Zixi Zhao , Shaotong Zhang , Jinran Wu , Yao Jin , Lulu Qiao , Guangxue Li , Sanzhong Li
{"title":"从现场测量的悬浮沉积物浓度剖面中分离水平平流分量","authors":"Zixi Zhao , Shaotong Zhang , Jinran Wu , Yao Jin , Lulu Qiao , Guangxue Li , Sanzhong Li","doi":"10.1016/j.watres.2025.124630","DOIUrl":null,"url":null,"abstract":"<div><div>The one-dimensional vertical diffusion-settling (1DV) model is a classical tool for analyzing sediment dynamics. However, it assumes that horizontal advection effects are negligible, making it effective for sandy coasts with strong vertical mixing but unsuitable for fine-grained sediments. Existing methods for separating advection effects rely on costly experimental techniques or physical process-based models, limiting their practicality. To overcome this challenge, this study introduces a data-driven approach based on dynamic mode decomposition (DMD), making it possible to separate horizontal advection components while reducing the complexity of the modeling process. By applying the DMD method hierarchically, three distinct components were reconstructed from the measured SSC profiles: (1) Profile I, representing the combined effect of storm-induced vertical mixing and background concentration; (2) Profile II, corresponding to tidal resuspension associated with the M2 tide; and (3) Profile III, representing horizontal advection driven by the M2 tide. The relative variance contribution rate (RVCR) of these profiles was analyzed throughout the study period, revealing that during storm events, Profile I dominated SSC variations, with a peak contribution of 98.7%. As the storm intensity weakened, the contribution of Profile I gradually declined, while that of Profile II increased. After the storm dissipated, Profile II became the dominant component controlling fine-grained SSC variations, reaching a maximum RVCR of 70.9%. The RVCR of Profile III remained below 2% during the storm period but increased following the storm, with a maximum of 7.8% observed throughout the study period. The reconstructed total SSC profiles exhibit high accuracy, with 83.7% of RMSE values below 0.3 g/L, validating the effectiveness of the proposed method. This study successfully separates horizontal advection components from observed SSC profiles using a data-driven decomposition method, providing technical support for extending the 1DV model to silty coasts and offering a new approach for analyzing sediment transport dynamics.</div></div>","PeriodicalId":443,"journal":{"name":"Water Research","volume":"288 ","pages":"Article 124630"},"PeriodicalIF":12.4000,"publicationDate":"2025-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Separating the horizontal advection component from field-measured suspended sediment concentration profiles\",\"authors\":\"Zixi Zhao , Shaotong Zhang , Jinran Wu , Yao Jin , Lulu Qiao , Guangxue Li , Sanzhong Li\",\"doi\":\"10.1016/j.watres.2025.124630\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The one-dimensional vertical diffusion-settling (1DV) model is a classical tool for analyzing sediment dynamics. However, it assumes that horizontal advection effects are negligible, making it effective for sandy coasts with strong vertical mixing but unsuitable for fine-grained sediments. Existing methods for separating advection effects rely on costly experimental techniques or physical process-based models, limiting their practicality. To overcome this challenge, this study introduces a data-driven approach based on dynamic mode decomposition (DMD), making it possible to separate horizontal advection components while reducing the complexity of the modeling process. By applying the DMD method hierarchically, three distinct components were reconstructed from the measured SSC profiles: (1) Profile I, representing the combined effect of storm-induced vertical mixing and background concentration; (2) Profile II, corresponding to tidal resuspension associated with the M2 tide; and (3) Profile III, representing horizontal advection driven by the M2 tide. The relative variance contribution rate (RVCR) of these profiles was analyzed throughout the study period, revealing that during storm events, Profile I dominated SSC variations, with a peak contribution of 98.7%. As the storm intensity weakened, the contribution of Profile I gradually declined, while that of Profile II increased. After the storm dissipated, Profile II became the dominant component controlling fine-grained SSC variations, reaching a maximum RVCR of 70.9%. The RVCR of Profile III remained below 2% during the storm period but increased following the storm, with a maximum of 7.8% observed throughout the study period. The reconstructed total SSC profiles exhibit high accuracy, with 83.7% of RMSE values below 0.3 g/L, validating the effectiveness of the proposed method. This study successfully separates horizontal advection components from observed SSC profiles using a data-driven decomposition method, providing technical support for extending the 1DV model to silty coasts and offering a new approach for analyzing sediment transport dynamics.