Tu Le Xuan

Mr. Tu Le Xuan

orcid

Research Focus & Metrics

Academic Career Length

6Years (2021-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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12 August 2022 in Ocean & Coastal Management
Verified
Journal Article
Closed access
TXTu Le Xuan
Tu Le Xuan
HBHoang Tran Ba
Hoang Tran Ba
VTVo Quoc Thanh
Vo Quoc Thanh
DWDavid P. Wright
David P. Wright
ATAhad Hasan Tanim
Ahad Hasan Tanim
Duong Tran AnhDuong Tran Anh
Duong Tran Anh

25 April 2021 in Sustainability
Verified
Journal Article
Open access
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TLThai Thanh Luom
Thai Thanh Luom
Nguyen Tan PhongNguyen Tan Phong
Nguyen Tan Phong
Nguyen Tan PhongNguyen Tan Phong
Nguyen Tan Phong
NTNguyen Thanh Tung
Nguyen Thanh Tung
TXTu Le Xuan
Tu Le Xuan
Duong Tran AnhDuong Tran Anh
Duong Tran Anh
Offshore breakwaters can be effective in reducing the energy of incident waves through dissipation, refraction or reflection. Breakwaters are increasingly constructed to stabilize eroded muddy coasts, particularly in developing countries. Accumulation of fine-grained sediment and wave attenuation are two attributes of a stable muddy coast. Effective interventions in stabilizing eroded muddy coasts include two important elements: accumulation of fine-grained sediment and wave reduction. The efficacy of offshore breakwaters in stabilizing eroded muddy coasts is, however, not yet adequately understood. A crucial question needing attention is whether accumulation of fine-grained sediment and wave attenuation should be used in evaluating the efficacy of these offshore breakwaters in stabilizing eroded muddy coasts. To address this issue, a pile-rock offshore breakwater in Huong Mai, Tieu Dua of Ca Mau, Vietnam was selected as an appropriate example in this regard. Accumulation of fine-grained sediment and wave attenuation were tested as means to investigate the efficacy of the Huong Mai structure in stabilizing the eroded muddy coast. The study was undertaken using field-based measurements and semi-structured interviews in three stages between October 2016 and December 2020. We found that this structure has had limited efficacy in stabilizing the eroded muddy coast. The structure was effective in dissipating the energy of incident waves, but we found no evidence of fine-grained sediment accumulation due to an inappropriate structural design. There was also no monitoring system in place, leading to difficulties in evaluating its efficacy in terms of wave attenuation and accumulation of fine-grained sediment. The gaps between the shoreline and the structure have not been adequately explained, resulting in substantial challenges in replicating the structure elsewhere. The Huong Mai structure should be strengthened using supplementary measures and granulometric tests in order to improve the efficacy in stabilizing eroded muddy coasts. The methods in this study provide new insights in this regard.

26 November 2022 in Water
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Journal Article
Open access
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DSDinh Cong San
Dinh Cong San
NDNguyen Binh Duong
Nguyen Binh Duong
NPNguyen Cong Phong
Nguyen Cong Phong
TXTu Le Xuan
Tu Le Xuan
Damien Pham Van BangDamien Pham Van Bang
Damien Pham Van Bang
KNKim Dan Nguyen
Kim Dan Nguyen
Every year, in the Vietnam Mekong Delta Coastal Zone (VMDCZ), erosions cause approximately 300 ha of agricultural land loss. Therefore, measures for shoreline protection are urgently needed. This paper discusses the impacts of protection measures in the Go-Cong Coastal Zone to prevent erosion/accretion processes, predicted by two numerical models, MIKE21-FM and TELEMAC-2D. Hard and soft measures have been proposed using breakwaters and sandbars, respectively. The simulations show that the erosion/accretion trends provided by both models are similar. For breakwaters, MIKE21-FM provides less accretion than TELEMAC-2D in areas extending over 300 m and 500 m from shorelines. However, for sandbars, MIKE21-FM shows higher accretion within areas extending over 500 m but less than 300 m. Sandbars cause higher accretion in a larger area, extending over 1000 m offshore. The simulation results allow us to propose two alternative measures: (1) a row of several breakwater units will be implanted at 300 m offshore. The length of each unit is 600 m, with a gap between two neighbouring units of 70 m and a crest elevation of 2.2 m above mean sea level (MSL). (2) A row of sandbar units will be posed at 500 m offshore, with a unit length of 1000 m and a gap between the two neighbouring units of 200 m. The crest elevation is fixed at MSL.

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VDVũ Hoàng Thái Dương
Vũ Hoàng Thái Dương
MZMoritz Zemann
Moritz Zemann
RLRoderick van der Linden
Roderick van der Linden
DTDan Trinh
Dan Trinh
POPeter Oberle
Peter Oberle
TXTu Le Xuan
Tu Le Xuan
In the presented work, design conditions for breakwaters were derived from offshore climate reanalysis data (ERA5), which were downscaled to the nearshore by two numerical approaches, i.e., SwanOne and Delft3D, for different average and extreme wave and weather conditions. Model validation was performed using in situ measurements. The advantages and disadvantages of both numerical approaches were investigated. Both models showed sufficient accuracy according to measurements in the field, where SwanOne offers a simple and fast calculation method, while Delft3D provides a more complete representation, not only of waves but also current dynamics. However, it requires a much broader amount of input parameters and more complex boundary conditions. Then, SwanOne was applicable to calculate nearshore wave characteristics based on the input parameters extracted from the statistical analysis of long-term ERA5 data. Based on this process, design wave heights and periods at the nearshore were determined for 10- to 100-year return periods. For breakwater design on the west coast of the Mekong Delta, maximum wave heights in a range of 1.1 m to 1.3 m at a distance of 100 m to 300 m could be determined for a return period of 20 years, corresponding to water depths of 2.33 m and 2.88 m, respectively.

9 January 2026
Verified
Book Chapter
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TXTu Le Xuan
Tu Le Xuan
HBHoang Tran Ba
Hoang Tran Ba
HMHung Le Manh
Hung Le Manh
ATAhad Hasan Tanim
Ahad Hasan Tanim
AGAlexandre S. Gagnon
Alexandre S. Gagnon
DADuong Tran Anh
Duong Tran Anh