汉江上游郧县五峰段史前大洪水水文学恢复研究

doi:10.11821/dlxb201311012

地理学报 ›› 2013, Vol. 68 ›› Issue (11): 1568-1577.doi: 10.11821/dlxb201311012

汉江上游郧县五峰段史前大洪水水文学恢复研究

刘涛, 黄春长, 庞奖励, 查小春, 周亚利, 张玉柱, 刘科

陕西师范大学旅游与环境学院, 西安710062

收稿日期:2013-08-17 修回日期:2013-09-09 出版日期:2013-11-20 发布日期:2013-11-20
通讯作者: 黄春长（1953-），男，陕西彬县人，博士，教授，博导，中国地理学会会员（S110000052M），主要从事全新世环境变化与人地关系演变研究。E-mail：cchuang@snnu.edu.cn
作者简介:刘涛（1988-），男，山西吕梁人，硕士研究生，环境变迁专业。E-mail：liu499169@163.com
基金资助:
国家自然科学基金重点项目（41030637；41271108）；教育部博士点基金优先发展领域项目（20110202130002）

Hydrological reconstructions of the pre-historical great floods in the Wufeng Reach of Yunxian County in the upper Hanjiang River

LIU Tao, HUANG Chunchang, PANG Jiangli, ZHA Xiaochun, ZHOU Yali, ZHANG Yuzhu, LIU Ke

College of Tourism and Environmental Sciences, Shaanxi Normal University, Xi'an 710062, China

Received:2013-08-17 Revised:2013-09-09 Online:2013-11-20 Published:2013-11-20
Supported by:
National Natural Science Foundation of China, No.41030637; No.41271108; Ph.D. Programs Foundation from Ministry of Education of China, No.20110202130002

摘要/Abstract

摘要： 通过深入的野外考察，在汉江上游郧县五峰段多个地点发现全新世古洪水事件的沉积学记录，为恢复史前特大洪水事件的洪峰水位和洪峰流量提供了物质基础。在系统获取河道水文参数的基础上，采用ArcGIS 耦合HEC-RAS模型，推算出其洪峰流量介于42 220~63 400m³/s 之间。对于河槽糙率的灵敏度检验表明，给定糙率变化±25%，模型模拟得到的洪峰流量误差在-10.6%~6.3%之间。这个误差范围远小于采用比降—面积法获得的结果。同时，采用该模型和同样的参数，依据该河段现代大洪水洪痕高程，恢复推算其洪峰流量，其结果与实测数据误差在-3.9%~1.0%之间。与其它方法相比较，这种新方法有效地提高了水文参数选取准确性，使得古洪水水文恢复计算结果更为可靠。本研究为超长尺度大洪水水文学恢复提供了新的途径，也获得了汉江上游万年尺度特大洪水的水文学数据资料，对汉江上游水利水电枢纽工程建设、水资源调度和防洪减灾具有重要的现实意义。

关键词: 古洪水水文学, 汉江上游, 全新世, HEC-RAS模型

Abstract: Palaeoflood hydrological studies were carried out in the upper reaches of the Hanjiang River. Typical palaeoflood slackwater deposits of the Holocene period were identified at several sites along the banks of the Wufeng reach in Yunxian County. They have recorded four episodes of extraordinary palaeoflood events (12,600-12,400 a BP, 4200-4000 a BP, 3200-2800 a BP and 1900-1700 a BP). The palaeoflood peak stages were estimated with the elevations and the deposition depths of the SWD. The palaeoflood peak discharges were estimated by using the HEC-RAS one dimensional model running within an ArcGIS environment. The results indicated that these palaeoflood discharges were between 42,220 and 63,400 m³/s. A sensitivity test performed on the model indicated that for a 25% variation in roughness values, an error between -10.6% and 6.3% was introduced into the results of peak discharge. The error is much smaller than that obtained by using the slope-area methods. Based on the flood stage indicators, the peak discharges of modern floods were also reconstructed in the same reach using the HEC-RAS model and the same hydraulic parameters. The error between the reconstructed and gauged peak flood discharges is between -3.9% and 1.0%. These showed that the palaeoflood peak discharges reconstructed by using the HEC-RAS model are reliable. The reconstructed peak discharges of the palaeoflood are much larger than those of the gauged largest floods in the upper reaches of the Hanjiang River. The flood data series of the river are therefore extended to a 10,000-year time-scale. This result provides reference in hydrological engineering, water resource management and flood mitigation on the river. And it is also very helpful in understanding the relationships between extreme flood events and global climate change.

Key words: palaeoflood hydrology, HEC-RAS hydraulic model, Holocene, Hanjiang River

刘涛, 黄春长, 庞奖励, 查小春, 周亚利, 张玉柱, 刘科. 汉江上游郧县五峰段史前大洪水水文学恢复研究[J]. 地理学报, 2013, 68(11): 1568-1577.

