Cumulative impact of human activities on hydro-sediment dynamics and morphodynamics in the highly altered Yangtze Estuary

IF 6.3 1区 地球科学 Q1 ENGINEERING, CIVIL Journal of Hydrology Pub Date : 2024-12-26 DOI:10.1016/j.jhydrol.2024.132625
Xiangju Han , Daidu Fan , Ju Huang , Junbiao Tu , Lingpeng Meng , Shenliang Chen
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Abstract

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.
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人类活动对高度蚀变长江口水沙动力学和形态动力学的累积影响
河口动态不仅受到上游人类活动的影响,而且还受到大型河口工程项目的显著影响。近几十年来,长江口已建成多个lsep工程,并对单个工程的影响进行了较好的研究,但其累积影响尚不明确。利用海图水深资料,研究了长江口1958 ~ 2020年的地貌变化。研究结果表明,在上游人为干扰下,河流泥沙流量从快速淤积(1958-1983)到中度淤积(1983-2011)再到中度淤积(2011-2020)的变化过程几乎与河流泥沙流量的减少同步。此外,在过去20年中,不断增加的lsep使河口侵蚀和沉积模式在局地和区域尺度上变得复杂。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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