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地理学报  2006 

长江来沙锐减与海岸滩涂资源的危机

DOI: 10.11821/xb200603007, PP. 282-288

Keywords: 河流入海泥沙,海岸滩涂,三角洲,长江

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Abstract:

利用小波分析方法对1951~2004年大通站系列水、沙和流域降水资料进行周期性和趋势性分析,利用Arc-GIS软件对长江三角洲海图进行滩涂面积计算和冲淤剖面分析,并于2002年5月~2005年7月在长江三角洲前缘的南汇岸段进行逐日潮滩高程测量,以进行三峡水库蓄水前后滩面冲淤的对比。结果表明尽管气候变化导致流域平均降水量以及大通径流量和输沙率存在2~3年和8~9年的波动周期(P<0.05),但大通输沙率从1960年代末开始出现明显的下降趋势(P<0.001),三峡工程运行后的2003年(6月开始蓄水)和2004年连续2年创历史新低,流域水库的修建是导致这一下降趋势的根本原因。长江来沙量的锐减正在导致三角洲前缘滩涂从淤涨向侵蚀转化。预测认为流域人类活动还将继续导致长江入海泥沙量的下降,今后几十年的大通输沙率将从目前的1.5×108~2×108t/a下降到1×108t/a左右;泛长江三角洲海岸滩涂资源将面临严峻挑战。

