THE CHANNEL DYNAMIC GEOMORPHOLOGY OF MIAODAO STRAIT,SHANDONG,CHINA

WANG Qing; ZHONG Shao-yun; LIU Jian-hua; SONG Chuan-guang

2006 Vol. 26, No. 2

Article Contents

Article navigation > Marine Geology & Quaternary Geology > 2006 > 26(2): 17-24

Next Article Previous Article

WANG Qing, ZHONG Shao-yun, LIU Jian-hua, SONG Chuan-guang. THE CHANNEL DYNAMIC GEOMORPHOLOGY OF MIAODAO STRAIT,SHANDONG,CHINA[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 17-24.

Citation:

WANG Qing, ZHONG Shao-yun, LIU Jian-hua, SONG Chuan-guang. THE CHANNEL DYNAMIC GEOMORPHOLOGY OF MIAODAO STRAIT,SHANDONG,CHINA[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 17-24.

THE CHANNEL DYNAMIC GEOMORPHOLOGY OF MIAODAO STRAIT,SHANDONG,CHINA

Coast Institute of Ludong University, Yantai 264025, China

Received Date: 04 September 2005

Revised Date: 20 October 2005

Abstract

Abstract

The authors have systematically analyzed the dynamic, sediment and topographic features of the Miaodao Strait,and then studied the channel effect and its dynamic topographical expressions including strait formation and evolution, tidal current convergence and divergence, erosion and deposition, difference of the flood and ebb tidal currents and the formation of the Dengzhou shoal, the channel sand transport and its sediment effects. According to the study results we know that the strait channel was formed with the gradual rise of then relative sea level since late Pleistocene.The modern Miaodao Strait and its dynamic system came into being during 5 000~6 000 aBP and then entered the modern development stage of the strait geomorphology.The Miaodao Strait has obvious strait effect.When flood current from west and ebb current from east flow through the E-W strait that opens westwards,the current speed changes with the area of the strait section.The central part of the strait experiences the largest erosion,and the erosion decreases with the increase of width of the strait and turns into accumulation.Silt from seabed of the strait and the nearby coast becomes the direct source of muddy area along the coast of the Yellow Sea in the north of the Shandony Peninsula.
- channel effects /
- dynamic geomorphology /
- Miaodao Strait

FullText(HTML)

