地理学报 ›› 2012, Vol. 67 ›› Issue (11): 1493-1504.doi: 10.11821/xb201211006
黄春长, 李晓刚, 庞奖励, 查小春, 周亚利
收稿日期:
2012-07-18
修回日期:
2012-08-19
出版日期:
2012-11-20
发布日期:
2012-11-20
作者简介:
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
基金资助:
国家自然基金重点项目(41030637); 教育部博士点基金优先发展领域项目(20110202130002)
HUANG Chunchang, LI Xiaogang, PANG Jiangli, ZHA Xiaochun, ZHOU Yali
Received:
2012-07-18
Revised:
2012-08-19
Online:
2012-11-20
Published:
2012-11-20
Supported by:
National Natural Science Foundation of China, No.41030637; Ph. D. Programs Foundation from Ministry of Education of China, No.20110202130002
摘要: 通过对黄河中游晋陕峡谷段进行系统地考察, 在多个地点发现全新世古洪水滞流沉积物。选择永和关段YHG剖面进行了沉积学和水文学研究。根据野外宏观沉积学特征, 确定YHG 剖面含有一组五层古洪水滞流沉积层。采样分析测试表明其磁化率低、烧失量小、CaCO3含量低, 粒度成分分类为粉沙质细沙和细沙质粉沙。它们是黄河洪水悬移质泥沙在高水位滞流情况下的沉积物, 记录了黄河晋陕峡谷段一期五次特大古洪水事件。通过地层学对比分析和OSL 测年断代, 确定这五次洪水发生在全新世中期—晚期转折阶段, 即3200-3000 aBP。这也是我国历史上商末—西周初年的气候恶化转折阶段。利用“古洪水SWD厚度与含沙量关系法”恢复古洪水洪峰水位, 采用面积—比降法计算出5 次古洪水事件洪峰流量介于28380~48590 m3/s 之间。该结果有效地延长了黄河中游洪水数据序列, 为万年尺度洪水流量—频率关系的计算提供了基础数据。这对于黄河中下游水利水电工程洪水设计和洪水资源化开发管理具有重要的现实意义, 对于揭示黄河中游水文过程对于全球变化的响应规律具有重要的科学意义。
黄春长, 李晓刚, 庞奖励, 查小春, 周亚利. 黄河永和关段全新世古洪水研究[J]. 地理学报, 2012, 67(11): 1493-1504.
HUANG Chunchang, LI Xiaogang, PANG Jiangli, ZHA Xiaochun, ZHOU Yali. Palaeoflood Sedimentological and Hydrological Studies on the Yongheguan Reach in the Middle Yellow River[J]. Acta Geographica Sinica, 2012, 67(11): 1493-1504.
[1] Bureau of Hydrology and Water Resources in the Middle Reaches of the Yellow River. Hydrology of the MiddleReaches of the Yellow River: The Hekou to Longmen Part. Zhengzhou: Yellow River Conservancy Press, 2001:1-207. [黄河中游水文水资源局. 黄河中游水文—河口镇至龙门区间. 郑州: 黄河水利出版社, 2001: 1-207.][2] Xu Jiahua, Li Xiaoyu, Chen Jianjun et al. Effects of Engineering on Storm Rains and Floods in the Middle Reaches ofthe Yellow River: The Hekou to Longmen Part. Zhengzhou: Yellow River Conservancy Press, 2009: 1-340. [徐建华, 李晓宇, 陈建军等. 黄河中游河口镇至龙门区间水利水保工程对暴雨洪水泥沙影响研究. 郑州: 黄河水利出版社,2009: 1-340.][3] Baker V R. Palaeoflood hydrology in a global context. Catena, 2006, 66(1/2): 161-168.[4] Kochel R C, Baker V R. Palaeoflood hydrology. Science, 1982, 215: 353-361.[5] Benito G, Sopena A, Sanchez Y. Sedimentology of high-stage flood deposits of the Tagus River, Central Spain.Sedimentary Geology, 2003, 157: 107-132.[6] Yang Dayuan, Ge Yu, Xie Yuebo et al. Sedimentary records of large Holocene floods from the middle reaches of theYellow River, China. Geomorphology, 2000, 33(1/2): 73-88.[7] Zhan Daojiang, Xie Yuebo. Palaeoflood Study. Beijing: China Water Power 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] Ge Zhaoshuai, Yang Dayuan, Xie Yuebo et al. Holocene extraordinary flood of Qinhe River and its recurrence interval.Journal of Natural Disasters, 2004, 13: 144-148. [葛兆帅, 杨达源, 谢悦波等. 沁河流域全新世特大洪水及其重现期初步研究. 自然灾害学报, 2004, 13: 144-148.][9] Xie Yuebo, Wang Wenhui, Wang Ping. Characteristics of grain size for palaeoflood slackwater deposits. Journal ofChinese Hydrology, 2000, 20(4): 18-20. [谢悦波, 王文辉, 王平. 