台湾海峡的海洋沉积环境研究进展
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摘要
台湾海峡是我国最大的海峡,也是南海与东海进行物质和能量交换的主要通道。区域内地震、台风等灾害多发,潮流作用较强,同时受黑潮分支、南海暖流和东海环流等多种水系的影响,众多的山溪性中小型河流从海峡两侧流入海洋,为海洋沉积环境的研究提供了一个天然的实验场。基于台湾海峡的沉积环境分区、台湾海峡潮成沙脊的沉积环境、山溪性河流入海沉积通量等方面进行综述,较系统地论述了目前在台湾海峡沉积环境方面所进行的研究工作,并为今后更好地研究该区域物质通量的输移过程、途径与归宿提供参考与借鉴。
The Taiwan Strait is the largest strait in China,and is also material and energy exchange's main channel between the South China Sea and the East China Sea.Disaster processes,such as earthquakes and typhoon,often occurred in the strait.The Taiwan strait has stronger tide,and is impacted by the branch of Kushiro,south China Sea warm current and East China Sea circulation,as well as a large number of small and medium-sized mountain rivers flow into oceans from both sides of the Strait,and it provides a good place for marine sedimentary environment research.We discuss some ways about the sedimentary environmental in Taiwan Strait,including sedimentary environmental district,tidal sand ridge and the sediment flux into the ocean by mountain rivers in the Taiwan Strait.It can provide a reference for studying the material flux transport process,ways and fates in the Taiwan Strait for the future.
The Taiwan Strait is the largest strait in China,and is also material and energy exchange's main channel between the South China Sea and the East China Sea.Disaster processes,such as earthquakes and typhoon,often occurred in the strait.The Taiwan strait has stronger tide,and is impacted by the branch of Kushiro,south China Sea warm current and East China Sea circulation,as well as a large number of small and medium-sized mountain rivers flow into oceans from both sides of the Strait,and it provides a good place for marine sedimentary environment research.We discuss some ways about the sedimentary environmental in Taiwan Strait,including sedimentary environmental district,tidal sand ridge and the sediment flux into the ocean by mountain rivers in the Taiwan Strait.It can provide a reference for studying the material flux transport process,ways and fates in the Taiwan Strait for the future.
引文
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[21]刘振夏,夏东兴.中国近海潮流沉积沙体[M].北京:海洋出版社,2004.
[22]杜晓琴,李炎,高抒.台湾浅滩大型沙波、潮流结构和推移质输运特征[J].海洋学报,2008,30(5):520-631.
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[27]Syvitski J P M,Saito Y.Morphodynamics of Deltas Under theInfluence of Humans[J].Global Planet Change,2007,57(3-4):261-282.
[28]Milliman J D,Lin S W,Kao S J,et al.Short-Term Changes inSeafloor Character Due to Flood-Derived Hyperpycnal Discharge:Typhoon Mindulle,Taiwan,July 2004[J].Geology,2007,35(9):779-782.
[29]Dadson S J,Hovius N,Chen H,et al.Earthquake-triggered increasein sediment delivery from an active mountain belt[J].Geology,2004,32(8):733-736.
[30]Dadson S,Hovius N,Pegg S,et al.Hyperpycnal river flows from anactive mountain belt[J].Journal of Geophysical Research,2005,110(F4016):1-13.
[31]Milliman J D,Kao S J.Hyperpycnal discharge of fluvial sediment tothe ocean:impact of super-typhoon Herb(1996)on TaiwaneseRivers[J].The Journal of Geology,2005,113(5):503-516.
[32]Kao S J,Milliman J D.Water and Sediment Discharge from SmallMountainous Rivers,Taiwan:The Roles of Lithology,EpisodicEvents and Human Activities[J].Journal of Geology,2008,116(5):431-448.
[33]Liu J P,Liu C S,Xu K H.Flux and fate of small mountainousrivers derived sediments into the Taiwan Strait[J].Marine Geology,2008,256(1-4):65-76.
[34]Lee I H,Lien R C,Liu J T,et al,Turbulent Mixing and InternalTides in Gaoping(Kaoping)Submarine Canyon,Taiwan[J].Journalof Marine Systems,2009,76(4):383-396.
[35]Lee I H,Wang Y H,Liu J T,et al.Internal Tidal Currents in theGaoping(Kaoping)Submarine Canyon[J].Journal of MarineSystems,2009,76(4):397-404.