References

[1]	Gregory J W.The relations of Thames and Rhine and age of the strait of Dover[J]. Geogr.J., 1927,50:52-59. Google Scholar
[2]	Keller G H, Richards A F. Sediments of the Malacca Strait[J]. Southeast Asia.J.Sediment.Petrol., 1967,37(1):102-127. Google Scholar
[3]	Hesse R,Von Rad U,Fabricius F H. Holocene sedimentation in the Strait of Otranto between the Adriaticand Ionian Seas(Mediterranean)[J].Marine Geology,1971,10:293-355. Google Scholar
[4]	Johnson D A. Phyiography,structure,and sediment-current interactions[J]. Marine Geology. 1984,58:1-34. Google Scholar
[5]	Ledbetter M T. Bottom-current speed in the Vema Channel recorded by particle size of sediment fine-fraction[J]. Marine Geology, 1984,58:137-150. Google Scholar
[6]	Stanley D J, Freeland G L,Sheng H. Dispersal of Mediterranean and Suez Bay sediments in the Suez Cannal[J]. Marine Geology,1982,49:61-79. Google Scholar
[7]	Cannon G A. Transport Variability in a Fjord[M]//The Estuary as a Filter.1984:67-78. Google Scholar
[8]	Pattiaratchi C B,Collins M B. Sediment transport under waves and tidal currents:a case study from the northern Bristol Channel, UK[J]. Marine Geology, 1984,56:27-40. Google Scholar
[9]	吉冈洋.冬季纪伊水道中的海洋锋[C]//华东师范大学《河口锋》课题组译.河口锋研究译文集.1971:40-54.[Marine fronts in Jiyi channel in winter[C]//Translated text collection of estuary front research.translated by the research group of estuary fronts, East China Normal University,1971:40 Google Scholar -54.] Google Scholar
[10]	金波,鲍才胜,林吉胜.琼州海峡东、西口地貌特征及其成因初探[J].海洋地质研究,1982,2(4):94-101. Google Scholar [JIN Bo,BAO Cai-sheng,LIN Ji-sheng. The landform characters and causes of formation in the east and west mouth of Qiongzhou Strait channel[J]. The Research of Marine Geology,1982,2(4):94-101.] Google Scholar
[11]	周起舞.淤泥质峡道地区深水港的泊稳与淤积[M].杭州:杭州大学出版社,1995:113-117.[ZHOU Qi-wu. The deep berk mooring stable and the deposition in the muddy strait channel area[M].Hangzhou:Publishing house of Hangzhou University,1995:113 Google Scholar -117.] Google Scholar
[12]	邱建立.舟山野鸭山港湾的平衡水下地形分析[J].海洋通报,1995,3:41-50.[QIU Jian-li. Equilibrium analyzing on the submarine topography of the Yeyashan bay, Zhoushan[J]. Marine Science Bulletin, 1995 Google Scholar ,3:41-50.] Google Scholar
[13]	蒋国俊.峡道效应研究——以舟山群岛地区峡道为例[D].华东师范大学,1996.[JIANG Guo-jun.The study of strait channel effects with special reference to Zhoushan islands channels[D]. East China Normal University,1996.] Google Scholar
[14]	陈沈良.崎岖列岛海区的水文泥沙及其峡道效应[J].海洋学报,2000,3:123-131.[CHEN Shen-liang.Hydrodynamics,sediments and strait-chennel effects for the Qiqu Archipelago[J]. Acta Oceanologia Sinica, 2000 Google Scholar ,3:123-131.] Google Scholar
[15]	李玉中,陈沈良.洋山港海域余流分离和会聚现象研究[J].水利学报,2003,5:24-34.[LI Yu-zhong,CHEN Shen-liang.Separation and convergence of residual flows in Yangshan harbor area[J].Hydraulic Sinica, 2003 Google Scholar ,5:24-34.] Google Scholar
[16]	陈雪英,胡泽建.山东蓬莱西庄附近海域波浪与海岸侵蚀[J].黄渤海海洋,1992,10(1):18-26. Google Scholar [CHEN Xue-ying,HU Ze-jian.Ocean waves and coastal erosion near the Xizhuang Village,Penglai City,Shandong Province[J].Journal of Oceanography of Huanghai and Bohai Seas,1992,10(1):18-26.] Google Scholar
