Tracing Flood Water Level along Nanjing Cliff Bank of the Yangtze River

  • The Key Laboratory of Coast & Island Development of Ministry of Education, Nanjing University, Nanjing 210093, China

Received date: 2004-06-08

  Revised date: 2004-10-09

  Online published: 2004-11-25

Supported by

National Natural Science Foundation of China, No. 40271004


Some remnant marks of flood water level, characterized by dark color and with small eroded holes distributed on the horizontal level marks, are found along the hillside of Nanjing. The same features of the remnant marks of flood water level are also found on the cape of Caishiji cliff of Cuiluo Mountain. Detailed analyses on the altitude of the remnant water level marks and sediment grain-size collected inside the eroded holes and on the Yangtze River floodplain are carried out and comparisons with flood historical literature and modern flood water level records are made. Based upon which the following conclusions are drawn: (1) The altitude of the first and second ancient water level marks at 8.5 m and 9.5 m which exceed the modern Yangtze River water surface by 5-6 m are considered as paleoflood remnant because they have been disengaged from present Yangtze River water surface for a long time. (2) The altitude of the third ancient water level mark is 10.5 m, which is 0.3 m higher than the catastrophic flood in 100 years recorded in history. According to historical records of the Yangtze River flood, the level this paleoflood event may be equivalent to the level of a catastrophic flood in 100-200 years. (3) The altitude of the highest ancient water level mark is 12.8 m which is probably equal to the height of the paleoflood taking place in high sea level time of the Holocene.

Cite this article

HE Huachun, WANG Ying, LI Shuheng . Tracing Flood Water Level along Nanjing Cliff Bank of the Yangtze River[J]. Acta Geographica Sinica, 2004 , 59(6) : 938 -947 . DOI: 10.11821/xb200406017


[1] Pan Fengying. On the channel change taking place at Changjiang River Nanjing reach since mid-Holocene. Journal of Nanjing Normal University (Natural Science), 1990, 13(4): 81-88.
[潘凤英. 中全新世以来长江南京河段的河床变迁. 南京师范大学学报 (自然科学版), 1990, 13(4): 81-88.]

[2] Xia Bangdong. Pre-Mesozoic tectonic evolution of the lower Yangtze region. Journal of Chengdu Institute of Technology, 1998, 25(2): 145-152.
[夏邦栋. 下扬子前中生代构造演化. 成都理工学院学报, 1998, 25(2): 145-152.]

[3] Committee of Yangtze River Water Resources of the Ministry of Water Resources (ed.). Atlas of Flood Control of Yangtze River. Beijing: Science Press, 2001. 130-131.

[4] Rui Xiaofang. Hydrologic analysis of formation and changing trend of flood on Nanjing reach of Yangtze River. Technology of Water Resources & Hydroelectricity, 1994, (10): 2-7.
[芮孝芳. 长江南京段洪水成因及趋势的水文学分析. 水利水电技术, 1994, (10): 2-7.]

[5] Institute of Geography, Chinese Academy of Sciences. Formation and characters of river channel along middle-lower reaches of the Yangtze River. Beijing: Science Press, 1985. 6-46.

[6] Yang Huairen. Research on Environment Changes. Nanjing: Hohai University Press, 1996. 366-373.

[7] Zhu Cheng. Holocene deposits and paleo-floods on the north bank of the Yangtze River, Nanjing Area. Geographical Research, 1997, 16(4): 23-30.
[朱诚. 南京江北地区全新世沉积与古洪水研究. 地理研究, 1997, 16(4): 23-30.]

[8] Water Resources Bureau, Jiangsu Province. Disaster Tables of Flood & Drought in the Jiangsu Province over the Last 2000 Years. Nanjing: Water Resources Bureau of Revolutionary Committee, Jinagsu Province, 1976. 26-47.

[9] Hydrological Department of the Ministry of Water Resources. Annals of Chinese Water Resources. Beijing: China Water Resources & Hydroelectricity Press, 1997. 463-489.

[10] Song Zhenghai (ed.). Atlas of Anomaly Chronology & Heavy Natural Disaster in Ancient China. Guangzhou: Guangdong Education Press, 1992. 305-317.

[11] Committee of Yangtze River Water Resources of the Ministry of Water Resources (ed.). Flood & Drought in the Yangtze River Basin. Beijing: China Water Resources & Hydroelectricity Press, 2002. 50-58.

[12] Xu Houze. Flood and Scientific & Technological Strategies in Yangtze River Basin. Beijing: Science Press, 1999. 270-274.
[许厚泽. 长江流域洪涝灾害与科技对策. 北京: 科学出版社, 1999. 270-274.]

[13] Rui Xiaofang. Formation and change trend of large flood in the lower tidal reach of the Yangtze River. Advances in Water Science, 1996, 7(3): 221-225.
[芮孝芳. 长江下游感潮河段大洪水和特大洪水的形成及趋势. 水科学进展, 1996, 7(3): 221-225.]

[14] Zhu Honggeng, Huang Honghu. Tendency analyses of water regime change in the lower reaches of Changjiang River. Journal of Heilongjiang Hydraulic Engineering College, 2002, 29(4): 18-20.
[朱红耕, 黄红虎. 长江下游水情变化趋势分析. 黑龙江水专学报, 2002, 29(4): 18-20.]

[15] Li Guofang, Huang Zheping et al. Risk analysis of design flood stage of Nanjing section of Yangtze River flood-protecting embankment. Journal of Hohai University, 1999, 27(2): 22-27.
[李国芳, 黄振平 等. 长江防洪堤南京段设计洪水位风险分析. 河海大学学报, 1999, 27(2): 22-27.]