[36]Liu J T,Hung J J,Lin H L,et al.From Suspended Particles to Strata:The Fate of Terrestrial Substances in the Gaoping(Kaoping)Submarine Canyon[J].Journal of Marine Systems,2009,76(4):417-432.
[37]Huh C A,Lin H L,Lin S W,et al.Modern Accumulation Rates anda Budget of Sediment off the Gaoping(Kaoping)River,SW Taiwan:A Tidal and Flood Dominated Depositional Environment around aSubmarine Canyon[J].Journal of Marine Systems,2009,76(4):405-416.
[38]Yu H S,Chiang C S,Shen S M.Tectonically Active SedimentDispersal System in SW Taiwan Margin with Emphasis on theGaoping(Kaoping)Submarine Canyon[J].Journal of MarineSystems,2009,76(4):369-382.
[39]Chung C H,You C F,Chu H Y.Weathering Sources in the Gaoping(Kaoping)River Catchments,Southwestern Taiwan:Insights fromMajor Elements,Sr Isotopes,and Rare Earth Elements[J].Journalof Marine Systems,2009,76(4):433-443.
[40]Fang M D,Chang W K,Lee C L,et al.The Use of PolycyclicAromatic Hydrocarbons as a Particulate Tracer in the Water Columnof Gaoping(Kaoping)Submarine Canyon[J].Journal of MarineSystems,2009,76(4):457-467.
[41]Wang R M,You C F,Chu H Y,et al.Seasonal Variability ofDissolved Major and Trace Elements in the Gaoping(Kaoping)River Estuary,Southwestern Taiwan[J].Journal of Marine Systems,2009,76(4):444-456.
[42]Horng C S,Huh C A,Chen K H,et al.Air Pollution HistoryElucidated from Anthropogenic Spherules and Their MagneticSignatures in Marine Sediments offshore of Southwestern Taiwan[J].Journal of Marine Systems,2009,76(4):468-478.
[43]Hung J J,Lu C T,Huh C A,et al.Geochemical controls ondistributions and speciation of As and Hg in sediments along theGaoping(Kaoping)Estuary-Canyon system off southwesternTaiwan[J].Journal of Marine Systems,2009,76(4):479-495.
[44]Liu C C,Chang C H,Wen C G,et al.Using Satellite Observations ofOcean Color to Categorize the Dispersal Patterns of River-BorneSubstances in the Gaoping(Kaoping)River,Shelf and CanyonSystem[J].Journal of Marine Systems,2009,76(4):496-510.
[45]汪小钦,王钦敏,邬群勇,等.遥感在悬浮物质浓度提取中的应用—以福建闽江口为例[J].遥感学报,2003,7(1):54-57.
[46]王海鹏,张培辉,陈峰,等.闽江口水下三角洲沉积特征及沉积环境I.现代沉积特征和沉积环境[J].台湾海峡,2000,19(1):113-118.
[47]刘苍宇,贾海林,陈祥锋.闽江河口沉积结构与沉积作用[J].海洋与湖沼,2001,32(2):177-184.
[48]蔡爱智,蔡月娥,朱孝宁,等.福建九龙江口入海泥沙的扩散和河口湾的现代沉积[J].海洋地质与第四纪地质,1991,11(1):57-67.
[49]蔡锋,黄敏芬,苏贤泽,等.九龙江河口湾泥沙运移特点与沉积动力机制[J].台湾海峡,1999,18(4):418-424.
[50]葛全胜,王芳,陈泮勤,等.全球变化研究进展和趋势[J].地球科学进展,2007,22(4):417-427.
[2]黄昭,王善雄.台湾海峡滨海断裂带的构造特征与活动性[J].大地测量与地球动力学,2006,26(3):16-22.
[3]Hong H S,Zhang C Y,Shang S L,et al.Interannual variability ofsummer coastal upwelling in the Taiwan strait[J].Continental ShelfResearch,2009,29(2):479-484.
[4]Wang Y H,Jan S,Wang D P.Transports and tidal current estimatesin the Taiwan Strait from shipboard ADCP observations(1999-2001)[J].Estuarine,Coastal and Shelf Science,2003,57(1-2):193-199.
[5]任明达,王乃梁.现代沉积环境概论[M].北京:科学出版社.1985.
[6]徐茂泉,陈友飞.海洋地质学[M].厦门:厦门大学出版社,1999.
