地理学报 ›› 2012, Vol. 67 ›› Issue (5): 609-620.doi: 10.11821/xb201205004
程岩1, 刘月1, 高建华2, 张春鹏1, 李富祥1,3, 刘敬伟1, 张亮1
收稿日期:
2011-07-30
修回日期:
2012-02-03
出版日期:
2012-05-20
发布日期:
2012-05-20
通讯作者:
刘月(1972-), 女, 辽宁锦州人, 副教授, 研究方向为河口生态与环境。E-mail: moonliudd@126.com
基金资助:
CHENG Yan1, LIU Yue1, GAO Jianhua2, ZHANG Chunpeng1, LI Fuxiang1,3, LIU Jingwei1, ZHANG Liang1
Received:
2011-07-30
Revised:
2012-02-03
Online:
2012-05-20
Published:
2012-05-20
Supported by:
摘要: 本文以鸭绿江口西汊道连续性较好、时间分辨率较高、以海湾性质为主的2 处现代沉积物为样本,对其沉积速率、粒度特征、碎屑矿物、重金属进行了测定和分析。柱状样记录了1920 年以来西汊道上游的沉积过程,平均沉积速率约为0.98 cm/a,粒度参数、指示性碎屑矿物、重金属的垂向分布显示出这里的沉积是以海相河口湾沉积为主,但交替存在河流沉积。通过与前期研究成果的比较,揭示了近百年来人类活动对鸭绿江口河床演变的影响。其中,兴修水利对河床演变的影响集中在早期,并带来了河床地貌的重大改变,西汊道失去了河流主汊道的地位;围垦带来的河床演变出现在中期,对河床地貌的影响也很深刻,表现为陆域面积不断扩大,水域面积不断缩小;航道治理等人类活动对河床演变的影响出现在中后期,河床地貌没有明显的改变;最近的人类活动影响有待观察。
程岩, 刘月, 高建华, 张春鹏, 李富祥, 刘敬伟, 张亮. 近百年来人类活动对鸭绿江口河床演变的影响[J]. 地理学报, 2012, 67(5): 609-620.
CHENG Yan, LIU Yue, GAO Jianhua, ZHANG Chunpeng, LI Fuxiang, LIU Jingwei, ZHANG Liang. Influence of Human Activities on the Riverbed Evolution in Yalu River Estuary during Recent One Century[J]. Acta Geographica Sinica, 2012, 67(5): 609-620.
[1] Mikhailova M V. Transformation of the Ebro River Delta under the impact of intense human-induced reduction ofsediment runoff. Water Resources, 2003, 30(4): 370-378. [2] Syvitski J P M, Vorosmarty C J, Kettner A J et al. Impact of human on the flux of terrestrial sediment to the globalocean. Science, 2005, 308: 376-380. [3] Vorosmarty C J, Meybeckc M, Feketea B et al. Anthropogenic sediment retention: Major global impact from registeredriver impoundments. Global and Planetary Change, 2003, 39: 169-190. [4] Zhao Huayun, Dai Shibao, Yang Shilun et al. Progress in studying on the delta evolution influenced by the humanactivity. Marine Sciences, 2007, 31(12): 83-87. [赵华云, 戴仕宝, 杨世伦等. 流域人类活动对三角洲演变影响研究进展. 海洋科学, 2007, 31(12): 83-87.] [5] Cheng Yan. Formation and evolution on geomorphology of Yalu River mouth and harbor construction. CoastalEngineering, 1988, 7(1): 28-36. [程岩. 鸭绿江河口地貌的形成、演变与港口建设. 海岸工程, 1988, 7(1): 28-36.] [6] Gao Mingxin, Cheng Yan, Li Xueming. Evolution of estuary geomorphology and problem of resources and environmentduring the development of Yalu River Delta. Ocean Development and Management, 1994, (3): 26-33. [高明辛, 程岩, 李雪铭. 鸭绿江三角洲开发中的河口地貌演变与资源环境问题. 海洋开发与管理, 1994, (3): 26-33.] [7] Cheng Yan, Zhang Yi. River channel evolution of lower Yalu River and its influence on harbor. Journal of SedimentResearch, 1990, (2): 77-84. [程岩, 张毅. 鸭绿江下游河道演变及其对港口的影响. 泥沙研究, 1990, (2): 77-84.] [8] Cheng Yan. Liu Yue, Li Fuxiang et al. Detrital Mineral characteristics and material source identification in surfacesediments of Yalu River estuary and adjacent waters. Geographical Research, 2010, 29(11): 1950-1960. [程岩, 刘月, 李富祥等. 鸭绿江口及邻近浅海碎屑矿物特征与物源辨识. 地理研究, 2010, 29(11): 1950-1960.] [9] Cheng Yan, Bi Lianxin. Primary character and motive change of shallow beach in Yalu River mouth. Journal ofSediment Research, 2002, (3): 59-63. [程岩, 毕连信. 鸭绿江河口浅滩的基本特征和动态变化. 泥沙研究, 2002, (3):59-63.] [10] Liu Yue, Cheng Yan, Zhang Chunpeng et al. Sedimentary records of light mineral representing the influence of humanactivities on riverbed evolution during recent 100 years. Journal of Eastern Liaoning University: Natural Science,2011, 18(2): 140-144. [刘月, 程岩, 张春鹏等. 近百年来人类活动对鸭绿江口河床演变影响的轻矿物沉积记录. 辽东学院学报, 2011, 18(2): 140-144.] [11] Gao Jianhua, Gao Shu, Dong Lixian et al. Sediment distribution and suspended sediment transport in Yalu RiverEstuary. Marine Science Bulletin, 2003, 22(5): 26-33. [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. 