[16] Zhang Qiang. Environmental changes since late-Pleistocene in northbank of Yangtze River, Nanjing. Scientia Geog. Sinica, 2001, 21(6): 498-504.
[张强. 南京江北地区晚更新世以来环境演变研究. 地理科学, 2001, 21(6): 498-504.]

[17] Li Congxian, Min Qiubao. Transgressive coast time and sea surface position of Yangtze River Delta in Holocene. Journal of Tongji University, 1981, (3): 104-108.
[李从先, 闵秋宝. 全新世长江三角洲顶部的海进时间和海面位置. 同济大学学报, 1981, (3): 104-108.]

[18] Zhongyuan Chen, Jiufa Li, Huanting Shen et al. Yangtze River of China: historical analysis of discharge variability and sediment flux. Geomorphology, 2001, 41: 77-91.

[19] Chen Xueying. Natural Disaster and Control Strategies in Yangtze River Basin. Wuhan: Hubei People's Press, 1999. 30-57.
[陈雪英. 长江流域重大自然灾害及防治对策. 武汉: 湖北人民出版社, 1999. 30-57.]

[20] Hu Mingsi, Luo Chengzheng (eds.). Chinese Historical Large Floods (V.II). Beijing: China Book Store, 1992. 275-362.

[21] Huang Lanxin. Flood water level along the main channel of the lower reaches of the Yangtze River in the past 40 years: variations and causes. Journal of Lake Sciences, 1999, 11(4): 99-104.
[黄兰心. 近40年来长江下游干流洪水位变化及原因初探. 湖泊科学, 1999, 11(4): 99-104.]

[22] Master Station of Hydrology in Jiangsu. Hydrology Statistics of Jiangsu Province. Nanjing: Master Station of Hydrology in Jiangsu Province, 1984. 746-770.
[江苏省水文总站. 江苏省水文统计. 南京: 江苏省水文总站, 1984. 746-770.]

[23] Hydrology Department of Yangtze River Planning Office. Characteristic Handbooks of Hydrological Information in Yangtze River Basin. Shanghai: Hydrology Department of Yangtze River Planning Office, 1958. 26-27.

[24] Hydrology Station of Water Resources Bureau of Revolutionary Committee, Jiangsu Province. Hydrological Handbooks of Jiangsu Province. Nanjing: Hydrology Station of Water Resources Bureau, Jiangsu Province, 1976. 166-167.

[25] Mei Jinhuan. Flood level analysis of dykes design in middle-lower mainstream of Yangtze River. Yangtze River, 2001, 32(12): 12-14.
[梅金焕. 长江中下游干流堤防设计洪水位分析. 人民长江, 2001, 32(12): 12-14.]

[26] Li Ming, Wang Li. Analysis of flood variation of Yangtze River region over the last 100 years. Journal of Southwest China Normal University (Natural Science), 1999, 24(1): 97-102.
[黎明. 近百年来长江洪水变化的初步分析. 西南师范大学学报 (自然科学版), 1999, 24(1): 97-102.]

[27] Zhang Jianxin, Ding Xianrong. Preliminary investigation on paleoflood. Jiangsu Geology, 1995, 19(4): 209-212.
[张建新, 丁贤荣. 古洪水调查初探. 江苏地质, 1995, 19(4): 209-212.]

[28] Yang Dayuan, Xie Yuebo. Paleoflood slack-water deposits. Acta Sedimentologica Sinica, 1997, 15(3): 29-32.
[杨达源, 谢悦波. 古洪水平流沉积. 沉积学报, 1997, 15(3): 29-32.]

[29] Wang Ying, Bhan Deonarine. Model Atlas of Surface Textures of Quartz Sand. Beijing: Science Press, 1985. 6-30.
[王颖, B.迪纳瑞尔. 石英砂表面结构模式图集. 北京: 科学出版社, 1985. 6-30.]

[30] Xie Yuebo, Fei Yuhong. Slack water deposits and flow peak level of a paleoflood. Acta Geoscientia Sinica, 2001, 22(4): 320-323.
[谢悦波, 费宇红. 古洪水平流沉积与水位. 地球学报, 2001, 22(4): 320-323.]

[31] Xie Yuebo, Jiang Hongtao. Paleoflood study. Jouranl of Nanjing Universtiy (Natural Science), 2001, 37(3): 390-394.
[谢悦波, 姜洪涛. 古洪水研究. 南京大学学报(自然科学), 2001, 37(3): 390-394.]

[32] Zhan Daojiang, Xie Yuebo. New advance in flood calculation. Hydrology, 1997, (1): 1-6.
[詹道江, 谢悦波. 洪水计算的新进展. 水文, 1997, (1): 1-6.]

[33] Zhan Daojiang, Qian Tie. Extreme calculation frequency analysis with paleoflood. In: B C Yen, Proceedings of the International Conference on Channel Flow and Catchment Runoff, 1989. 1004-1012.

[34] Zhan Daojiang. Paleoflood study in China. Annual Report of Science and Technology. Journal of Hohai University, 1995, (suppl.): 7-10.

[35] Baker V R, Kochal R C. Flood Geomorphology. The University of Arizona, Tucson, Arisona USA, 1998. 124-129.

[36] Xie Yuebo, Wang Wenhui et al. Characteristics of grain size for palaeoflood slackwater deposits. Hydrology, 2000, 20(4): 18-20.
[谢悦波, 王文辉 等. 古洪水平流沉积粒度特征. 水文, 2000, 20(4): 18-20.]