat to constructions since 1978 to 2005 : The Seine estuary (France)</s1></fA08><fA11 i1="01" i2="1"><s1>CUVILLIEZ (Antoine)</s1></fA11><fA11 i1="02" i2="1"><s1>DELOFFRE (Julien)</s1></fA11><fA11 i1="03" i2="1"><s1>LAFITE (Robert)</s1></fA11><fA11 i1="04" i2="1"><s1>BESSINETON (Christophe)</s1></fA11><fA14 i1="01"><s1>Labomtoire de Morphodynamique Continentale et Côdère, Université de Rouen, UMR CNRS 6143 M2C</s1><s2>76821 Mont St. Aignan</s2><s3>FRA</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></fA14><fA14 i1="02"><s1>Université du Havre, FST</s1><s2>76058 Le Havre</s2><s3>FRA</s3><sZ>1 aut.</sZ></fA14><fA14 i1="03"><s1>Maison de l'estuaire de la Seine (Center of Scientific culture and Technique of the Estuary)</s1><s2>76600 Le Havre</s2><s3>FRA</s3><sZ>4 aut.</sZ></fA14><fA20><s1>165-174</s1></fA20><fA21><s1>2009</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>21151</s2><s5>354000187385680060</s5></fA43><fA44><s0>0000</s0><s1>© 2009 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>3/4 p.</s0></fA45><fA47 i1="01" i2="1"><s0>09-0393913</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Geomorphology : (Amsterdam)</s0></fA64><fA66 i1="01"><s0>NLD</s0></fA66><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><affiliations><list><country><li>France</li></country><region><li>Haute-Normandie</li><li>Région Normandie</li></region><settlement><li>Le Havre</li><li>Mont St. Aignan</li></settlement><orgName><li>Université de Rouen</li><li>Université du Havre</li></orgName></list><tree><country name="France"><region name="Région Normandie"><name sortKey="Cuvilliez, Antoine" sort="Cuvilliez, Antoine" uniqKey="Cuvilliez A" first="Antoine" last="Cuvilliez">Antoine Cuvilliez</name></region><name sortKey="Bessineton, Christophe" sort="Bessineton, Christophe" uniqKey="Bessineton C" first="Christophe" last="Bessineton">Christophe Bessineton</name><name sortKey="Cuvilliez, Antoine" sort="Cuvilliez, Antoine" uniqKey="Cuvilliez A" first="Antoine" last="Cuvilliez">Antoine Cuvilliez</name><name sortKey="Deloffre, Julien" sort="Deloffre, Julien" uniqKey="Deloffre J" first="Julien" last="Deloffre">Julien Deloffre</name><name sortKey="Lafite, Robert" sort="Lafite, Robert" uniqKey="Lafite R" first="Robert" last="Lafite">Robert Lafite</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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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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