LIU Tao, HUANG Chunchang, PANG Jiangli, ZHA Xiaochun, ZHOU Yali, ZHANG Yuzhu, LIU Ke. Hydrological reconstructions of the pre-historical great floods in the Wufeng Reach of Yunxian County in the upper Hanjiang River[J]. Acta Geographica Sinica, 2013, 68(11): 1568-1577.

参考文献

[1] Baker V R. Palaeoflood hydrology in a global context. Catena, 2006, 66(1/2): 161-168.
[2] Nathan A Sheffer, Mayte Rico, Yehouda Enzel et al. The palaeoflood record of the Gardon River, France: A comparison with the extreme 2002 flood event. Geomorphology, 2008, 98: 71-83.
[3] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary hydro-climatic events during the period AD 200-300 recorded by slackwater deposits in the upper Hanjiang River valley, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 374: 274-283.
[4] Knox J C. Sensitivity of modern and Holocene floods to climate change. Quaternary Science Reviews, 2000, 19: 439-457.
[5] Benito G, Thorndycraft V R, Rico M et al. Palaeo flood and floodplain records from Spain: Evidence for long-term climate variability and environmental changes. Geomorphology, 2008, 101: 68-77.
[6] Kochel R C, Baker V R. Palaeoflood hydrology. Science, 1982, 215: 353-361.
[7] Zhan Daojiang, Xie Yuebo. Palaeoflood Study. Beijing: China WaterPower Press, 2001: 1-83.[詹道江, 谢悦波. 古洪水研究. 北京: 中国水利水电出版社, 2001: 1-83.]
[8] Alpa S. A mid-late Holocene flood record from the alluvial reach of the Mahi River, western India. Catena, 2007, 70: 330-339.
[9] Gerardo B, Alfonso S, Yolanda S et al. Palaeoflood record of the Tagus River (Central Spain) during the Late Pleistocene and Holocene. Quaternary Science Reviews, 2003, 22: 1737-1756.
[10] Yael Jacoby, Tamir Grodek, Yehouda Enzel. Late Holocene upper bounds of flood magnitudes and twentieth century large floods in the ungauged, hyperarid alluvial Nahal Arava, Israel. Geomorphology, 2008, 95: 274-294.
[11] Ortega J A, Garz′on G. A contribution to improved flood magnitude estimation in base of palaeoflood record and climatic implications. Natural Hazards and Earth System Sciences, 2009, 9: 229-239.
[12] England J F Jr, Godaire J E, Klinger R E et al. Paleohydrologic bounds and extreme flood frequency of the upper Arkansas River, Colorado, USA. Geomorphology, 2010, 124: 1-16.
[13] Webb R H, Jarrett R. D. One-dimensional estimation techniques for discharges of paleofloods and historical floods. Water Science and Application, 2002, 5: 111-125.
[14] Yang Dayuan, Ge Yu, Xie Yuebo et al. Sedimentary records of large Holocene floods from the middle reaches of the Yellow River, China. Geomorphology, 2000, 33(1/2): 73-88.
[15] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Sedimentary records of the extraordinary floods at the ending of the mid-Holocene Climatic Optimum along the upper Weihe River, China. Holocene, 2012, 22(6), 675-686.
[16] Huang Chunchang, Pang Jiangli, Zha Xiaochun. Holocene palaeoflood events recorded by slackwater deposits along the upper Jinghe River valley, middle Yellow River basin, China. Journal of Quaternary Science, 2012, 27(5), 485-493.
[17] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary floods related to the climatic event at 4200 a BP on the Qishuihe River, middle reaches of the Yellow River, China. Quaternary Science Reviews, 2011, 30: 460-468.
[18] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary floods of 4100-4000 a BP recorded at the Late Neolithic ruins in the Jinghe River gorges, middle reach of the Yellow River, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 289(3): 1-9.
[19] Xie Yuebo, Fei Yuhong, Shen Qipeng. Slack water deposits and flow peak level of a paleoflood. Acta Geoscientia Sinica, 2001, 22(4): 320-323.[谢悦波, 费宇红, 沈起鹏. 古洪水平流沉积与水位. 地球学报, 2001, 22(4): 320-323.]
[20] Huang Chunchang, Li Xiaogang, Pang Jiangli et al. Palaeoflood sedimentological and hydrological studies on the Yongheguan reach in the middle Yellow River. Acta Geographica Sinica, 2012, 67(11): 1493-1504.[黄春长, 李晓刚, 庞奖励等. 黄河永和关段全新世古洪水研究. 地理学报, 2012, 67(11): 1493-1504.]
