简介：Hydrodynamiccharactersonahorizontal,thin,rigidplatelocatedbeneaththefreesurfacearenumericallyinvestigated.Assumingalinear,time-harmonicpotentialflowandutilizingGreenidentity,thegoverningLaplaceequationcanbesimplifiedintoFredholmintegralequationofthesecondkind.Supposinglinear-orderdiscontinuouselementsalongintersectingverticalboundaries,andbyuseoftheboundaryelementmethod,numericalsolutionaboutsourcestrengthdistributionontheplatecanbechangedintoaseriesofalgebraicequations.The3DGreenfunctionisintroducedtosetuptheintegralequations,andtheGMRESsolverisperformedforsolvingthelargedenselinearsystemofequations.Theadded-mass,dampingforceandexcitingforceareevaluateddirectlyfromtheequations.Itisfoundthattheadded-masscoefficientbecomesnegativeforarangeoffrequencieswhentheplateissufficientlyclosetothefreesurface.

简介：Thepurposeofthispaperistodevelopafunctionalmethodfordesigningaseriesofsubmergedbreakwatersonpracticaltopography.ThemethodisusedtoverifythefeasibilityandeffectivenessofBraggbreakwatersforcoastalprotectionbyusingfieldtopography.ThefirstpartofthispaperprovidesdefinitionsandproceduresneededinthedesignprocessforapplyingthemechanismofBraggreflection.Next,Braggbreakwatersaredesignedonthebasisofthecross-sectionaltopographyandthenontheplanetopographyoftheMi-Tuocoastbyfollowingtheproposedprocessandprocedure.Numericalmodeling(Hsuetal.,2003;WenandTsai,2008)wasusedasadesignandassessmenttool.Finally,theeffectivenessandfeasibilityofaBraggbreakwaterwasassessedbypracticalcases.BasedonthemechanismofBraggreflection,anoptimumlayoutforaseriesofsubmergedbreakwatersisproposedtoprotecttheMi-Tuocoast.Theresultsindicatethattheproperlayoutofaseriesofsubmergedcreakwaterscanachievetheobjectiveofbeachprotection.

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简介：暴露于波浪的跨岸的沉积运输率为沿海的形态学，象防波堤那样的海洋的结构的设计，突堤，防波提等等，和由于onoff岸沉积交通的沿海的侵蚀和生长的预防是很重要的。在现在的学习，跨岸的沉积运输的实验与1/8，1/10和1/15的起始的沙滩斜坡在一条实验室波浪隧道被执行。由使用常规波浪，不同深海的波浪险峻由一个踏脚板类型波浪生成器产生了，沙滩的几何特征在影响开关岸沉积运输的暴风雨条件和参数下面介绍与d50=0.25的中等直径为沙滩材料被调查，0.32，0.45，0.62和0.80公里。近海酒吧几何特征是从海岸线的水平距离到酒吧开始(Xb)，冠(Xt)，并且(Xs)结束指，从酒吧冠的深度到静止的水水平(ht)，并且酒吧体积(V酒吧)。当时，试验性的结果显示了那深海的险峻(H0/L0)增加，到海滨的网运动增加了。与增加的波浪险峻，移动附此从静止的水拓宽垂直距离的酒吧铺平到酒吧开始(Xb)，冠(Xt)并且结束(Xs)从海岸的点和水平距离排队到酒吧开始，冠和结束的点增加了。它也从试验性的结果被显示出来自开始并且结束点到海岸线的酒吧的水平距离与沙滩斜坡的减少增加了。从这研究获得的试验性的结果与以前的试验性的工作相比并且发现具有象试验性的大小的一样的大小并且跟随期望的基本趋势。

简介：—Theresultsofdesignandexperimentofasubmergedsemi-circularbreakwaterattheYangtzeestuaryshowthatthesubmergedstructurewillbeunsafewhenthegeneralempiricalwaveforceformulaforsemi-circularbreakwaterisusedindesign.Therefore,anewcalculationmethodforthewaveforcesact-ingonasubmergedsemi-circularstructureisgiveninthispaper,inwhichthewaveforceactingonthein-sidecircumferenceofsemi-circulararchisincluded,andthephasemodificationcoefficientinthegeneralempiricalformulaisadjustedaswell.Thenewwaveforcecalculationmethodhasbeenverifiedbythere-sultsofsevenrelatedphysicalmodeltestsandadoptedinthedesignofthesouthesturaryjettyofthefirststageprojectofDeepChannelImprovementProjectoftheYangtzeRiverEstuary,thetotaljettylengthbe-ing17.5km.

