RAN Longjiang, SHI Yong, GAO Jianhua, LIU Yue, LI Fuxiang, BAI Fenglong, LI Jun. GAIN SIZE VARIATION AND ITS INFLUENCING FACTORS IN THE SEDIMENT CORES OF YALU RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2012, 32(2): 31-42. DOI: 10.3724/SP.J.1140.2012.02031
Citation: RAN Longjiang, SHI Yong, GAO Jianhua, LIU Yue, LI Fuxiang, BAI Fenglong, LI Jun. GAIN SIZE VARIATION AND ITS INFLUENCING FACTORS IN THE SEDIMENT CORES OF YALU RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2012, 32(2): 31-42. DOI: 10.3724/SP.J.1140.2012.02031

GAIN SIZE VARIATION AND ITS INFLUENCING FACTORS IN THE SEDIMENT CORES OF YALU RIVER ESTUARY

More Information
  • Received Date: June 29, 2011
  • Revised Date: September 18, 2011
  • The gain size parameters and sensitive components of the core sediments in the Yalu river estuary were analyzed in order to reveal the depositional characteristics under changing dynamic environment. The depositional characteristics in the estuary areas are influenced by both the nature and human activities. 210Pb was used for dating the cores. The sediments in the west Yalu River channel are dominated by mud and sand under the action of tidal current, and the vertical variation of gain size parameters is small. The cores in western tidal flat of the estuary, controlled by tide and wave, contained shell fragments, and the' gains became coarser from certain depth to the surface. The variation of the sediments characteristics in the Yalu river estuary was mainly affected by the variations of water and sediment discharges induced by human activities in recent decades. The wavy characteristics of the core sediments indicate the unstable feature of the river before 1941. Due to the decrease in both the sediment and water discharges, the sandy sediment had been decreasing and instead silt component increasing during the period from 1941 to 1970(1980). The grain composition and sensitive components remained stable during the period of 1970(1980) and 1990 since the sediment and water flux had little change. However, with the further decreasing of the sediment flux, the trend of sediment coarsening upwards have been recorded near the Yalu River mouth after 1990.
  • [1]
    陈吉余,陈沈良.中国河口研究五十年:回顾与展望[J]. 海洋与湖沼,2007,38(6):481-486.

    [CHEN Jiyu,CHEN Shenliang. China estuarine research for 50 years:retrospect and prospect[J]. Oceanologia et Limnologia Sinica,2007, 8(6):481-486.]
    [2]
    Leithold E L, Perkey D W, Blair N E, et al. Sedimentation and carbon burial on the northern California shelf:the signatures of land-use change[J]. Continental Shelf Research, 2005, 25:349-371.
    [3]
    高抒.浅海细颗粒沉积物通量与循环过程[J].世界科技研究与发展,2000,22(5):73-77.

    [GAO Shu. Fine-grained Sediment Fluxes and Cycling on Continental Shelves[J]. World Sci-tech R&D, 2000,22(5):73-77.]
    [4]
    杨作升,陈晓辉.百年来长江口泥质区高分辨率沉积粒度变化及影响因素探讨[J].第四纪研究,2007,27(5):690-698.

    [YANG Zuosheng,CHEN Xiaohui. Centurial high resolution records of sediment gain-size variation in the mud area off the Changjiang(Yangtze river) estuary and its influencial factors[J]. Quaternary Sciences, 2007,27(5):690-698.]
    [5]
    程岩,毕连信.鸭绿江河口浅滩的基本特征和动态变化[J].泥沙研究,2002,3:59-63.[CHENG Yan, BI Lianxin. Primary character and motive change of shallow beach in Yalujiang river mouth[J]. Journal of Sediment Research, 2002

    ,3:59-63.]
    [6]
    王励.中朝界河鸭绿江河口段(虎山以下)河道演变分析[D]:哈尔滨工业大学硕士学位论文,2006.[WANG Li. Analyze of channel change in Yalu River estuary after Hushan-Boundary River between China and North Korea[D]:Master's degree thesis Of Harbin industrial university,2006.]
    [7]
    高建华,李军,汪亚平,等.鸭绿江河口及近岸海域沉积物中矿物组成、分布及其沉积动力学意义[J].海洋学报,2009,31(3):84-94.

    [GAO Jianhua, LI Jun, WANG Yaping, et al. Heavy mineral distribution and their implications for sediment dynamics in the Yalu Estuary and its adjacent sea area[J]. Actaoceanolo Gicasinica, 2009, 31(2):1-11.]
    [8]
    中国海湾志编纂委员会.中国海湾志:第十四分册(重要河口)[M].北京:海洋出版社,1998:386-432.[State Oceanic Administration. Chinese Harbours and Embayments (Volume 14):Important Estuaries[M]. Beijing:China Ocean Press, 1998

    :386-432.]
    [9]
    金惜三,李炎.鸭绿江洪季的河口最大混浊带[J].东海海洋,2001,19(1):1-9.

    [JIN Xisan, LI Yan. Turbidity maximum belt of Yalujiang River estuary in the wet season[J]. Donghai Marine Science, 2001,19(1):1-9.]
    [10]
    GAO Jianhua, GAO Shu, CHENG Yan, et al. Formation of turbidity maxima in the Yalu River Estuary, China[J].Journal of Coastal Research, 2004,43(SI):134-146.
    [11]
    白凤龙,高建华,汪亚平,等.鸭绿江口的潮汐特征[J].海洋通报,2008,27(3):7-13.