</div></div>\",\"PeriodicalId\":443,\"journal\":{\"name\":\"Water Research\",\"volume\":\"288 \",\"pages\":\"Article 124630\"},\"PeriodicalIF\":12.4000,\"publicationDate\":\"2025-09-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Water Research\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0043135425015337\",\"RegionNum\":1,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENGINEERING, ENVIRONMENTAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Water Research","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0043135425015337","RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
Separating the horizontal advection component from field-measured suspended sediment concentration profiles
The one-dimensional vertical diffusion-settling (1DV) model is a classical tool for analyzing sediment dynamics. However, it assumes that horizontal advection effects are negligible, making it effective for sandy coasts with strong vertical mixing but unsuitable for fine-grained sediments. Existing methods for separating advection effects rely on costly experimental techniques or physical process-based models, limiting their practicality. To overcome this challenge, this study introduces a data-driven approach based on dynamic mode decomposition (DMD), making it possible to separate horizontal advection components while reducing the complexity of the modeling process. By applying the DMD method hierarchically, three distinct components were reconstructed from the measured SSC profiles: (1) Profile I, representing the combined effect of storm-induced vertical mixing and background concentration; (2) Profile II, corresponding to tidal resuspension associated with the M2 tide; and (3) Profile III, representing horizontal advection driven by the M2 tide. The relative variance contribution rate (RVCR) of these profiles was analyzed throughout the study period, revealing that during storm events, Profile I dominated SSC variations, with a peak contribution of 98.7%. As the storm intensity weakened, the contribution of Profile I gradually declined, while that of Profile II increased. After the storm dissipated, Profile II became the dominant component controlling fine-grained SSC variations, reaching a maximum RVCR of 70.9%. The RVCR of Profile III remained below 2% during the storm period but increased following the storm, with a maximum of 7.8% observed throughout the study period. The reconstructed total SSC profiles exhibit high accuracy, with 83.7% of RMSE values below 0.3 g/L, validating the effectiveness of the proposed method. This study successfully separates horizontal advection components from observed SSC profiles using a data-driven decomposition method, providing technical support for extending the 1DV model to silty coasts and offering a new approach for analyzing sediment transport dynamics.
期刊介绍:
Water Research, along with its open access companion journal Water Research X, serves as a platform for publishing original research papers covering various aspects of the science and technology related to the anthropogenic water cycle, water quality, and its management worldwide. The audience targeted by the journal comprises biologists, chemical engineers, chemists, civil engineers, environmental engineers, limnologists, and microbiologists. The scope of the journal include:
•Treatment processes for water and wastewaters (municipal, agricultural, industrial, and on-site treatment), including resource recovery and residuals management;
•Urban hydrology including sewer systems, stormwater management, and green infrastructure;
•Drinking water treatment and distribution;
•Potable and non-potable water reuse;
•Sanitation, public health, and risk assessment;
•Anaerobic digestion, solid and hazardous waste management, including source characterization and the effects and control of leachates and gaseous emissions;
•Contaminants (chemical, microbial, anthropogenic particles such as nanoparticles or microplastics) and related water quality sensing, monitoring, fate, and assessment;
•Anthropogenic impacts on inland, tidal, coastal and urban waters, focusing on surface and ground waters, and point and non-point sources of pollution;
•Environmental restoration, linked to surface water, groundwater and groundwater remediation;
•Analysis of the interfaces between sediments and water, and between water and atmosphere, focusing specifically on anthropogenic impacts;
•Mathematical modelling, systems analysis, machine learning, and beneficial use of big data related to the anthropogenic water cycle;
•Socio-economic, policy, and regulations studies.