共 50 条
A hybrid mechanism and ridge regression model to separate the effects of advection and resuspension on suspended sediment concentration
被引:3
|作者:
Li, Yuting
[1
,2
]
Song, Zhiyao
[2
]
Li, Ruijie
[3
]
Chen, Peng
[2
]
Quan, Xiufeng
[3
]
机构:
[1] Nanjing Normal Univ, Coll Marine Sci & Engn, Nanjing 210023, Peoples R China
[2] Nanjing Normal Univ, Key Lab Virtual Geog Environm, Nanjing 210023, Peoples R China
[3] Hohai Univ, Key Lab Coastal Disaster & Def, Minist Educ, Nanjing 210098, Peoples R China
基金:
中国国家自然科学基金;
关键词:
Coastal estuaries;
Suspended sediment concentration;
Advection;
Sediment resuspension;
FINITE-VOLUME METHOD;
NUMERICAL-MODEL;
WATER-QUALITY;
RIVER;
TRANSPORT;
RISK;
CAPACITY;
ESTUARY;
FLUX;
D O I:
10.1016/j.ecolind.2023.111149
中图分类号:
X176 [生物多样性保护];
学科分类号:
090705 ;
摘要:
Estuarine and coastal areas are land-sea interaction zones where sediment particles can easily move, leading to water quality and aquatic ecological issues. The suspended sediment concentration (SSC) is an important indicator of the movement of suspended particles and coastal water environments monitoring. However, traditional in situ SSC observations cannot directly separated contributions of advection and sediment resuspension. In this study we aim to propose a hybrid mechanism and ridge regression model to improve the accuracy of instantaneous SSC estuarine and coastal waters. The new model is based on the application of hydrodynamic factors, functional principles and dimensional evaluation methods, which can analysis the effects of horizontal convective transport, vertical suspended upward movement on the SSC. It is compared with existing formulas (models) and mathematical model (Mike21) calculation results, using field data from single stations at the Yangtze River Estuarine. The comparison shows that the accuracy of the new SSC calculation model based on the equations in this paper is high. The Pearson correlation coefficient of the new model has increased by approximately 0.20, and the relative mean square error and the mean absolute error have decreased by approximately 0.26. In addition, the new model can explain the hysteresis of the sediment transport process and water flow change reasonably.
引用
收藏
页数:15
相关论文