    [BAI Fenglong, GAO Jianhua, WANG Yaping, et al. Tidal characteristics at Yalu River estuary[J]. Marine Science Bulletin, 2008, 27(3):7-13.]
    [12]
    李家胜,高建华,李军,等. 鸭绿江河口元素常量元素地球化学分布特征及其控制因素[J].海洋地质与第四纪地质,2010,30(1):25-32.

    [LI Jiasheng, GAO Jianhua, LI Jun, et al. Distribution and controlling factors of major elements in sediments of the Yalu river estuary[J]. Marine Geology and Quaternary Geology, 2010,30(1):25-32.]
    [13]
    Mcmanus J. Grain size determination and interpretation[C]//Techniques in Sedimentology. Oxford:Black2well,1988:63285.
    [14]
    Flynnw W. The determination of low level of polonium-210 in environmental materials[J]. Analytica Chimica Acta, 1968, 43:221-227.
    [15]
    Goldburg E D,Koide M. Rates of sediment accumulation in the Indian Ocean[C]//In:Geiss J,Goldburg E D (Ed.). Earth Science and Meteoritics, Amsterdam:North-Holland publishing Company,1963:90-102.
    [16]
    程岩.鸭绿江河口地貌的形成与演变[D]:东北师范大学硕士学位论文,2007.[CHENG Yan. Estuary landform's formation and evolution of Yalu River[D]:Master's degree thesis of Northeast normal university,2007.]
    [17]
    高建华,高抒,董礼先,等.鸭绿江河口地区沉积物特征及悬沙输送[J].海洋通报,2003,22(5):26-33.

    [GAO Jianhua, GAO Shu, DONG Lixian, et al. Sediment distribution and suspended sediment transport in Yalu River estuary[J]. Marine Science Bulletin, 2003,22(5):26-33.]
    [18]
    高峰,孙连成,麦苗.鸭绿江河口潮流泥沙数值模拟[J].水道港口,2009,30(2):89-95.

    [GAO Feng, SUN Liancheng, MAI Miao. Numerical simulation of tidal current and sediment in Yalu River estuary[J].Journal of Waterway and Harbor,2009,30(2):89-95.]
    [19]
    范代读,李从先.现代潮汐层偶与古环境解释[J].自然科学进展,2000,10(12):1109-1114.

    [FAN Daidu,LI Congxian. Modern tidal couplets and interpretation on paleo-environment[J]. Progress in Natural Science, 2000,10(12):1109-1114.]
    [20]
    程岩.鸭绿江河口地貌的形成、演变与港口建设[J].海港工程,1988,7(1):28-35.

    [CHENG Yan. Formation and evolution on geomorphology of Yalu River mouth and harbor construction[J]. Coastal Engineering, 1988,7(1),28-35.]
    [21]
    Yang S L, Cao A, Hotz H J, et al. Trends in annual discharge from the Yangtze River to the sea (1865-2004)[J]. Hydrological Sciences-Journal-des Sciences Hydrologiques, 2005,50(5):825-836.
    [22]
    李鸿鹰,程岩.鸭绿江三角洲开发中的资源与环境问题[J].经济地理,1996,16(3):37-42.

    [LI Hongying,CHENG Yan. The resource and environment problems in Yalu River delta development. Economic geography,1996,16(3):37-42.]
    [23]
    Mahmood K. Reservoir sedimentation. Impact, Extent and Mitigation[M]. World Bank technical paper 71, Washington, D C,1987.
    [24]
    程岩,张毅.鸭绿江下游河道演变及其对港口的影响[J].泥沙研究,1990,2:77-84.[CHENG Yan,ZHANG Yi.The formation of Yalu River downstream channel and its influence for ports[J]. Journal of Sediment Research,1990

    ,2:77-84.]
    [25]
    李光天,符文侠,贾锡钧.辽东潮间浅滩的综合特征[J].地理学报,1986,41(3):262-273.

    [LI Guangtian,FU Wenxia,JIA Xijun.The comprehensive characteristic of the Liaodong peninsular tidal flat[J]. Acta Geographica Sinica,1986,41(3):262-273.]
    [26]
    LIU Cheng, SUI Jueyi, WANG Zhaoyin. Sediment load reduction in Chinese Rivers[J]. International Journal of Sediment Research, 2008, 23:44-55.
    [27]
    陈吉余.开发浅海滩涂资源拓展我国的生存空间[J].中国工程科学,2000,2(3):27-31.

    [CHEN Jiyu. To exploiting lower tidal flats for expending living space of China[J]. Engineering Science, 2000,2(3):27-31.]
    [28]
    沈焕庭.黄海沿岸河口过程类比[J].海洋与湖沼,1990,21(5):449-457.

    [SHEN Huanting. Comparative studies of estuaries bordering the Yellow Sea[J]. Oceanologia et Limnologia Sinica, 1990, 21(5):449-457.]
    [29]
    严杰,高建华,李军,等.鸭绿江河口及近岸地区稀土元素的物源指示意义[J].海洋地质与第四纪地质,2010,30(4):95-103.

    [YAN Jie, GAO Jianhua, LI Jun,et al. Implications of REE for provenance in the Yalu estuary and its adjacent sea area[J]. Marine Geology and Quaternary Geology, 2010,30(4):95-103.]

Catalog

    Article views (1877) PDF downloads (12) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return