Yang Wang , Rijun Hu , Xiaodong Zhang , Jiandong Qiu , Naishuang Bi , Longhai Zhu , Yongchen Xu , Jingrui Li , Zhaohan Yi
{"title":"人类活动强烈影响下典型潮湾系统泥沙源汇过程","authors":"Yang Wang , Rijun Hu , Xiaodong Zhang , Jiandong Qiu , Naishuang Bi , Longhai Zhu , Yongchen Xu , Jingrui Li , Zhaohan Yi","doi":"10.1016/j.margeo.2025.107564","DOIUrl":null,"url":null,"abstract":"<div><div>Tidal inlet bays are regions of intense material and energy exchange between the land and the sea. In this study, based on surface sediment grain size, geochemistry, bathymetric topography, and 1354 satellite images from 1984 to 2022, we used numerical modeling, bathymetric comparison methods to examine the sediment transport, sediment provenance, and relative contributions in the Dingzi Bay area. It summarizes the source-sink patterns under intense human activities. Dingzi Bay is predominantly erosive, with differences in the erosion and deposition of tidal flats on both sides of the bay, characterized by erosion on the north tidal flat and deposition on the south tidal flat. The main sources of bay sediments are river sediment transport and erosion from the north coast. The south tidal flat inside the bay and the south beach outside the bay are the few sink areas in the bay. The sediment transport path in the study area is from river sediments transported into the bay, with some bay sediments being moved out of the bay with the ebb current. Eroded sediments from the north beach are transported along the coast to the bay mouth, and some sediments are moved into the bay with the flood current. Intense human activities in the river basin leading to a reduction in terrestrial sediment supply are the main cause of bay erosion, and the ebb current-dominated tidal current further exacerbates the erosion of the bay.</div></div>","PeriodicalId":18229,"journal":{"name":"Marine Geology","volume":"486 ","pages":"Article 107564"},"PeriodicalIF":2.6000,"publicationDate":"2025-04-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Sediment source - sink processes in a typical tidal inlet bay system under intense human activities, Dingzi Bay, China\",\"authors\":\"Yang Wang , Rijun Hu , Xiaodong Zhang , Jiandong Qiu , Naishuang Bi , Longhai Zhu , Yongchen Xu , Jingrui Li , Zhaohan Yi\",\"doi\":\"10.1016/j.margeo.2025.107564\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Tidal inlet bays are regions of intense material and energy exchange between the land and the sea. In this study, based on surface sediment grain size, geochemistry, bathymetric topography, and 1354 satellite images from 1984 to 2022, we used numerical modeling, bathymetric comparison methods to examine the sediment transport, sediment provenance, and relative contributions in the Dingzi Bay area. It summarizes the source-sink patterns under intense human activities. Dingzi Bay is predominantly erosive, with differences in the erosion and deposition of tidal flats on both sides of the bay, characterized by erosion on the north tidal flat and deposition on the south tidal flat. The main sources of bay sediments are river sediment transport and erosion from the north coast. The south tidal flat inside the bay and the south beach outside the bay are the few sink areas in the bay. The sediment transport path in the study area is from river sediments transported into the bay, with some bay sediments being moved out of the bay with the ebb current. Eroded sediments from the north beach are transported along the coast to the bay mouth, and some sediments are moved into the bay with the flood current. Intense human activities in the river basin leading to a reduction in terrestrial sediment supply are the main cause of bay erosion, and the ebb current-dominated tidal current further exacerbates the erosion of the bay.</div></div>\",\"PeriodicalId\":18229,\"journal\":{\"name\":\"Marine Geology\",\"volume\":\"486 \",\"pages\":\"Article 107564\"},\"PeriodicalIF\":2.6000,\"publicationDate\":\"2025-04-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Marine Geology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0025322725000891\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Marine Geology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0025322725000891","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Sediment source - sink processes in a typical tidal inlet bay system under intense human activities, Dingzi Bay, China
Tidal inlet bays are regions of intense material and energy exchange between the land and the sea. In this study, based on surface sediment grain size, geochemistry, bathymetric topography, and 1354 satellite images from 1984 to 2022, we used numerical modeling, bathymetric comparison methods to examine the sediment transport, sediment provenance, and relative contributions in the Dingzi Bay area. It summarizes the source-sink patterns under intense human activities. Dingzi Bay is predominantly erosive, with differences in the erosion and deposition of tidal flats on both sides of the bay, characterized by erosion on the north tidal flat and deposition on the south tidal flat. The main sources of bay sediments are river sediment transport and erosion from the north coast. The south tidal flat inside the bay and the south beach outside the bay are the few sink areas in the bay. The sediment transport path in the study area is from river sediments transported into the bay, with some bay sediments being moved out of the bay with the ebb current. Eroded sediments from the north beach are transported along the coast to the bay mouth, and some sediments are moved into the bay with the flood current. Intense human activities in the river basin leading to a reduction in terrestrial sediment supply are the main cause of bay erosion, and the ebb current-dominated tidal current further exacerbates the erosion of the bay.
期刊介绍:
Marine Geology is the premier international journal on marine geological processes in the broadest sense. We seek papers that are comprehensive, interdisciplinary and synthetic that will be lasting contributions to the field. Although most papers are based on regional studies, they must demonstrate new findings of international significance. We accept papers on subjects as diverse as seafloor hydrothermal systems, beach dynamics, early diagenesis, microbiological studies in sediments, palaeoclimate studies and geophysical studies of the seabed. We encourage papers that address emerging new fields, for example the influence of anthropogenic processes on coastal/marine geology and coastal/marine geoarchaeology. We insist that the papers are concerned with the marine realm and that they deal with geology: with rocks, sediments, and physical and chemical processes affecting them. Papers should address scientific hypotheses: highly descriptive data compilations or papers that deal only with marine management and risk assessment should be submitted to other journals. Papers on laboratory or modelling studies must demonstrate direct relevance to marine processes or deposits. The primary criteria for acceptance of papers is that the science is of high quality, novel, significant, and of broad international interest.