References

[1]  GoodwinP,MehtaAJ,ZedlerJB.Coastalwetlandrestoration:anintroduction.J.CoastalRes.,2001,27:1-6.
[2]  TrenhaileAS.CoastalDynamicsandLandforms.OxfordUK:OxfordUniversityPress,1997.366.
[3]  FanosAM.TheimpactofhumanactivitiesontheerosionandaccretionoftheNiledeltacoast.JournalofCoastalResearch,1995,11(3):821-833.
[4]  StanleyDJ,WarneAG.Niledeltainitsdestructionphase.JournalofCoastalResearch,1998,14(3):794-825.
[5]  ColemanJM,RobertHH,StoneGW.MississippiRiverdelta:anoverview.JournalofCoastalResearch,1998,14:698-716.
[6]  CarriquiryJD,SánchezA,Camacho-IbarVF.SedimentationinthenorthernGulfofCaliforniaaftercessationoftheColoradoRiverdischarge.SedimentaryGeology,2001,144(1-2):37-62.
[7]  Sánchez-ArcillaA,JiménezJA,ValdemoroHI.TheEbroDelta:morphodynamicsandvulnerability.JournalofCoastalResearch,1998,14(3):754-772.
[8]  BatallaRJ,GómezCM,KondolfGM.Riverimpoundmentandchangesinflowregime.EbroRiverbasin,northeasternSpain.JournalofHydrology,2004,290:117-136.
[9]  XuJiongxin.TheYellowRiverMouthextensionsince1194asinfluencedbyhumanactivities.ProgressinGeography,2001,20:1-9.
[10]  YangZS,WangHJ,SaitoYetal.PhasechangeofthemodernHuanghedeltaevolutionsinceitslastendchannelshiftin1976(anditsphasechange).In:ThanawatJarupongsakul,YoshikiSaito(eds.),5thInternationalConferenceonAsianMarineGeology,AGCP-475DeltaMAPandAPNMega-Delta,January13-18,2004,Bangkok,Thailand.256.
[11]  [罗宪林,李春初,罗章仁.海南岛南渡江三角洲的废弃与侵蚀.海洋学报,2000,22(3):55-60.]
[12]  [陈吉余,王宝灿,刘苍字.中国海岸地貌.见:陈吉余,王宝灿,虞志英主编,中国海岸发育过程和演变规律.上海:上海科技出版社,1989.18-48.]
[13]  HuFangxi,GuGuochuan,HanMingbaoetal.Characteristicsoftides,currentsandsedimenttransportationinWenzhouRegion.In:ChenJiyu,WangBaocan,YuZhiying(eds.),DevelopmentsandEvolutionofChina'sCoast.Shanghai:ShanghaiScientific&TechnicalPublishers,1989.403-415.
[14]  YangShilun,FuDejian,ChenXiaohuaetal.Tidesandtide-dominatedcoasts.In:YangShilun(ed.),AnIntroductiontoCoastalEnvironmentsandGeomorphologicalProcesses.Beijing:ChinaOceanPress,2003.87-115.
[15]  [杨世伦,傅德健,陈小华.潮汐和潮汐作用为主的海岸.见:杨世伦主编,海岸环境和地貌过程导论.北京:海洋出版社,2003.87-115.]
[16]  YangSL,ZhaoQY,BelkinIM.TemporalvariationinthesedimentloadoftheYangtzeRiverandtheinfluencesofthehumanactivities.JournalofHydrology,2002,263:56-71.
[17]  YangSL,DingPX,ChenSL.ChangesinprogradationrateofthetidalflatsatthemouthoftheChangjiangRiver,China.Geomorphology,2001,38:167-180.
[18]  YangShilun,HeSonglin.TheformationandevolutionoftheJiuduanshatidalislandaswellastheirrelationtothedevelopmentofthenorthandsouthpassagesintheYangtzeRiverEstuary.TheOceanEnigeering,1998,16(4):55-65.
[19]  [杨世伦,贺松林.长江口九段沙的形成演变及对南北槽发育的影响.海洋工程,1998,16(4):55-65.]
[20]  YuZhiying,LouFei.TheevolvementcharacteristicsofNanhuizuiforelandintheChangjiangEstuary,China.ActaOceanologicaSinica,2004,26(3):47-53.
[21]  AroraVK,BoerGJ.Effectsofsimulatedclimatechangeonthehydrologyofmajorriverbasins.J.Geophys.Res.,2001,106(D4):3335-3348.
[22]  [李九发,万新宁,陈小华等.上海滩涂后备土地资源及其可持续开发途径.长江流域资源与环境,2003,12(1):17-22.]
[23]  [许炯心.人类活动对公元1194年以来黄河河口延伸速率的影响.地理科学进展,2001,20:1-9.]
[24]  QianChunlin.EffectsofthewaterconservancyprojectsintheLuanheRiverBasinonLuanheRiverDelta,HebeiProvince.ActaGeographicaSinica,1994,49(2):158-166.
[25]  [钱春林.引滦工程对滦河三角洲的影响.地理学报,1994,49(2):158-166.]
[26]  LuoXianlin,LiChunchu,LuoZhangren.ErosionandabandonmentoftheNanduRiverDelta,HainanIsland.ActaOceanologicaSinica,2000,22(3):55-60.
[27]  EismaD.IntertidalDeposits:RiverMouths,TidalFlatsandCoastalLagoons.BocaRaton,Florida:CRCPress,1998.459.
[28]  LiB,LiC,ShenH.ApreliminarystudyonsedimentfluxintheChangjiangDeltaduringthepostglacialperiod.ScienceinChina(SeriesD),2003,46(7):743-752.
[29]  ChenJiyu,WangBaocan,LiuCangzi.CoastalgeomorphologyinChina.In:ChenJiyu,WangBaocan,YuZhiying(eds.),DevelopmentsandEvolutionofChina'sCoast.Shanghai:ShanghaiScientific&TechnicalPublishers,1989.18-48.
[30]  [胡方西、谷国传、韩明宝等.温州海区潮汐、水流及泥沙流基本特征.见:陈吉余,王宝灿,虞志英主编,中国海岸发育过程和演变规律.上海:上海科技出版社,1989.403-415.]
[31]  DaviesJL.Amorphogenicapproachtoworldshorelines.Zeit.furGeomorph.,1964,8:127-142.
[32]  YangShilun.Coastalwetland.In:YangShilun(ed.),AnIntroductiontoCoastalEnvironmentsandGeomorphologicalProcesses.Beijing:ChinaOceanPress,2003.171-186.
[33]  [杨世伦.海岸湿地.见:杨世伦主编,海岸环境和地貌过程导论.北京:海洋出版社,2003.171-186.]
[34]  TorrenceC,CompoGP.Apracticalguidetowaveletanalysis.BulletinoftheAmericanMeteorologicalSociety,1998,79:61-78.
[35]  YangSL,FriedrichsCT,DingPXetal.MorphologicalresponseoftheouterYangtzeRiverMouthtomajorstorms.Estuaries,2003,26(6):1416-1425.
[36]  DimaM,RimbuN,DimaI.Arcticoscillationvariabilitygeneratedthroughinter-oceaninteractions.Geophys.Res.Letters,2002,29.doi:10.1029/2002GL014717.
[37]  YangSL,ZhangJ,ZhuJetal.,2005.ImpactofdamsonYangtzeRiversedimentsupplytotheseaanddeltaintertidalwetlandresponse.JournalofGeophysicalResearch,2005,110(F03006).doi:10.102912004JF000271.
[38]  [虞志英,楼飞.长江口南汇嘴近岸海床近期演变分析:兼论长江流域来沙量变化的影响.海洋学报,2004,26(3):47-53.]
[39]  ManabeS,MillyPCD,WetheraldR.Simulatedlong-termchangesinriverdischargeandsoilmoistureduetoglobalwarming.Hydrol.Sci.J.,2004,49(4):625-642.
[40]  XuJX.Sedimentfluxtotheseaasinfluencedbychanginghumanactivitiesandprecipitation:exampleoftheYellowRiver,China.Environ.Manage.,2003,31(3):328-341.
[41]  LiJiufa,WanXinning,ChenXiaohuaetal.CoastallandresourcesinShanghaiwithanalysisontheirsustainableexploitation.ResourcesandEnvironmentintheYangtzeBasin,2003,12(1):17-22.

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