简介：Thispaperdiscussessomeprevious,andpresentssomenewexperimentalresultsonwavetransmissionoversubmergedbreakwaters.Theobjectiveofthisstudyistoevaluatewavetransmissioncoefficientanddevelopatwo-dimensional(2D)modelasanimprovementtotheexistingwavetransmissioncoefficientmodels.Factorswhichaffectwavetransmissionoversubmergedbreakwatersarediscussedthroughaseriesoflaboratoryexperiments.Basicrecommendationsforevaluationanddesignofsubmergedrubble-monudbreakwatersarepresented.Fromthetestresults,acalculationformulaofwavetransmissioncoefficientisproposed.

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简介：Thenumericalinvestigationofregularwavesinteractingwithasubmergedhorizontaltwin-platebreakwaterispresentedinthispaper.Anumericalmodelwithanabsorbingwave-makerisestablishedbasedontheVOFmethod.Thevalidityofthemodelisverifiedbyexperimentalresults.Comparisonsbetweenthenumericalandexperimentalresultsshowthatboththewatersurfaceprofilesandthewave-inducedpressurescanbemodeledaccurately.Wavedeformationoverthebreakwater,waterparticlevelocitiesaroundthebreakwater,andthewave-inducedpressuresonthestructurearenumericallyinvestigated.Thepressureamplitudesofthefundamentalandsecondharmonicsonthemodelsurfaceareexaminedinvariouswaterdepths.Thecomputedandexperimentalresultshaverevealedthatthehigherfrequencycomponentsaregeneratedattheonshoresideofthebreakwater.Furthermore,thecomputedresultsdemonstrateacirculatingflowformedattheonshoresideofthebreakwater.

简介：由于胭脂波浪的物理机制的复杂性，rogue-wavestructure相互作用问题的理论学习仍然取得很少进步。为常规形状的结构，然而，给理论分析是可能的，如果流氓波浪的一个相对简单的模型被使用。波浪负担，由作为胭脂波浪的一个直觉的基本模型被知道的一个集中的波浪导致了，在沉没半的柱体之上被学习经分解。集中的波浪由高斯信封波浪是近似的，包含流氓波浪的大多数特征的一个理想的模型。衍射速度潜力通过水平力量的流动地，和公式的分离被导出，弯曲时刻被建议。导出的公式适当地被简化，并且对数字结果通过比较验证了。另外，参数的影响集中的沉没深度和波浪例如集中的度，放，彻底地被调查。

简介：Investigatingthewavefieldnearstructuresincoastalandoffshoreengineeringisofincreasingsignificance.Inthepresentstudy,simulationisdoneofthewaveprofileandflowfieldforwavespropagatingoversubmergedbars,usingPLIC-VOF(PiecewiseLinearInterfaceConstruction)totracethefreesurfaceofwaveandfinitedifferencemethodtosolvevertical2DNavier-Stokes(N-S)equations.AcomparisonofthenumericalresultsfortwokindsofsubmergedbarswiththeexperimentalonesshowsthatthePLIC-VOFmodelusedinthisstudyiseffectiveandcancomputethewavefieldprecisely.

