台湾河海输运系统宿命整合研究综述

doi:10.11867/j.issn.1001-8166.2013.01.0031

地球科学进展 ›› 2013, Vol. 28 ›› Issue (1): 31 -38. doi: 10.11867/j.issn.1001-8166.2013.01.0031

台湾河海输运系统宿命整合研究综述

赵强，修宗祥

1. 国家海洋局第一海洋研究所，山东青岛266061；
2. 海洋沉积与环境地质国家海洋局重点实验室，山东青岛266061

收稿日期:2012-08-20 修回日期:2012-12-02 出版日期:2013-01-10
通讯作者: 赵强(1981-)，男，山东泰安人，博士后，主要从事海洋地质研究. E-mail:zq-hys@163.com
基金资助:
国家自然科学基金青年基金项目“西沙石岛风成碳酸盐形成演化及其古气候意义”（编号：41106064）和“深水陆坡区碎屑流对海底管道潜在冲击影响的定量研究——以荔湾3-1田为例”（编号：41206058）；国家科技重大专项子课题“南海北部陆坡区地质灾害风险评价预测研究”（编号：211ZX05-001-02）资助.

Overview of the Fate of the Substance in River-Sea -Transport System around Taiwan

Zhao Qiang， Xiu Zongxiang

1. First Institute of Oceanography, State Oceanic Administration, Qingdao266061, China;2. Key Laboratory of Marine Sedimentology and Environmental Geology, Qingdao266061, China

Received:2012-08-20 Revised:2012-12-02 Online:2013-01-10 Published:2013-01-10

下载PDF ( 1425 )

台湾河海输运系统宿命研究是一个“从源到汇”的整合性研究计划，包括FATESKP，FATESCOMMARC和FATESHYPER 3个独立计划，自2003年启动至今已历时9年，分阶段滚动发展，取得了众多研究成果。该研究计划试图查清在构造活跃的热带季风气候区，并常有台风侵袭的浪控弱潮海岸环境下，沉积物在山区小径流、窄陆架、陆坡及海底峡谷之间的物质分散机制，且随着研究的深入，研究区逐步向南海北部、台湾海峡以及冲绳海槽扩展，在南海“从源到汇”的研究中一枝独秀。通过综述台湾河海输运系统宿命整合研究计划，对其研究方法、内容、取得的成果及遇到的问题进行了简要分析，以期为大陆南海北部“从源到汇”的研究提供借鉴。

关键词: 台湾, 河海输运系统, 整合研究, 从源到汇

The research of the fate of river-sea transport system of Taiwan, consisting of three independent projects, FATES-KP, FATES-COMMARC and FATES-HYPER, is an integrated scientific project from a source-to-sink perspective. The three projects have been implemented one after another from 2003. Up to now, it has undergone nine years and a lot of important results have been obtained. The research intended to investigate the working of a material dispersal system consisting of a small mountainous river, a narrow shelf, and a nearby submarine canyon in a tectonically active setting that is also influenced by the monsoon climate. Along with the advance of the project, the research area gradually expanded to the north of South China Sea, Taiwan Strait and Okinawa trough. The project takes the lead of source-to-sink research of the South China Sea. This paper reviews the research methods, contents, main achievements and problems during the project in order to provide some helpful suggestions to the source-to-sink research of South China Sea of Mainland.

Key words: Taiwan, River-sea transport system, Integrated research, Source-to-sink

中图分类号:

P736

[1]NSF. Margins Program Science Plans 2004[R]. New York,2003:131-157.

[2]Wang Pinxian. Deep sea sediments and Earth system[J]. Marine Geology & Quaternary Geology, 2009, 29(4): 1-11.[汪品先. 深海沉积与地球系统[J]. 海洋地质与第四纪地质, 2009, 29(4): 1-11.]

[3]Li Tiegang, Cao Qiyuan, Li Anchun, et al. Source to sink: Sedimentation in the continental margins[J]. Advances in Earth science, 2003, 18(5): 713-721.[李铁刚, 曹奇原, 李安春, 等. 从源到汇: 大陆边缘的沉积作用[J]. 地球科学进展, 2003, 18(5): 713-721.]

[4]Yu Hoshing, Chiang Chengshing, Shen Sumin. Tectonically active sediment dispersal system in SW Taiwan margin with emphasis on the Gaoping (Kaoping) submarine canyon[J]. Journal of Marine Systems, 2009, (76): 369-382.

[5]Liu J T, Lin H L. Sediment dynamics in a submarine canyon: A case of river-sea interaction[J]. Marine Geology, 2004, 207(1/4): 55-81.

