USING SHALLOW NEARSHORE BERM NOURISHMENTS TO ENHANCE BEACH WIDTH

Matthieu A. de Schipper, Casper J. Onnink, Brittany L Bruder, Katherine L. Brodie
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Abstract

Nearshore berms or shoreface nourishments are sandy coastal interventions in which sediment is placed seaward of the land-water interface. These projects rely on natural forces to redistribute sediment in the nearshore zone and mitigate erosion, increase beach width or both. However, there is still limited knowledge on the connection between the morphodynamic development of the nourishment body and the changes to the beach landward to it. Several aspects make it difficult to connect the changes in the sub-aqueous and sub-aerial zones of the cross-shore profile, amongst others the lack of data and the small signal in beach changes with respect to the natural variability. We hypothesize that this obscurity also originates from the deep placement of most nearshore berms, making them mobilized very infrequently. This study examines observations of a unique shallow nearshore berm at New Smyrna (FL) where about 350,000 m3 of sediment dredged from a nearby inlet was deposited in the nearshore zone by moving the end of an outflow pipe along a 400-m section of coast.
利用浅水的近岸护堤来增加滩宽
近岸护堤或滨面营养物是砂质海岸干预物,其中沉积物被放置在陆地-水界面的向海方向。这些项目依靠自然力量来重新分配近岸地区的沉积物,减轻侵蚀,增加海滩宽度或两者兼而有之。然而,对于营养体形态动力学发育与滩地向陆源方向变化之间的关系,人们的认识仍然有限。有几个方面使得很难将跨岸剖面的水下和空中区域的变化联系起来,其中包括缺乏数据和海滩变化相对于自然变率的小信号。我们假设,这种模糊也源于大多数近岸护堤的深位置,使它们很少活动。本研究考察了新士麦那(FL)一个独特的浅水近岸护堤的观测结果,在那里,通过沿着400米长的海岸移动流出管的末端,从附近的一个入口疏浚了约35万立方米的沉积物,沉积在近岸区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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