简介：BasedonthesimulationwiththeOcean-AtmosphereCoupledModelCCSMandOceanModelPOPunderthegreenhousegasemissionscenariooftheIPCCSRESA2(IPCC,2001),andontheearthcrustsubsidenceandglaciermeltingdata,therelativesealevelchangeisobtainedalongthecoastofChinainthe21stcentury.UsingtheSRTMelevationdatathesubmergenceofcoastallowlandiscalculatedundertheextremewaterlevelwitha100-yearreturnperiod.Thetotalfloodingareasare98.3×103and104.9×103km2for2050and2080,respectively.Forthethreeregionsmostvulnerabletoextremesealevelrise,i.e.,thecoastofBohaiBay,theYangtzeRiverDeltatogetherwithneighboringJiangsuProvinceandnorthernZhejiangProvince,andthePearlRiverDelta,thefloodedareasare5.0×103,64.1×103and15.3×103km2in2050and5.2×103,67.8×103and17.2×103km2in2080,respectively.

简介：全部的推迟的微粒(TSP)样品沿着Qingdao的海岸在三个地点被收集，中国，在前并且在在2002年3月的主要尘暴期间。为比较，PM_(10)(有空气动力学的直径的微粒物质不到10μm)样品被收集三个地点赎回。词法观察和体积和单个粒子的组合分析被使用扫描与为TSP和PM_(10)的散X光检查系统(SEM/EDX)取样的一个精力装备的电子显微镜学执行。结果证明形态学的不同类型的粒子有类似的形态学的不同元素的作文，而是粒子总是没为非灰尘样品有一样的元素的作文。非灰尘粒子的Themorphology和作文在不同地点是不同的。分数维、球形的粒子为非灰尘样品主要在粗粒级存在，当时在好模式(<10μm)有絮状物，一起结队并且包含外壳的元素的好粒子形成。与非灰尘粒子相比，尘粒以形态学，颗粒大小和作文是更同类的。有andwell分布式的尺寸在灰尘样品统治了的不规则的形状的粒子，包含象Mg那样的外壳的元素，艾尔，Si，Ca，Fe，等等。高硫内容显示了那同类并且多相反应在Qingdao的特定的环境发生在尘粒的表面上。

简介：Settlingvelocityisafundamentalparameterinsedimenttransportdynamics.ForuniformPar-ticles,thereareabundantformulasforcalculationoftheirsettlingvelocities.Butinnaturalfields,sedi-mentconsistsofnon-uniformparticles.Theinteractionamongparticlesiscomplexandshouldnotbeneg-lected.Inthispaper,basedontheanalysisofsettlingmechanismofnon-cohesiveandnon-uniformparti-cles,atheoreticalmodeltodescribesettlingmechanismisproposed.Besidessuspensionconcentrationandupwardturbulentflowcausedbyotherparticles,collisionamongparticlesisanothermainfactorinflu-encingsettlingvelocity.Byintroducingthecollisiontheory,equationsoffallvelocitybeforecollision,colli-sionprobability,andfallvelocityaftercollisionareestablished.Finally,aformulausedtocalculatetheset-tlingvelocityofnon-cohesiveparticleswithwidegraingradationispresented,whichagreeswellwiththeexperimentaldata.

简介：Basedontheanalysisoftropicalcyclone(TC)databaseintheNorthwestPacific(NWP)from1945to2008,wenotonlyextractthetemporalvariationofTCintensityandfrequency,butalsogivetheirspatialdistributionbothintheNWPandintheSouthChinaSea(SCS).TheresultsshowthatthereisanobservationalincreaseofTCactivities,whichmanifestsastheenhancementofthepowerdissipationindex(PDI)andthegrowthofTCfrequency,especiallyfortyphoonsandstrongtyphoons.TheinhomogeneousspatialdistributionsofTCfrequencyandintensityarealsoprovidedbothintheNWPandintheSCS.Forexample,theregionofZhongshaIslandsandDongshaIslandsintheSCS(15°～22°N,115°～120°E),westtothePhilippineIslandsistheplacewithfrequentoccurrenceofstrongtyphoons,amongwhichthewindspeedof7TCsin64yearsexceeds60m/s.

