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Springer Oceanography Yonggang Jia Xiaolei Liu Shaotong Zhang Hongxian Shan Jiewen Zheng Wave-Forced Sediment Erosion and Resuspension in the Yellow River Delta Springer Oceanography TheSpringerOceanographyseriesseekstopublishabroadportfolioofscientificbooks, aimingatresearchers,students,andeveryoneinterestedinmarinesciences.Theseries includes peer-reviewed monographs, edited volumes, textbooks, and conference proceedings. It covers the entire area of oceanography including, but not limited to, Coastal Sciences, Biological/Chemical/Geological/Physical Oceanography, Paleo- ceanography,andrelatedsubjects. More information about this series at http://www.springer.com/series/10175 Yonggang Jia Xiaolei Liu (cid:129) (cid:129) Shaotong Zhang Hongxian Shan (cid:129) (cid:129) Jiewen Zheng Wave-Forced Sediment Erosion and Resuspension in the Yellow River Delta 123 YonggangJia Xiaolei Liu Shandong Provincial KeyLaboratory Shandong Provincial KeyLaboratory of Marine EnvironmentandGeological of Marine EnvironmentandGeological Engineering, Collegeof Environmental Engineering, Collegeof Environmental Science andEngineering Science andEngineering Ocean University of China Ocean University of China Qingdao,Shandong,China Qingdao,Shandong,China ShaotongZhang Hongxian Shan Collegeof Marine Geosciences Shandong Provincial KeyLaboratory Ocean University of China of Marine EnvironmentandGeological Qingdao,Shandong,China Engineering, Collegeof Environmental Science andEngineering Jiewen Zheng Ocean University of China Pilot National Laboratory for Marine Qingdao,Shandong,China Science andTechnology(Qingdao) Qingdao,Shandong,China ISSN 2365-7677 ISSN 2365-7685 (electronic) SpringerOceanography ISBN978-981-13-7031-1 ISBN978-981-13-7032-8 (eBook) https://doi.org/10.1007/978-981-13-7032-8 JointlypublishedwithShanghaiJiaoTongUniversityPress,Shanghai,China TheprinteditionisnotforsaleinMainlandChina.CustomersfromMainlandChinapleaseorderthe printbookfrom:ShanghaiJiaoTongUniversityPress. LibraryofCongressControlNumber:2019934364 ©ShanghaiJiaoTongUniversityPressandSpringerNatureSingaporePteLtd.2020 Thisworkissubjecttocopyright.AllrightsarereservedbythePublishers,whetherthewholeorpart of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission orinformationstorageandretrieval,electronicadaptation,computersoftware,orbysimilarordissimilar methodologynowknownorhereafterdeveloped. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publicationdoesnotimply,evenintheabsenceofaspecificstatement,thatsuchnamesareexemptfrom therelevantprotectivelawsandregulationsandthereforefreeforgeneraluse. Thepublishers,theauthors,andtheeditorsaresafetoassumethattheadviceandinformationinthis book are believed to be true and accurate at the date of publication. Neither the publishers nor the authorsortheeditorsgiveawarranty,expressorimplied,withrespecttothematerialcontainedhereinor for any errors or omissions that may have been made. The publishers remains neutral with regard to jurisdictionalclaimsinpublishedmapsandinstitutionalaffiliations. ThisSpringerimprintispublishedbytheregisteredcompanySpringerNatureSingaporePteLtd. The registered company address is: 152 Beach Road, #21-01/04 Gateway East, Singapore 189721, Singapore Preface Sediment erosion and resuspension is a process in which soil particles on the surfaceoftheseabedareactivatedbyhydrodynamicforceandeventuallyenterthe overlying water body. It is the root cause of beach evolution as well as channel erosion and siltation, an important cause of instability of offshore engineering structures, and an important path of releasing and transporting seabed buried pol- lutantstothewaterbody.Accuratepredictionofsedimenterosionandresuspension process has been a challenge for coastal engineers and scholars. The traditional view is that sediment erosion and resuspension is induced by wave-current combined shear stress, and the quantitative evaluation method is mainly based on the balance between erosion force and erosion resistance. However,inawave-dominanthydrodynamicenvironment,thefine-grainedseabed ispronetoaccumulationofporewaterpressureandevenseabedliquefactionunder the action of wave loading. Such characteristic of wave–seabed interaction causes constantchangesinthecomposition,structure,physical,andmechanicalproperties of the seabed sediments, and thus further affects the erosion and resuspension processofsediments.Duetothecomplexityoftheprocessandtheinterdisciplinary nature of the problem, there