[7]Boggs W,Wang Huaqing,Chen Ruqin.Structure and compo--sition of sediment model in the continental shelf of Taiwan[J].Acta Oceanography Taiwanica,1974,4:13-561.
[8]秦蕴珊,郑铁民.东海大陆架沉积物分布特征的初步探讨[C]∥黄东海地质.北京:科学出版社,1982:39-51.
[9]金翔龙.东海海洋地质[M].北京:海洋出版社,1992.
[10]周定成.台湾海峡西岸海底沉积类型的展布及其控制因素[J].海洋学报,1987,9(1):64-68.
[11]俞何兴,周颖蔚.台湾北部及西部陆架之地貌与地质特征[J].中国科学(D辑),2001,31(6):486-495.
[12]曾成开,朱永其,王秀昌.台湾海峡的底质类型与沉积分区[J].台湾海峡,1982,1(1):54-61.
[13]郭允谋,郑承忠,潘亚明.台湾海峡的现代沉积环境[C]∥台湾海峡及邻近海域海洋科学讨论会论文集.北京:海洋出版社,1995:145-153.
[14]Liu Z X,Xia D X,Berné,et al.Tidal deposition systems of China'scontinental shelf,with special reference to the eastern Bohai Sea[J].Marine Geology,1998,145(3-4):225-253.
[15]刘锡清,刘守全,王圣洁,等.南海灾害地质发育规律初探[J].中国地质灾害与防治学报,2002,13(1):12-16.
[16]郑铁民,张君元.台湾浅滩及其附近大陆架的地形和沉积特征的初步研究[C]∥黄东海地质.北京:科学出版社,1982:52-66.
[17]杨顺良.闽南-台湾浅滩渔场地形地貌与上升流的关系[C]∥闽南-台湾浅滩渔场上升流区生态系研究.北京:科学出版社,1991:39-46.
[18]马道修,刘锡清.台湾浅滩构造台地的形成与发展[J].海洋地质动态,1994,7:4-6.
[19]蓝东兆,张维林,陈承惠,等.台湾浅滩中粗砂的时代与成因[J].台湾海峡,1991,10(2):156-161.
[20]Cai A Z,Zhu X N,Li Y M,et al.Sedimentary environment inTaiwan Shoal[J].Chinese Journal of Oceanology and Limnology,1992,10(4):331-339.
[21]刘振夏,夏东兴.中国近海潮流沉积沙体[M].北京:海洋出版社,2004.
[22]杜晓琴,李炎,高抒.台湾浅滩大型沙波、潮流结构和推移质输运特征[J].海洋学报,2008,30(5):520-631.
[23]范开国,黄韦艮,贺明霞,等.SAR浅海水下地形遥感研究进展[J].遥感技术与应用,2008,23(4):479-485.
[24]Liao H R,Yu H S.Morphology,hydrodynamics and sedimentcharacteristics of the Changyun Sand Ridge offshore westernTaiwan[J].Terrestrial,Atmospheric and Oceanic Sciences,2005,16(3):621-640.
[25]Liao H R,Yu H S,Su C C.Morphology and sedimentation of sandbodies in the tidal shelf sea of eastern Taiwan Strait[J].MarineGeology,2008,248(3-4):161-178.
[26]Milliman J D,Syvitski J P M.Geomorphic/tectonic control ofsediment discharge to the ocean:the importance of smallmountainous rivers[J].The Journal of Geology,1992,100(5):525-544.
[27]Syvitski J P M,Saito Y.Morphodynamics of Deltas Under theInfluence of Humans[J].Global Planet Change,2007,57(3-4):261-282.
[28]Milliman J D,Lin S W,Kao S J,et al.Short-Term Changes inSeafloor Character Due to Flood-Derived Hyperpycnal Discharge:Typhoon Mindulle,Taiwan,July 2004[J].Geology,2007,35(9):779-782.
[29]Dadson S J,Hovius N,Chen H,et al.Earthquake-triggered increasein sediment delivery from an active mountain belt[J].Geology,2004,32(8):733-736.
[30]Dadson S,Hovius N,Pegg S,et al.Hyperpycnal river flows from anactive mountain belt[J].Journal of Geophysical Research,2005,110(F4016):1-13.
[31]Milliman J D,Kao S J.Hyperpycnal discharge of fluvial sediment tothe ocean:impact of super-typhoon Herb(1996)on TaiwaneseRivers[J].The Journal of Geology,2005,113(5):503-516.