[21] Shi Fucheng, Yi Yuanjun, Mu Ping. Investigation, Research and Study on the Yellow River Historical Flood. Zhengzhou: Yellow River Water Conservancy Press, 2002: 81-123.[史辅成, 易元俊, 慕平. 黄河历史洪水调查、考证和研究. 郑州: 黄河水利出版社, 2002: 81-123.]
[22] Li Wenhao. Hydrologic characteristics analysis in the upper reaches of Hanjiang River. Journal of Water Resources & Water Engineering, 2004, 15(2): 54-58.[李文浩. 汉江上游流域水文特性分析. 水资源与水工程学报, 2004, 15(2): 54-58.]
[23] Zhang Kai. Analyses of rainstorm and flood characteristics in the upper reaches of Hanjiang River. Journal of Catastrophology, 2006, 21(3): 98-102.[张楷. 汉江上游暴雨洪水特性研究. 灾害学, 2006, 21(3): 98-102.]
[24] He Sudi. Characteristics of soil erosion in Hanjiang valley and possble countermeasures. Resources and Environment in the Yangtze Basin, 1997, 6(3): 271-276.[贺素娣. 汉江流域水土流失特点及防治对策. 长江流域资源与环境, 1997, 6(3): 271-276.]
[25] Yang Yongde, Zou Ning, Guo Xiwang et al. Analysis and calculation of design flood at Baihe gauge station in Hanjiang River. Water Resources Research, 1997, 18(3): 36-38.[杨永德, 邹宁, 郭希望等. 汉江白河水文站设计洪水分析计算. 水资源研究, 1997, 18(3): 36-38.]
[26] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Prehistorical floods in the Guanzhong Basin in the Yellow River drainage area: A case study along the Qishuihe River Valley over the Zhouyuan Loess Tableland. Sci. Sin. Terrae, 2011, 41: 1658-1669.[黄春长, 庞奖励, 查小春等. 黄河流域关中盆地史前大洪水研究: 以周原漆水河谷地为例. 中国科学, 2011, 41: 1658-1669.]
[27] Zha Xiaochun, Huang Chunchang, Pang Jiangli et al. The Holocene palaeoflood events in the Yunxi Reach in the upper reaches of Hanjiang River. Acta Geographica Sinica, 2012, 67(5): 671-680.[查小春, 黄春长, 庞奖励等. 汉江上游郧西段全新世古洪水事件研究. 地理学报, 2012, 67(5): 671-680.]
[28] Li Xiaogang, Huang Chunchang, Pang Jiangli et al. Palaeoflood hydrological study in the Baihe Reach in the upper reaches of the Hanjiang River. Scientia Gepgraphica Sinica, 2012, 32(8): 971-978.[李晓刚, 黄春长, 庞奖励等, 汉江上游白河段万年尺度洪水水文学研究. 地理科学, 2012, 32(8): 971-978.]
[29] Xu Jie, Huang Chunchang, Pang Jiangli et al. Sedimentological and hydrological studies of the palaeoflood events in the Ankang east section in the upper reaches of the Hanjiang River. Journal of Lake Sciences, 2013, 25(3): 445-454.[许洁, 黄春长, 庞奖励等. 汉江上游安康东段全新世古洪水沉积学与水文学研究. 湖泊科学, 2013, 25(3): 445-454.]
[30] Zhang Yuzhu., Huang Chunchang, Pang Jiangli et al. Holocene palaeofloods related to climatic events in the upper reaches of the Hanjiang River valley, middle Yangtze River Basin, China. Geomorphology, 2013, 195: 1-12.
[31] Qin Jiaming, Yuan Daoxian, Cheng Hai et al. The Y. D. and climate abrupt events in the early and middle Holocene:stalagmite oxygen isotope record from Maolan, Guizhou, China. Science in China: Series D, 2005, 48(4): 530-537.
[32] Gasse, F. Diatom-inferred salinity and carbonate oxygen isotopes in Holocene waterbodies of the western Sahara and Sahel (Africa). Quaternary Science Reviews, 2002, 21: 737-767.
[33] Mayewski P A, Meeker L D. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110, 000-year long glaciochemical series. Journal of Geophysical Research, 1997, 102: 26345-26366.
[34] Meese D A, Gow A J, Grootes P et al. The accumulation record from the GISP2 Core as an indicator of climate change throughout the Holocene. Science 1994, 266: 1680-1682.
[35] US Army Corps of Engineers HEC. HEC-RAS River Analysis System Hydraulic Reference Manual. Davis, California, USA, 2010.
[36] School of Water Resource and Hydropower. Hydraulics. Beijing: Higher Education Press, 1986: 335-336.[武汉水利电力学院水力学教研室. 水力学. 北京: 高等教育出版社, 1986: 335-336.]
[37] Chow V T. Open-channel Hydraulics. New York: McGraw-Hill Book Company Inc., 1959.
[38] O'Connor J E, Webb R H. Hydraulic modelling for paleoflood analysis//Baker V R, Kochel R C, Patton P C. Flood Geomorphology. New York: Wiley, 1988: 393-402.

汉江上游郧县五峰段史前大洪水水文学恢复研究

Hydrological reconstructions of the pre-historical great floods in the Wufeng Reach of Yunxian County in the upper Hanjiang River

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