[17]	武桂秋,孟祥东,夏东兴,等.关于登州浅滩作用的研究[J].海洋与湖沼,1997,28(4):419-425. Google Scholar [WU Gui-qiu, MENG Xiang-dong, XIA Dong-xing,et al.Research on the effect of Dengzhou shoal[J].Oceanologia et Limnologia Sinica, 1997,28(4):419-425.] Google Scholar
[18]	李福林,夏东兴,王文海,等.登州浅滩的形成、动态演化及可恢复性研究[J].海洋学报,2004,26(6):65-73. Google Scholar [LI Fu-lin,XIA Dong-xing,WANG Wen-hai,et al.Discussion on the evolution cause and its recovery for the Dengzhou shoal,China[J].Acta Oceanologia Sinica, 2004,26(6):65-73.] Google Scholar
[19]	秦蕴珊,赵一阳.渤海地质[M].北京:科学出版社,1985.[QIN Yun-shan, ZHAO Yi-yang. Geology of Bohai Sea[M]. Beijing:Science Press,1985.] Google Scholar
[20]	孟昭翰,张爱芙,王栋成,等.渤海海峡长岛风特性研究[J].太阳能学报,2001,22(1):64-71. Google Scholar [MENG Zhao-han,ZHANG Ai-fu,WANG Dong-cheng,et al.Study on the wind speciality in Bohai sea channel[J].Acta Energiae Solaris Sinica,2001,22(1):64-71.] Google Scholar
[21]	刘敏厚,吴世迎,王永吉.黄海晚第四纪沉积[M].北京:海洋出版社,1987.[LIU Min-hou,WU Shi-ying,WANG Yong-ji.Late Quaternary deposits of the Yellow Sea[M].Beijing:China Ocean Press, 1987.] Google Scholar
[22]	刘敬圃,赵松龄.渤海海底埋藏黄土及沿岸出露黄土的成因[J].海洋与湖沼,1995,26(4):363-368. Google Scholar [LIU Jing-pu,ZHAO Song-ling.Origin of the buried loess in the Bohai Sea bottom and the exposed loess along the coastal zone[J]. Oceanologia et Limnologia Sinica, 1995,26(4):363-368.] Google Scholar
[23]
[24]	郑铁民.黄海晚更新世的黄土沉积[J].海洋与湖沼,1994,25(3):336-344. Google Scholar [ZHENG Tie-min.Loess deposit in Yellow Sea during late Pleistocene[J]. Oceanologia et Limnologia Sinica, 1994,25(3):336-344.] Google Scholar
[25]	赵奎寰.登州浅滩物质来源及运移趋势[J].海岸工程,1992,11(1):32-40. Google Scholar [ZHAO Kui-huan.The sediment source of Dengzhou shallows and its transport tendency[J].Coastal Engineering,1992,11(1):32-40.] Google Scholar
[26]	秦蕴珊,李凡.黄河入海泥沙对渤海和黄海沉积作用的影响[J].海洋科学集刊,1986,27:124-134.[QIN Yun-shan,LI Fan. The effects of the Yellow River sediment on the sedimentation of the Bohai Sea and the Yellow Sea[J].Studia Marina Sinica, 1986 Google Scholar ,27:124-134.] Google Scholar
[27]	Park Y A,Khim B M. Clay minerals of the recent fine-grained sediment on the Korean continental shelves[J].Continental Shelf Research,1990,10:1179-1191. Google Scholar
[28]	董礼先,苏纪兰,王康善.黄渤海潮流场及其与沉积物搬运的关系[J].海洋学报,1989,11(1):102-114. Google Scholar [DONG Li-xian,SU Ji-lan,WANG Kang-shan.Tidal current field and its effect on sediment transport within Yellow Sea and Bohai Sea[J]. Acta Oceanologia Sinica, 1989,11(1):102-114.] Google Scholar
[29]	秦蕴珊,李凡.渤海海水中悬浮体的研究[J].海洋学报,1982,4(2):191-200. Google Scholar [QIN Yun-shan, LI Fan.Study on the suspended matter in seawater in the Bohai Sea[J]. Acta Oceanologia Sinica, 1982,4(2):191-200.] Google Scholar
[30]	Milliman J D,QIN Yun-shan,Park Y A.Sediments and sedimentary processes in the Yellow and East China Seas[M]//Taira A,Masuda F.Sedimentary Facies in the Active Plate Margin.Tokyo:Terra Scientific Publishing Company,1989:233-249. Google Scholar
[31]	王桂芝,高抒,李凤业.北黄海西部的全新世泥质沉积[J].海洋学报,2003,25(4):125-134. Google Scholar [WANG Gui-zhi,GAO Shu,LI Feng-ye.Holocene mud deposits in the west of the north Yellow Sea[J]. Acta Oceanologia Sinica,2003,25(4):125-134.] Google Scholar
[32]	齐君,李凤业,宋金明,等.北黄海沉积速率及其沉积通量[J].海洋地质与第四纪地质,2004,24(2):9-14. Google Scholar [QI Jun,LI Feng-ye,SONG Jin-ming,et al.Sedimentation rate and flux of the north Yellow Sea[J].Marine Geology and Quaternary Geology, 2004,24(2):9-14.] Google Scholar