简介：Naturalhazardssuchashurricanesmaycauseextensiveeconomiclossesandsocialdisruptionforcivilstructuresandinfrastructuresincoastalareas,implyingtheimportanceofunderstandingtheconstructionperformancesubjectedtohurricanesandassessingthehurricanedamagesproperly.Theintensityandfrequencyofhurricaneshavebeenreportedtochangewithtimeduetothepotentialimpactofclimatechange.Inthispaper,aprobability-basedmodelofhurricanedamageassessmentforcoastalconstructionsisproposedtakingintoaccountthenon-stationarityinhurricaneintensityandfrequency.Thenon-homogeneousPoissonprocessisemployedtomodelthenon-stationarityinhurricaneoccurrencewhilethenon-stationarityinhurricaneintensityisreflectedbythetime-variantstatisticalparameters（e.g.,meanvalueand/orstandarddeviation）,withwhichthemeanvalueandvariationofthecumulativehurricanedamageareevaluatedexplicitly.TheMiami-DadeCounty,Florida,USA,ischosentoillustratethehurricanedamageassessmentmethodproposedinthispaper.Theroleofnon-stationarityinhurricaneintensityandoccurrencerateduetoclimatechangeinhurricanedamageisinvestigatedusingsomerepresentativechangingpatternsofhurricaneparameters.

简介：AerosolsampleswerecollectedonboardtheresearchvesselXuelongduringtheFifteenthChineseAntarcticResearchExpedition(CHINAREXV)inNovember1998-April1999andtheFirstChineseArcticResearchExpeditioninJuly-September1999.TheareastraversedbytheexpeditionarycruisesincludetheArcticOcean,thewesternNorthPacificOceanandtheeasternIndianOcean,covering75°N-69°Sand75°E-133°W.AerosolsampleswerealsotakenattheChineseZhongshanStationinEastAntarcticaduringtheCHINAREXV.Analysisofthesamplesyieldedconcentrationsofnon-sea-saltsulfateandothersolublechemicalspeciesinthemarineboundarylayer.Thedatasuggestthatthechemicalcompositionofthemarineaerosolsisinfluencedbythreemajorsources:continentalairmasses,primaryoceanicemissions,andsecondarymarineaerosolsoriginatedfromoceanicemissions.Theresultsshowthat,awingtostronganthropogenicsulfuremissionsfromtheAsiancontinent,non-sea-saltsulfateconcentrationsintheNorthernHemisphere(thewesternNorthPacific)marineaerosolaresignificantlyhigherthanthoseintheSouthernHemisphere(theeasternIndianOcean).Aerosolnon-sea-saltsulfateconcentrationsappeartobeinverselycorrelatedwithaerosolnon-sea-saltchloridewhichshowssignificantlynegativevalues,indicatingthelossofchloridebyseasalts,inmostaerosolsamples.SincegaseousHClmaybeinvolvedinchemicalreactionsthatdepleteatmosphericozoneinthemarineboundarylayer(MBL),highlevelsofacidicnon-sea-salt-sulfatereleasedbyhumanactivitiesinthelowandmid-latitudesoftheNorthernHemispheremaybecomeanimportantpotentialcontributortothelossofatmosphericozoneintheMBL.

简介：Inthispaper,thecharacteristicsofdifferentformsofmildslopeequationsfornon-linearwaveareanalyzed,andnewnon-lineartheoreticmodelsforwavepropagationarepresented,withnon-lineartermsaddedtothemildslopeequationsfornon-stationarylinearwavesanddissipativeeffectsconsidered.Numericalsimulationmodelsaredevelopedofnon-linearwavepropagationforwatersofmildlyvaryingtopographywithcomplicatedboundary,andtheeffectsarestudiedofdifferentnon-linearcorrectionsoncalculationresultsofextendedmildslopeequations.Systematicalnumericalsimulationtestsshowthatthepresentmodelscaneffectivelyreflectnon-lineareffects.

