TY - JOUR
T1 - Cumulative impact of human activities on hydro-sediment dynamics and morphodynamics in the highly altered Yangtze Estuary
AU - Han, Xiangju
AU - Fan, Daidu
AU - Huang, Ju
AU - Tu, Junbiao
AU - Meng, Lingpeng
AU - Chen, Shenliang
N1 - Publisher Copyright:
© 2024 Elsevier B.V.
PY - 2025/4
Y1 - 2025/4
N2 - Estuarine dynamics is influenced not only by upstream human activities but also significantly by large-scale estuarine engineering projects (LSEPs). In recent decades, multiple LSEPs have been constructed in the Yangtze Estuary, and the impacts of single project have been well studied, but their cumulative impacts remain elusive. This study investigates Yangtze Estuary morphological changes from 1958 to 2020 by chart bathymetric data. Results reveal a shift from rapid accretion (1958–1983) to moderate accretion (1983–2011), and then to moderate erosion (2011–2020), almost coeval with declining fluvial sediment discharge in response to the upstream human disturbances. Moreover, increasing LSEPs have complexified estuarine erosion and deposition patterns over local to regional scales in the past two decades. The impacts of LSEPs on estuarine dynamics are further examined by a coupled model based on Delft3D in the Yangtze Estuary under six scenarios. Results indicate that the residual water flux and residual sediment flux both form a convergence center at the South Passage mouth, aligning with the persistent muddy depo-center. The hydro-sediment dynamics intensify at the upper reaches of the South Passage, North Passage, and North Channel while weaken at the lower reaches under the cumulative effects of three constructed LSEPs. However, the planning Hengsha Shoal Offshore Groins project will cause contrasting effects in the North Channel. As the LSEPs increase, estuarine sediment accretion intensity decreases, declining the net suspended sediment budget by ∼ 8.7 % after four LSEPs. These findings highlight numerical modeling is a powerful tool for worldwide estuarine planning and management.
AB - Estuarine dynamics is influenced not only by upstream human activities but also significantly by large-scale estuarine engineering projects (LSEPs). In recent decades, multiple LSEPs have been constructed in the Yangtze Estuary, and the impacts of single project have been well studied, but their cumulative impacts remain elusive. This study investigates Yangtze Estuary morphological changes from 1958 to 2020 by chart bathymetric data. Results reveal a shift from rapid accretion (1958–1983) to moderate accretion (1983–2011), and then to moderate erosion (2011–2020), almost coeval with declining fluvial sediment discharge in response to the upstream human disturbances. Moreover, increasing LSEPs have complexified estuarine erosion and deposition patterns over local to regional scales in the past two decades. The impacts of LSEPs on estuarine dynamics are further examined by a coupled model based on Delft3D in the Yangtze Estuary under six scenarios. Results indicate that the residual water flux and residual sediment flux both form a convergence center at the South Passage mouth, aligning with the persistent muddy depo-center. The hydro-sediment dynamics intensify at the upper reaches of the South Passage, North Passage, and North Channel while weaken at the lower reaches under the cumulative effects of three constructed LSEPs. However, the planning Hengsha Shoal Offshore Groins project will cause contrasting effects in the North Channel. As the LSEPs increase, estuarine sediment accretion intensity decreases, declining the net suspended sediment budget by ∼ 8.7 % after four LSEPs. These findings highlight numerical modeling is a powerful tool for worldwide estuarine planning and management.
KW - Delft3D
KW - Human Activities
KW - Hydro-sediment Dynamics
KW - Morphodynamics
KW - Suspended Sediment Budget
KW - Yangtze Estuary
UR - https://www.scopus.com/pages/publications/85213274577
U2 - 10.1016/j.jhydrol.2024.132625
DO - 10.1016/j.jhydrol.2024.132625
M3 - 文章
AN - SCOPUS:85213274577
SN - 0022-1694
VL - 651
JO - Journal of Hydrology
JF - Journal of Hydrology
M1 - 132625
ER -