[6]Mullenbach B L, Nittrouer C A. Rapid deposition of fluvial sediment in the Eel Canyon, northern California[J]. Continental Shelf Research, 2000, 20: 2 191-2 212.

[7]Palanques A, Khatab M E, Puig P, et al. Downward particle fluxes in the Guadiaro submarine canyon depositional system (north-western Alboran Sea), a river flood dominated system[J]. Marine Geology, 2005, 220: 23-40.

[8]Liu J T, Lin H L, Hung J J. A submarine canyon conduit under typhoon conditions off Southern Taiwan[J].Deep-Sea Research I, 2006, 53: 223-240.

[9]Kudrass H R, Michels K H, Wiedicke M, et al. Cyclones and tides as feeders of a submarine canyon off Bangladesh[J]. Geology, 1998, 26(8): 715-718.

[10]National Sun Yat-sen University Institute of Marine Geology and Chemistry. The fate of terrestrial substances in the Kao-ping submarine Canyon[EB/OL].[2012-08-20] www.mgac. nsysu.edu.tw/liu/FATES.[台湾中山大学海洋地质与化学研究所. 高屏河—海输运系统中陆源物质之宿命整合研究[EB/OL]. [2012-08-20] www.mgac.nsysu.edu.tw/liu/FATES.]

[11]Liu Zuqian. Fate and transport of terrestrial/non-terrestrial substances in a collision margin of arc and continent-general plan[EB/OL].(2008-11-12)[2012-08-20] http:∥140.117.120.62:8080/ir/handle/987654321/13536.[刘祖乾. 陆源和非陆源物质在弧陆碰撞板块边缘中之宿命的整合研究—总计划[EB/OL].(2008-11-12)[2012-08-20] http:∥140.117.120.62:8080/ir/handle/987654321 /13536.]

[12]Liu Zuqian, Du Xiaoqin. Source-to-sink’ research for the Taiwan Strait: A conceptual framework[EB/OL].(2011-03-30)[2012-08-20]http:∥ocean2012.oc.ntu.edu.tw/main/wp-content/uploads/2011/10/abstract.pdf.[刘祖乾, 杜晓琴. 台湾海峡“从源到汇”研究的初步构想[EB/OL].(2011-03-30)[2012-08-20]http:∥ocean2012.oc.ntu.edu.tw/main/wp-content/uploads/2011/10/abstract.pdf.]

[13]Liu Zuqian, Xiao Shijun. Fate of terrestrial/nonterrestrial sediments in high yield particle-export river-sea systems-general plan[EB/OL]. (2011-07-01)[2012-08-20] http:∥ir.lis.nsysu.edu.tw:8080/handle/987654321/44675.[刘祖乾, 萧士俊. 陆源/非陆源物质在高输砂量之河—海输运系统中的宿命整合研究—总计划及子计划——高输砂量之河—海输运系统中颗粒动力作用及沈积的综合研究[EB/OL].(2011-07-01)[2012-08-20]http:∥ir.lis.nsysu.edu.tw:8080/handle/987654321/44675.]

[14]Liu Zuqian. The fate of terrestrial substances in Kao-ping submarine canyon-general plan.[EB/OL].(2009-04-21)[2012-08-20]http:∥ir.lis.sysu.edu.tw:8080/handle/987654321/33239.[刘祖乾.高屏河—海输运系统中陆源物质之宿命的整合研究—总计划[EB/OL].(2009-04-21)[2012-08-20]http:∥ir.lis.nsysu.edu.tw:8080/handle/987654321/33239.]

[15]Liu J T, Liu K j, Huang J C. The influence of a submarine canyon on river sediment dispersal and inner shelf sediment movements: A perspective from grain-size distributions[J]. Marine Geology,2002, 181(4): 357-386.

[16]Feng Shidun. The Change of Bottom Flow of Kaoping Submarine Canyon [D]. Taibei: Institute of Oceanography National Taiwan University, 1988.[冯世墩. 高屏峡谷底层流之变化[D]. 台北: 台湾大学海洋研究所,1988.]

[17]Lin Yuru. The Influence of Topography to the Movement of Water Mass in Kaoping Submarine Canyon[D]. Taibei: Institute of Marine Physics, National Sun-Yat-sen University,2006.[林育如. 高屏峡谷水团运动受地形水深影响[D]. 台北: 台湾中山大学海洋物理研究所, 2006.]