is not only a lack of systematic understanding of the physical mechanism but also a lack of a highly universal computational model for quantitativepredictionofthesedimenterosionandresuspensionundersuchwave– seabed interaction, which seriously constrains the development of offshore engi- neering calculations and numerical simulations. In this monograph, the Yellow River Delta was selected as the research area. Withthefundingofmultipleprojects,wecombinedinsitulong-termobservations, fieldinvestigations,laboratory simulation experiments, andtheoretical calculations to systematically study the physical mechanism by which wave-induced liquefac- tionoffine-grainedseabedaffectssedimenterosionandresuspension.Basedonthe understanding of the mechanism, we modified the traditional shear erosion model and proposed a calculation model of liquefaction erosion. Finally, we verified the v vi Preface applicability of the model by comparison with measured data and used the new modeltocalculateandpredictthesedimenterosionandresuspension,sourceratios, and their influence on long-term beach evolution in the Chengdao sea area of the Yellow River Delta under different sea conditions. The research results of this monograph are of great scientific values to understanding the dynamic changes ofthefine-grained seabed sedimentsinresponsetowaves,analysisand evaluation of the engineering geological environment conditions of the seabed, prediction, prevention, and control of geological disasters in the estuary delta, and under- standingtheresuspension,long-distancetransport,andfateofsedimentsfromrivers into the sea. This monograph consists of eight chapters. Chapter 1 mainly introduces the research progress in related fields. Chapter 2 mainly introduces the engineering geological environment and sediment properties of the Yellow River Delta as a representativeresearcharea,includingtheformationandevolution,topographyand geomorphology, and marine dynamic environment of the modern Yellow River Delta,andthesedimenttypes,distribution,geologicalstrata,grainsizecomposition characteristics, mineral composition characteristics, microstructure characteristics, and physical and mechanical properties. Chapter 3 introduces the current erosion status in the Yellow River Delta, including the current status of erosion in the intertidal zone and on the underwater delta. Chapter 4 introduces the erodibility characteristicofseabedsedimentsinthetypicalstudyareaofdeltalobesformedin different sedimentary ages in the Yellow River Delta. Chapter 5 introduces the occurrence process ofsedimentresuspension inthe Yellow River Delta. Chapter 6 introducesthewave-inducedporepressureresponseinrelationtosedimenterosion and resuspension in the Yellow River Delta. Chapter 7 introduces the physical mechanismsofsedimenterosionandresuspensionintheYellowRiverDeltaunder the action of waves. Chapter 8 introduces the theoretical prediction of wave-induced sediment erosion and resuspension in the Yellow River Delta. Thecontentscoveredinthisbookincludemajorresearchoutcomesofnumerous research projects sponsored by National Natural Science Foundation of China (40876042; 41072215; 41072316; 41402253; 41427803), Qingdao National Laboratory for Marine Science and Technology (QNLM2016ORP0110). Several postgraduate students from the Shandong Provincial Key Laboratory of Marine Environmental and Geological Engineering participated in relevant research work, includingXiangmeiMeng,ZhongnianYang,LeiGuo,LipingZhang,ChaoqiZhu, Mingzheng Wen, Hong Zhang, etc. The editors in charge of this book Dan Li and XiaofeiLialsocontributedgreateffortforthesmoothpublicationofthisbook.Iam grateful to Prof. Dong-Sheng Jeng (School of Engineering, Griffith University, Australia) for his kind support and help during the completion of the monograph. We hereby express our sincere gratitude to them. The study on wave-induced sediment erosion and resuspension on fine-grained seabed represented by the Yellow River Delta is the intersection of estuarine sed- iment dynamics, marine soil mechanics, and marine geology. Although we have Preface vii triedhardtodosometentativeresearch,aslimitedbytheauthors’academicrealm, levelofknowledge,andthecomplexityoftheacademicproblemsstudied,thereare inevitablysome inadequacies inthebook. Wesincerelyrequestreaders tocriticize and correct. Qingdao, China Yonggang Jia January 2019 Contents 1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 1.1 Sediment Dynamics in the World’s Major Estuaries . . . . . . . . . . . 