海洋通报, 2003, 22(5): 26-33.] [12] Bai Fenglong, Gao Jianhua, Wang Yaping et al. Tidal characteristics at Yalu River estuary. Marine Science Bulletin,2008, 27(3): 7-13. [白凤龙, 高建华, 汪亚平等. 鸭绿江口的潮汐特征. 海洋通报, 2008, 27(3): 7-13.] [13] Yang Haili, Zheng Yulong. The sediment records of environmental changes under interactions of nature with mankindduring last hundred years in the Yangpu Bay of Hainan, China. Acta Oceanologica Sinica, 2008, 30(4): 95-103. [杨海丽, 郑玉龙. 海南洋浦湾近百年来人与自然相互作用下的环境沉积记录. 海洋学报, 2008, 30(4): 95-103.] [14] Yang Zuosheng, Chen Xiaohui. Centural high resolution records of sediment grain-size variation in the MUD area offthe Changjiang (Yangtze River) Estuary and its influential factors. Quaternary Sciences, 2007, 27(5): 690-699. [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. 第四纪研究, 2007, 27(5): 690-699.] [15] Zhang Zhenke, Li Yanming, Meng Hongming et al. Grain size and its environmental significance of the core from thetidal flat Yuantuojiao Point, Jiangsu Province. Quaternary Sciences, 2008, 28(4): 690-694. [张振克, 李彦明, 孟红明等. 江苏圆陀角附近潮滩沉积岩芯粒度变化及其环境意义. 第四纪研究, 2008, 28(4): 690-694.] [16] Liu Xuying, Gao Jianhua, Bai Fenglong et al. Grain size information in different evolution periods of Xinyanggangtidal flat in Jiangsu Province. Marine Geology & Quaternary Geology, 2008, 28(4): 27-35. [刘旭英, 高建华, 白凤龙等. 苏北新洋港潮滩柱状沉积物粒度分布特征. 海洋地质与第四纪地质, 2008, 28(4): 27-35.] [17] Appleby P G, Nolan P J, Gifford D W et al. 210Pb dating by low background gamma counting. Hydrobiologia, 1986,143: 21-27 [18] McManus J. Grain size determination and interpretation//Tucker M//Techniques in Sedimentology. Oxford: Blackwell,1988: 63-85. [19] State Bureau of Technical Supervision. Marine Investigation Specifications: Geological-geophysical Survey. Beijing:Standards Press of China, 1993: 13-15. [国家技术监督局. 海洋调查规范: 海洋地质地球物理调查. 北京: 中国标准出版社, 1993: 13-15.] [20] State Oceanic Administration. GB/T 17378-5-98 Marine Monitoring Standard. Beijing: China Ocean Press, 1998. [国家海洋局. GB/T 17378-5-98 海洋监测规范. 北京: 海洋出版社, 1998.] [21] Gao Jianhua, Li Jun, Wang Zhenyan et al. Heavy metal distribution and their influence factors in sediments of YaluRiver estuary and its adjacent sea area. Geochimica, 2008, 37(5): 430-438. [高建华, 李军, 王珍岩等. 鸭绿江河口及近岸地区沉积物中重金属分布的影响因素分析. 地球化学, 2008, 37(5): 430-438.] [22] Wang Zhongbo, Yang Shouye, Li Ping et al. Detrital mineral compositions of the Changjiang River sediments andtheir tracing implications. Acta Sedimentologica Sinica, 2006, 24(4): 570-578. [王中波, 杨守业, 李萍等. 长江水系沉积物碎屑矿物组成及其示踪意义. 沉积学报, 2006, 24(4): 570-578] [23] Gao Jianhua, Li Jun, Wang Yaping et al. Heavy mineral distributions and their implications for sediment dynamics inthe Yalu Estuary and its adjacent sea area. Acta Oceanologica Sinica, 2009, 31(3): 84-94. [高建华, 李军, 汪亚平等.鸭绿江河口及近岸海域沉积物中重矿物组成分布及其沉积动力学意义. 海洋学报, 2009, 31(3): 84-94.] [24] Guan Jian, Sun Wei. The space-time distribution regulations of the precious metal and nonferrous metal deposits in theeastern part of Jilin Province. Jilin Geology, 2003, 22(2): 27-33. [关键, 孙炜. 吉林省东部贵金属、有色金属矿床的时空分布规律. 吉林地质, 2003, 22(2): 27-33.] [25] Huo Youguang. The general picture of extracting copper ore in China during modern time. Journal of Xi'an College ofGeology, 1994, 16(3): 85-91. [霍有光. 中国近代铜矿开发概貌. 西安地质学院学报, 1994, 16(3): 85-91.] |
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