古洪水平流沉积粒度特征. 水文, 2000, 20(4): 18-20.][10] Xie Yuebo, Fei Yuhong, Shen Qipeng. Slack water deposits and flood peak level of a palaeoflood. Acta GeoscientiaSinica, 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.][11] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Prehistorical floods in the Guanzhong Basin in the Yellow Riverdrainage area: A case study along the Qishuihe River Valley over the Zhouyuan loess tableland. Science China: EarthScience, 2011, 41(11): 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: 地球科学, 2011, 41(11): 1658-1669.][12] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary floods related to the climatic event at 4200 a B.P.on the Qishuihe River, middle reaches of the Yellow River, China. Quaternary Science Reviews, 2011, 30: 460-468.[13] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary floods of 4100-4000 a BP recorded at the LateNeolithic ruins in the Jinghe River gorges, middle reach of the Yellow River, China. Palaeogeography,Palaeoclimatology, Palaeoecology, 2010, 289(3): 1-9.[14] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Sedimentary records of the extraordinary floods at the ending ofthe mid-Holocene climatic optimum along the upper Weihe River, China. Holocene, 2012, 22(6): 675-686.[15] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Holocene Palaeoflood Events recorded by slackwater depositsalong the Lower Jinghe River Valley, Middle Yellow River Basin, China. Journal of Quaternary Science, 2012, 27(5):485-493.[16] Li Xiaogang, Huang Chunchang, Pang Jiangli et al. Hydrological Studies of the Holocene palaeoflood in the Hukoureach of the Yellow River. Acta Geographica Sinica, 2007, 62(3): 291-300. [李晓刚, 黄春长, 庞奖励等. 黄河壶口段全新世古洪水事件及其水文学研究. 地理学报, 2010, 65(11): 1371-1380.][17] Wei Haiyan, Huang Chunchang, Zha Xiaochun et al. Sedimentary studies of the late Holocene flood slackwaterdeposits in the Shanxi-Shaanxi Gorges, middle reach of the Yellow River. Geological Review, 2010, 56(5):745-752. [魏海燕, 黄春长, 查小春等. 黄河中游晋陕峡谷段全新世晚期洪水滞流沉积研究. 地质论评, 2010, 56(5):745-752.][18] Hao Gaojian, Huang Chunchang, Xing Yingying et al. Sedimentary characteristics of the slackwater deposits ofHolocene extreme floods in the FJJ section in the Yellow River valley, Ji County. Journal of Arid Land Resources andEnvironment, 2011, 25(3): 106-112. [郝高建, 黄春长, 邢莹莹等. 黄河晋陕峡谷吉县段全新世古洪水滞流沉积特征研究. 干旱区资源与环境, 2011, 25(3): 106-112.][19] Wang Xiaqing, Huang Chunchang, Pang Jiangli et al. Sedimentological study of the palaeoflood slackwater deposits inthe Hukou-Longmen reach of the Yellow River. Chinese Journal of Soil Science, 2011, 42(4): 781-787. [王夏青, 黄春长, 庞奖励等. 黄河壶口至龙门段全新世古洪水滞流沉积物研究. 土壤通报, 2011, 42(4): 781-787.][20] Li Yuqin, Huang Chunchang, Zha Xiaochun et al. Paleoflood occurrence in the late period of the Longshan Culture inthe middle reaches of the Jinghe River. Acta Geographica Sinca, 2009, 64(5): 541-552. [李瑜琴, 黄春长, 查小春等.