1 1.2 Sediment Erosion and Resuspension . . . . . . . . . . . . . . . . . . . . . . 2 1.3 Research Advance . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 1.3.1 Research Advance on Sediment Erosion and Resuspension. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 1.3.2 Research Advance on Wave-Induced Seabed Response . . . 9 1.3.3 Research Advance of Sediment E&R Considering Wave-Seabed Response . . . . . . . . . . . . . . . . . . . . . . . . . . 14 1.3.4 Research Advance of Sediment E&R in the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 1.4 Outline of the Book . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21 2 Geo-Marine Environment and Sediment Properties of the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . 25 2.1 Overview. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 2.2 Formation and Evolution of the Modern Yellow River Delta . . . . 26 2.2.1 Geographical Range. . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 2.2.2 Historical Sediment Discharge . . . . . . . . . . . . . . . . . . . . . 27 2.2.3 Channel Changes. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28 2.2.4 Coastline Change. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28 2.3 Topography and Geomorphology of the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 32 2.3.1 Topography. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 32 2.3.2 Geomorphology. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 33 2.4 Marine Dynamics in the Modern Yellow River Delta . . . . . . . . . . 37 2.4.1 Meteorology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 2.4.2 Waves. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 2.4.3 Tide . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38 ix x Contents 2.4.4 Currents . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40 2.4.5 Storm Surge . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 43 2.5 Seabed Sediment Properties of the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45 2.5.1 Sediment Types and Distribution in the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45 2.5.2 Geological Strata. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 46 2.5.3 Sediment Grain Size and Mineral Composition . . . . . . . . . 47 2.5.4 Sediment Microstructure . . . . . . . . . . . . . . . . . . . . . . . . . 52 2.5.5 Physical and Mechanical Properties of Sediment . . . . . . . . 56 2.6 Summary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 59 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 3 Erosion Survey of the Modern Yellow River Delta. . . . . . . . . . . . . . 65 3.1 Overview. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 65 3.2 Erosion Survey of a Typical Coast . . . . . . . . . . . . . . . . . . . . . . . 66 3.2.1 Methodology. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 66 3.2.2 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 69 3.2.3 Analysis of Coastal Erosion . . . . . . . . . . . . . . . . . . . . . . . 72 3.3 Erosion Survey of the Subaqueous Delta . . . . . . . . . . . . . . . . . . . 84 3.3.1 Methodology. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 84 3.3.2 Historical Erosion and Deposition Evolution of the Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 84 3.3.3 Impact of Storm Surge on Subaqueous Delta Erosion . . . . 87 3.4 Summary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 95 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 95 4 Erodibility of Seabed Sediments in the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 97 4.1 Overview. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 97 4.2 Flume Measurements of Sediment Erodibility . . . . . . . . . . . . . . . 98 4.2.1 Methodology. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 98 4.2.2 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 102 4.2.3 The Spatial Difference of Sediment Erodibility . . . . . . . . . 104 4.2.4 The Effect of Sediment Physical-Mechanical Properties on Erodibility . . . . . . . . . . . . . . . . . . . . . . . . . 104 4.2.5 The Effect of Crab-Burrows on Erodibility . . . . . . . . . . . . 107 4.3 CSM Measurements of Sediment Erodibility . . . . . . . . . . . . . . . . 108 4.3.1 Methodology. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 108 4.3.2 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 110 4.3.3 Implications for Erosional Landforms of the Modern Yellow River Delta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 115

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