Beach Response to a Shoreface Nourishment (Aveiro, Portugal)

被引:19
|
作者
Mendes, Diogo [1 ,2 ,5 ]
Pais-Barbosa, Joaquim [2 ,3 ]
Baptista, Paulo [1 ,2 ]
Silva, Paulo A. [2 ,3 ]
Bernardes, Cristina [1 ,2 ]
Pinto, Celso [4 ]
机构
[1] Univ Aveiro, Dept Geociencias, Campus Santiago, P-3810193 Aveiro, Portugal
[2] Univ Aveiro, Ctr Estudos Ambiente & Mar CESAM, Campus Santiago, P-3810193 Aveiro, Portugal
[3] Univ Aveiro, Dept Fis, Campus Santiago, P-3810193 Aveiro, Portugal
[4] Agencia Portuguesa Ambiente IP, Rua Murgueira 9, P-2610124 Alfragide, Amadora, Portugal
[5] HAEDES, P-2025452 Azoia De Cima, Portugal
关键词
beach nourishment; field observations; storm; beach accretion; COASTAL STRETCH; EVOLUTION; VARIABILITY; TRANSPORT; PRECISE; PROJECT; SAND;
D O I
10.3390/jmse9101112
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
In Aveiro (NW coast of Portugal), a coastal monitoring programme was carried out in sequence of a shoreface nourishment intervention (over than 2 M m(3)) performed in 2020. In this programme, almost one year of biweekly subaerial topographies and quarterly bathymetric surveys have been collected along a 10 km coastal stretch between June 2020 and June 2021. In this study, topographic and bathymetric surveys were analysed to assess the expectation that if the shoreface nourishment is located in sufficiently shallow water depths, its landward movement will feed adjacent beaches and, consequently, increase the subaerial beach volume. Results show that the subaerial beach volume is well correlated with the 1.05 m (above MSL) isoline displacement through time. While the seaward limit of the shoreface nourishment moved landwards about 200 m, the shoreline proxy (isoline of 1.05 m) displayed a maximum seaward displacement of 60 m. The displacement of the shoreline proxy was highly variable in space, along the 10 km coastal stretch, and also in time, during storm events. During such events, both landward and seawards displacement of the shoreline proxy took place, depending on the spatial position. Moreover, while beaches close to the initial shoreface nourishment intervention displayed faster accretion patterns than those located farther away, the well-defined onshore movement of the shoreface nourishment did not result in a considerable beach volume increase. The achieved results were also compared against case studies of shoreface nourishments with similar volumes performed worldwide.
引用
收藏
页数:19
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