简介：InthisstudyweassessedthecurrentstatusofcoralreefsalongtheSaudiArabiancoastoftheRedSea.AmongthethreegrowthformsofAcroporidcorals,thebranchingformswerefoundtodominateintheFarassanIslands(44.55%±11.10%cover)followedbytabularformsintheDogaIslands(rangingbetween18%±6.47%and18.30%±9.47%cover).DigitateformswererarelyfoundalongthecoastexceptatMaqna.Amongthefivegrowthformsofnon-Acroporidcorals,weobservedmaximumcoverofbranchingformsintheYanbuoffshorearea(58.89%±15.11%cover)followedbytheJeddahcoast(24.76%±14.04%cover).TheMilleporaspp.,anon-Scleractiniancoral,wasabundantatallthenear-shoresites,suchasJeddah(10.70%±8.21%)andAl-Wajh(9.81%±6.69%).Thelivecoralcover(includingbothScleractinianandnon-Scleractiniancorals)ofSaudiRedSeacoastwasseentobehigherinthenorthandgraduallydecreasetowardsthesouth.PrincipalComponentanalysisshowedthatthecontributionofAcroporidcoralswasgreaterinthesouthernregionthaninthenorthernandmiddleregions,butvice-versainthecaseofnon-Acroporidcorals.Bray-Curtisclusteranalysiscategorizedallthestudysitesintotwomajorclusterswith60%similarity.Amongthem,onecluster-formingsitesfromMaqnatoMasturah(Northernregion)andthesecondonecomprisedthemiddleandsouthernregions(JeddahtoFarassanIslands),andoneoutlierRabigh.

简介：OptimalstockingdensitieswereinvestigatedfortheseacucumberApostichopusjaponicusSelenkaunderfeed-supplementandnon-feed-supplementregimesinnetenclosuresfor333d.Substantialweightlossoccurredduringtheaestivationphase(AE).Decreasedgrowthrateswerealsoobservedduringthewinterphase(WT).Incontrast,seacucumbersshowedrapidgrowthduringthespring(SP)andautumn(AU)phases.Feedingregimesconsiderablyinfluencedthegrowthperformance,i.e.,seacucumbersgrewfasterunderfeed-supplementregimethanundernon-feed-supplementregime(P<0.05).Theaveragesurvivalratesofseacucumbersunderfeed-supplementregimewerehigherthanthoseundernon-feed-supplementregimeforboththeautumnphaseandspringphase,butthedifferenceswereonlysignificantforthelatterphase(P<0.05).ThefittedB-Ncurvesshowedthattheoptimalstockingdensities,intermsofnetproduction,were22.3ind.m-2forfeed-supplementregimeand14.1ind.m-2fornon-feed-supplementregime.

简介：Seacucumbers,ApostichopusjaponicusSelenka,werefeddietscontainingnon-immunostimulant(basaldiet),0.2%β-glucanand0.02%glycyrrhizininarecirculatorywatersystemfor45days,andsubsequentlychallengedwithVibriosplendidusbyinjectionat1.0×108cfu/seacucumberfor15days.Phagocyticcapacity(PC),intracellularsuperoxideanionproduction(ISAP),ly-sozyme(LSZ)activityandsuperoxidedismutase(SOD)activityinthecoelomicfluidwereanalyzedonthe0th,5th,10thand15thdaysafterinjection.Resultsshowedthatafterthe45-dayfeedingperiod,PC,ISAP,LSZactivityandSODactivityinseacucumbersfedwithdietaryβ-glucanorglycyrrhizinweresignificantlyhigherthaninthosefedwiththebasaldiet.Onthe5thdayafterinfection,alltheimmuneparametersexaminedintheseacucumbersinjectedwithV.splendidusdecreasedinvaluesignificantly.Onthe15thday,PC,ISAPandLSZactivityreturnedtolevelssimilartothoseonthe0thday.Fortheseacucumbersinjectedwithsaline,therewerenosignificantdifferencesinalltheimmuneparametersexaminedandinthecumulativemorbidityduringthe15-daychallengingtrial.AfterinjectingwithV.splendidus,thecumulativemorbidityofseacucumbersfedwiththebasaldietwassignificantlyhigherthanthosefedwithdietaryβ-glucanorglycyrrhizinwhenchallengedwithV.splendiduschallengedseacucumberfedwiththebasaldietwassignificantlyhigherthanthosefedwithdietaryβ-glucanorglycyrrhizin.Therewasnosignificantdifferenceincumulativemorbiditybetweenthedietaryβ-glucanandglycyrrhizintreatmentsovertime.