Impressive abrasion rates of marked pebbles on a coarse-clastic beach within a 13-month timespan

被引:24
作者
Bertoni, Duccio [1 ]
Sarti, Giovanni [1 ]
Grottoli, Edoardo [2 ]
Ciavola, Paolo [2 ]
Pozzebon, Alessandro [3 ]
Domokos, Gabor [4 ]
Novak-Szabo, Timea [4 ]
机构
[1] Univ Pisa, Dipartimento Sci Terra, Via S Maria 53, I-56126 Pisa, Italy
[2] Univ Ferrara, Dipartimento Fis & Sci Terra, Via Saragat 1, I-44122 Ferrara, Italy
[3] Univ Siena, Dipartimento Ingn Informaz & Sci Matemat, Via Roma 56, I-53100 Siena, Italy
[4] Budapest Univ Technol & Econ, Dept Mech Mat & Struct, Muegyet Rkp 1-3,K261, H-1111 Budapest, Hungary
关键词
Abrasion rate; Pebble; Coarse-clastic beach; Beach nourishment; Coastal management; Marina di Pisa; MARINA DI PISA; GRAVEL BEACH; MIXED SAND; TRANSPORT; SHAPE; EVOLUTION; COAST; RIVER; SIZE;
D O I
10.1016/j.margeo.2016.09.010
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this paper the abrasion rate on a coarse-clastic beach was evaluated by calculating the volume loss recorded on indigenous pebbles within a 13-month timespan. The experiment was carried out at Marina di Pisa (Italy) on an artificial beach that was built to counteract the erosion processes affecting this sector of the coast. A total of 240 marble pebbles (120 rounded and 120 angular) were marked using the RFID technology and injected on the beach. The volume loss measured after consecutive recovery campaigns was progressively increasing, reaching the maximum value after 13 months (61% overall). The average volume loss is consistent between rounded and angular pebbles at any time (59.3% and 64.2% after 13 months respectively), meaning that the roundness is not a primary control factor on abrasion rate. The pebbles that did not reach such abrasion rates after 8 and 10 months (volume loss less than 20%) were found at heights equal or greater than 2 m above mean sea level, on the crest of the storm berm that formed during the strongest storms. This implies that the highest wearing is achieved in the lower portion of the bacicshore, which is also the area that underwent major topographic modifications. Here, sea water action might also exert chemical influence on the pebbles, adding to the mechanical abrasion. The main result of this research, indicating an impressive volume loss on beach pebbles in a short timespan, could be of key importance for coastal managers. The optimization of coarse sediment beach nourishments is also relevant, taking into right consideration that the volume loss due to sediment abrasion might exceed 50% of the original fill volume just after 1 year in the most dynamic portion of the beach. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:175 / 180
页数:6
相关论文
共 26 条
[21]   The marble beaches of Tuscany [J].
Nordstrom, Karl F. ;
Pranzini, Enzo ;
Jackson, Nancy L. ;
Coli, Massimo .
GEOGRAPHICAL REVIEW, 2008, 98 (02) :280-300
[22]   Updrift river mouth migration on cuspate deltas: two examples from the coast of Tuscany (Italy) [J].
Pranzini, E .
GEOMORPHOLOGY, 2001, 38 (1-2) :125-132
[23]  
Russell R.D., 1939, SPECIAL PUBLICATION, V4, P32, DOI DOI 10.1306/SV10340C2
[24]  
Sternberg H., 1875, Z F R BAUWESEN, V25, P483
[25]   Abrasion model of downstream changes in grain shape and size along the Williams River, Australia [J].
Szabo, Timea ;
Fityus, Stephen ;
Domokos, Gabor .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2013, 118 (04) :2059-2071
[26]  
Zingg T., 1935, Schweiz. Mineral. Petrogr. Mitt., V15, P52, DOI [10.3929/ethz-a-000103455, DOI 10.3929/ETHZ-A-000103455]