The Effects of Intra-Annual Variability of River Discharge on the Spatio-Temporal Dynamics of Saltmarsh Vegetation at River Mouth Bar: Insights from an Ecogeomorphological Model

被引:6
|
作者
Zhang, S. [1 ,2 ]
Gao, W. [1 ,2 ,3 ]
Shao, D. [1 ,2 ,4 ]
Nardin, W. [5 ]
Gualtieri, C. [6 ]
Sun, T. [1 ,2 ]
机构
[1] Beijing Normal Univ, Sch Environm, State Key Lab Water Environm Simulat, Beijing 100875, Peoples R China
[2] Minist Educ, Yellow River Estuary Wetland Ecosyst Observat & R, Dongying 257200, Shandong, Peoples R China
[3] Beijing Normal Univ, Res & Dev Ctr Watershed Environm Ecoengn, Zhuhai 519087, Guangdong, Peoples R China
[4] Beijing Normal Univ, Beijing 100875, Peoples R China
[5] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA
[6] Univ Naples Federico II, Dept Civil Architectural & Environm Engn, Via Claudio 21, I-80125 Naples, Italy
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
ecogeomorphological model; river mouth bar; river deltas; saltmarsh; intra-annual variation; unsteady river discharge; SEA-LEVEL RISE; SPARTINA-ALTERNIFLORA; YANGTZE ESTUARY; FRESH-WATER; SEDIMENT; PLANT; DELTA; MORPHODYNAMICS; ECOSYSTEMS; INVASION;
D O I
10.3808/jei.202300498
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Natural or human-induced intra-annual variation of river discharge alters estuarine hydrological regimes and further affects habitat conditions for saltmarsh vegetation, particularly at the river mouth bar. In this study, numerical experiments were performed in Delft3D to simulate the evolution of a schematized river mouth bar under prototypical unsteady river discharge scenarios. The simulated hydrodynamic and morphodynamic changes were used to drive a vegetation dynamics model developed based on Spartina alterniflora in real time to model the resultant vegetation responses throughout the plant life history. Our results show that the imposed seasonal high flow can create more potential suitable habitat for the vegetation expansion and at the same time, cause marsh erosion through flood-induced drag force and substrate erosion. The overall effect of the trade-off between expansion and erosion depends on the timing, magnitude and duration of the high flow as well as its carried sediment concentration, leading to three vegetation response regimes, namely, minimal impact with small flood, erosion with big flood and low sediment supply, and expansion with big flood and high sediment supply. Besides, the timing of the high flow determines whether the vegetation has enough time to occupy the newly created subaerial area after the high flow and thereby affects the overall saltmarsh extent. The proposed vegetation response regimes are verified in principle in real cases such as Yellow River Estuary, Wax Lake Delta and Yangtze River Estuary. Our findings can help inform water diversion projects in river deltas to restore coastal wetlands in terms of suitable sediment supply and timing, etc.
引用
收藏
页码:108 / 122
页数:15
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