Sand Spit Morphology at an Inlet on Phu Quoc Island, Vietnam

Author:

Duy Dinh Van1ORCID,Ty Tran Van1,Thanh Tran Nhat1,Minh Huynh Vuong Thu2ORCID,De Cao Van3,Duong Vu Hoang Thai4ORCID,Dan Trinh Cong4,Viet Nguyen Trung5ORCID,Tanaka Hitoshi6ORCID

Affiliation:

1. Water Resource Engineering Faculty, College of Engineering, Can Tho University, Can Tho 94115, Vietnam

2. Water Resources Department, College of Environment and Natural Resources, Can Tho University, Can Tho 94115, Vietnam

3. Institute of Coastal and Offshore Engineering, 658 Vo Van Kiet Street, Ward 1, District 5, Ho Chi Minh City 74900, Vietnam

4. Institute of Water and River Basin Management, Karlsruhe Institute of Technology, Kaiserallee 12, 76131 Karlruhe, Germany

5. Faculty of Civil Engineering, Thuy Loi University, Ha Noi 11515, Vietnam

6. Institute of Liberal Arts and Sciences, Tohoku University, 41 Kawauchi, Aoba-ku, Sendai 980-8576, Japan

Abstract

Tidal inlets with attached sand spits are a very common coastal landform. Since the evolution of sand spits along coastlines influence the social-economic development of local coastal areas, sand spits have become the objects of numerous studies. However, previous studies have mainly focused on sand spits that are usually in the scale of hundreds of meters in width, whilst knowledge about the evolution of smaller-scale sand spits still remains limited. Therefore, in this study, the morphological change of a small and unexplored sand spit in front of Song Tranh Inlet on the west coast of Phu Quoc Island, Vietnam is investigated. Satellite images are first used to observe the morphological change of the sand spit and calculate the longshore sediment transport rates (LSTR) along the sand spit. Waves and beach sediments are collected at the study site to calculate the longshore sediment transport rate using the CERC formula. It is found that there is a seasonal variation in the evolution of the sand spit at Song Tranh Inlet. The longshore sediment transport rates along the spit calculated by image analysis are 39,000 m3/year, 66,000 m3/year, and 40,000 m3/year, whilst the longshore sediment transport rate calculated by the CERC formula is 72,000 m3/year. This study aims to contribute to the methodology for investigating the evolutions of small sand spits and, specifically, sustainable coastal management for Phu Quoc Island, which is well-known as the Pearl Island of Vietnam.

Publisher

MDPI AG

Subject

Water Science and Technology,Aquatic Science,Geography, Planning and Development,Biochemistry

Reference57 articles.

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2. Duc Anh, N.Q., Tanaka, H., Tam, H.S., Tinh, N.X., Tung, T.T., and Viet, N.T. (2020). Comprehensive Study of the Sand Spit Evolution at Tidal Inlets in the Central Coast of Vietnam. J. Mar. Sci. Eng., 8.

3. Tanaka, H., and Shuto, N. (1993). Coastal Engineering 1992, American Society of Civil Engineers.

4. Bedload transport and dune bedforms characteristics in sand-bed rivers supplying a retreating beach of the northern Adriatic Sea (Italy);Cilli;J. Hydrol. Reg. Stud.,2021

5. Morphological Evolution of Sand Spits in Thailand;Saengsupavanich;Mar. Geod.,2021

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