[18]Zhang Yujia. Flow Observation of Kaoping Submarine Canyon and Nearby Sea[D]. Taibei: Institute of Marine Resources, National Sun Yat-sen University, 2001.[张育嘉. 高屏峡谷及附近海域之流场观测[D]. 台北: 台湾中山大学海洋资源研究所,2001.]

[19]Wang Junhao. Observation and Analysis of Flow Variations in the Mouth of Kao-Ping River[D]. Taibei: Institute of Marine Physics, National Sun-Yat-sen University,2007.[王君豪. 高屏溪口流场三维结构的观测分析[D]. 台北: 台湾中山大学海洋物理研究所，2007.]

[20]Wu Menglin. The Study of Flow Dynamics in Kao-ping Submarine Canyon and Near Kao-ping Shelf[D]. Taibei: Institute of Marine Geology and Chemistry, National Sun Yat-sen University,2004.[吴孟麟. 高屏海底峡谷与陆棚流场之研究[D]. 台北: 台湾中山大学海洋地质及化学研究所, 2004.]

[21]Wang Y H, Lee I H, Liu J T. Observation of internal tidal currents in the Kaoping canyon off southwestern Taiwan[J]. Estuarine,Coastal and Shelf Science, 2008, 80: 153-160.

[22]Lee I H, Lien R C, Liu J T, et al. Turbulent mixing and internal tides in Gaoping (Kaoping) submarine canyon, Taiwan[J]. Journal of Marine Systems, 2009, 76(4): 383-396.

[23]Lee I H, Wang Y H, Liu J T, et al. Internal tidal currents in the Gaoping (Kaoping) submarine canyon[J].Journal of Marine Systems,2009,76:397-404.

[24]Liu J T, Wang Y H, Lee I H, et al. Quantifying tidal signatures of the benthic nepheloid layer in Gaoping submarine canyon in southern Taiwan[J]. Marine Geology, 2010, 271(1/2): 119-130.

[25]Guo Jiada. Sinking Partical Dynamicals in the Gaoping Submarine Canyon[D]. Taibei: Institute of Marine Geology and Chemistry, National Sun Yat-sen University, 2011.[郭嘉达. 高屏海底峡谷沉降颗粒动力之研究[D]. 台北: 台湾中山大学海洋地质及化学研究, 2011.]

[26]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 System, 2009, 76 (4): 417-432.

[27]Liu J T, Chao S Y, Hsu R T. The influence of suspended sediments on the plume of a small mountainous river[J]. Journal of Coastal Research, 1999,15: 1 002-1 010.

[28]Xu Fengxin. Deposition of Terrestrial Organic Materials from Small Mountainous Rivers on the Narrow Continental Shelf, Southwest of Taiwan[D]. Taibei: Institute of Oceanography National Taiwan University,2008.[许凤心. 台湾西南海域陆源有机碳沉降受邻近岛屿型河川颗粒传输影响之研究[D]. 台北: 台湾大学海洋研究所, 2008.]

[29]Huh C A, Lin H L, Lin S, et al. Modern accumulation rates and a budget of sediment off the Gaoping (Kaoping) river, SW Taiwan: A tidal and flood dominated depositional environment around a submarine canyon[J]. Journal of Marine Systems, 2009: 76(4): 405-416.

[30]Lee I H, Liu J T. Rectification of the heading and tilting of sediment trap arrays due to strong tidal currents in a submarine canyon[J].Geophysical Research Letters, 2006, 33, L08609. doi: 10.1029/2005GL025183

[31]Hus R T, Liu J T. Capturing a hyperpycnal event by mooring observations in the head of Gaoping submarine canyon after typhoon Fanapi[EB/OL]. (2011-04-01)[2012-08-20]http:∥www. mgac.n sysu. edu. tw /liu/student_poster/2011NSC-Ray.pdf.

[1]	张晓栋,刘志飞,张艳伟,赵玉龙. 海洋微塑料源汇搬运过程的研究进展[J]. 地球科学进展, 2019, 34(9): 936-949.
[2]	林冠慧,张长义. 巨大灾害后的脆弱性：台湾集集地震后中部地区土地利用与覆盖变迁[J]. 地球科学进展, 2006, 21(2): 201-210.
[3]	张小飞;王仰麟;李正国. 台湾地区景观研究领域及其发展方向[J]. 地球科学进展, 2004, 19(5): 845-851.
[4]	林海. 台湾全球变化研究现状[J]. 地球科学进展, 2001, 16(4): 580-583.
[5]	汤懋苍. 台湾地震与大陆旱涝[J]. 地球科学进展, 1994, 9(1): 38-41.

阅读次数

全文

摘要