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

被引:33
作者
Cuvilliez, Antoine [1 ,2 ]
Deloffre, Julien [2 ]
Lafite, Robert [2 ]
Bessineton, Christophe [3 ]
机构
[1] Univ Havre, FST, F-76058 Le Havre, France
[2] Univ Rouen, Lab Morphodynam Continentale & Cotiere, UMR CNRS M2C 6143, F-76821 Mont St Aignan, France
[3] Maison Estuaire Seine Ctr Sci Culture & Tech Estu, F-76600 Le Havre, France
关键词
Remote sensing; Tidal mudflat; Human impact; Macrotidal estuary; SEDIMENT TRANSPORT; MACROTIDAL ESTUARY; TURBIDITY MAXIMUM; RIVER ESTUARY; SALT-MARSH; FACIES; INLET;
D O I
10.1016/j.geomorph.2008.08.010
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
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 1250 000 m(3) 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. (C) 2008 Elsevier B.V. All rights reserved.
引用
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页码:165 / 174
页数:10
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