泾河中游龙山文化晚期特大洪水水文学研究. 地理学报, 2009, 64(5):541-552.][21] Yao Ping, Huang Chunchang, Pang Jiangli et al. Palaeoflood hydrological studies in the middle reaches of theBeiluohe River. Acta Geographica Sinica, 2008, 63(11): 1198-1206. [姚平, 黄春长, 庞奖励等. 北洛河中游黄陵洛川段全新世古洪水研究. 地理学报, 2008, 63(11): 1198-1206.][22] Zha Xiaochun, Huang Chunchang, Pang Jiangli. Holocene extreme floods and environmental change of QishuiheRiver in western Guanzhong Basin. Acta Geographica Sinica, 2007, 62(3): 291-300. [查小春, 黄春长, 庞奖励. 关中西部漆水河全新世特大洪水与环境演变. 地理学报, 2007, 62(3): 291-300.][23] Wan Honglian, Huang Chunchang, Pang Jiangli et al. Holocene extreme floods of the Baoji Gorges of the WeiheRiver. Quaternary Science, 2010, 30(2): 430-440. [万红莲, 黄春长, 庞奖励等. 渭河宝鸡峡全新世特大洪水水文学研究. 第四纪研究, 2010, 30(2): 430-440.][24] Wang Hengsong, Huang Chunchang, Zhou Yali et al. OSL dating of the paleoflood events in the middle reaches of theWeihe River. Acta Sedimentologica Sinica, 2012, 30(2): 102-111. [王恒松, 黄春长, 周亚利等. 渭河咸阳段全新世古洪水事件光释光测年研究. 沉积学报, 2012, 30(2): 102-111.][25] Wang Hengsong, Huang Chunchang, Zhou Yali et al. OSL dating of the Holocene paleoflood events: A case study ofthe Lintong segment in the lower Weihe River Valley. Acta Geoscientica Sinica, 2012, 33(2): 227-235. [王恒松, 黄春长, 周亚利等. 全新世古洪水事件光释光测年研究: 以渭河下游临潼段为例. 地球学报, 2012, 33(2): 227-235.][26] Huang Chunchang, Su Hongxia. Climate change and Zhou relocations in early Chinese history. Journal of HistoricalGeography, 2009, 35(2): 297-310.[27] Huang Chunchang, Pang Jiangli, Su Hongxia et al. Holocene environmental change inferred from the loess-palaeosolsequences adjacent to the floodplain of the Yellow River, China. Quaternary Science Reviews, 2009, 28(25/26):2633-2646.[28] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Impact of monsoonal climatic change on Holocene overbankflooding along the Sushui River, middle reaches of the Yellow River, China. Quaternary Science Reviews, 2007, 26:2247-2264.[29] James C Knox. Sensitivity of modern and Holocene foods to climate change. Quaternary Science Reviews, 2000, 19:439-457.[30] Huang Chunchang, Jia Yaofeng, Pang Jiangli et al. Holocene colluviation and its implications for tracinghuman-induced soil erosion and re-deposition on the piedmont loess lands of the Qinling Mountains, northern China.Geoderma, 2006, 136: 838-851.[31] Shi Fucheng, Yi Yuanjun, Mu Ping. Investigation, Research and Study on the Yellow River Historical Flood.Zhengzhou: Yellow River Water Conservancy Press, 2000: 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.][32] School of Water Resource and Hydropower in Wuhan. Hydraulics. Beijing: Higher Education Press, 1980: 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.] |
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