[32]Kao S J,Milliman J D.Water and Sediment Discharge from SmallMountainous Rivers,Taiwan:The Roles of Lithology,EpisodicEvents and Human Activities[J].Journal of Geology,2008,116(5):431-448.
[33]Liu J P,Liu C S,Xu K H.Flux and fate of small mountainousrivers derived sediments into the Taiwan Strait[J].Marine Geology,2008,256(1-4):65-76.
[34]Lee I H,Lien R C,Liu J T,et al,Turbulent Mixing and InternalTides in Gaoping(Kaoping)Submarine Canyon,Taiwan[J].Journalof Marine Systems,2009,76(4):383-396.
[35]Lee I H,Wang Y H,Liu J T,et al.Internal Tidal Currents in theGaoping(Kaoping)Submarine Canyon[J].Journal of MarineSystems,2009,76(4):397-404.
[36]Liu J T,Hung J J,Lin H L,et al.From Suspended Particles to Strata:The Fate of Terrestrial Substances in the Gaoping(Kaoping)Submarine Canyon[J].Journal of Marine Systems,2009,76(4):417-432.
[37]Huh C A,Lin H L,Lin S W,et al.Modern Accumulation Rates anda Budget of Sediment off the Gaoping(Kaoping)River,SW Taiwan:A Tidal and Flood Dominated Depositional Environment around aSubmarine Canyon[J].Journal of Marine Systems,2009,76(4):405-416.
[38]Yu H S,Chiang C S,Shen S M.Tectonically Active SedimentDispersal System in SW Taiwan Margin with Emphasis on theGaoping(Kaoping)Submarine Canyon[J].Journal of MarineSystems,2009,76(4):369-382.
[39]Chung C H,You C F,Chu H Y.Weathering Sources in the Gaoping(Kaoping)River Catchments,Southwestern Taiwan:Insights fromMajor Elements,Sr Isotopes,and Rare Earth Elements[J].Journalof Marine Systems,2009,76(4):433-443.
[40]Fang M D,Chang W K,Lee C L,et al.The Use of PolycyclicAromatic Hydrocarbons as a Particulate Tracer in the Water Columnof Gaoping(Kaoping)Submarine Canyon[J].Journal of MarineSystems,2009,76(4):457-467.
[41]Wang R M,You C F,Chu H Y,et al.Seasonal Variability ofDissolved Major and Trace Elements in the Gaoping(Kaoping)River Estuary,Southwestern Taiwan[J].Journal of Marine Systems,2009,76(4):444-456.
[42]Horng C S,Huh C A,Chen K H,et al.Air Pollution HistoryElucidated from Anthropogenic Spherules and Their MagneticSignatures in Marine Sediments offshore of Southwestern Taiwan[J].Journal of Marine Systems,2009,76(4):468-478.
[43]Hung J J,Lu C T,Huh C A,et al.Geochemical controls ondistributions and speciation of As and Hg in sediments along theGaoping(Kaoping)Estuary-Canyon system off southwesternTaiwan[J].Journal of Marine Systems,2009,76(4):479-495.
[44]Liu C C,Chang C H,Wen C G,et al.Using Satellite Observations ofOcean Color to Categorize the Dispersal Patterns of River-BorneSubstances in the Gaoping(Kaoping)River,Shelf and CanyonSystem[J].Journal of Marine Systems,2009,76(4):496-510.
[45]汪小钦,王钦敏,邬群勇,等.遥感在悬浮物质浓度提取中的应用—以福建闽江口为例[J].遥感学报,2003,7(1):54-57.
[46]王海鹏,张培辉,陈峰,等.闽江口水下三角洲沉积特征及沉积环境I.现代沉积特征和沉积环境[J].台湾海峡,2000,19(1):113-118.
[47]刘苍宇,贾海林,陈祥锋.闽江河口沉积结构与沉积作用[J].海洋与湖沼,2001,32(2):177-184.
[48]蔡爱智,蔡月娥,朱孝宁,等.福建九龙江口入海泥沙的扩散和河口湾的现代沉积[J].海洋地质与第四纪地质,1991,11(1):57-67.
[49]蔡锋,黄敏芬,苏贤泽,等.九龙江河口湾泥沙运移特点与沉积动力机制[J].台湾海峡,1999,18(4):418-424.
[50]葛全胜,王芳,陈泮勤,等.全球变化研究进展和趋势[J].地球科学进展,2007,22(4):417-427.
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