吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (6): 1822-1832.doi: 10.13278/j.cnki.jjuese.201506206

• 地质工程与环境工程 • 上一篇    下一篇

黄河上游靖远-景泰段全新世古洪水水文学

胡贵明, 黄春长, 周亚利, 庞奖励, 查小春, 郭永强   

  1. 陕西师范大学旅游与环境学院, 西安 710062
  • 收稿日期:2015-02-23 发布日期:2015-11-26
  • 通讯作者: 黄春长(1953),男,教授,博士生导师,主要从事资源开发与环境演变研究,E-mail:cchuang@snnu.edu.cn。 E-mail:cchuang@snnu.edu.cn
  • 作者简介:胡贵明(1989),男,博士研究生,主要从事资源开发与环境演变研究,E-mail:guduyuyi@163.com
  • 基金资助:

    国家自然科学基金项目(41471071);教育部博士点基金优先发展领域项目(20110202130002)

Palaeoflood Hydrological Reconstruction in Jingyuan- Jingtai Reach in Upper Yellow River Valley

Hu Guiming, Huang Chunchang, Zhou Yali, Pang Jiangli, Zha Xiaochun, Guo Yongqiang   

  1. College of Tourism and Environmental Sciences, Shaanxi Normal University, Xi'an 710062, China
  • Received:2015-02-23 Published:2015-11-26

摘要:

对黄河上游靖远景泰段峡谷进行系统野外考察,在靖远县金坪村(JPC)发现典型的全新世古洪水滞流沉积物。通过光释光(OSL)测年和与黄河吉县段FJJ剖面进行地层对比,确定这期特大古洪水事件发生在 3 200~3 000 a B.P.,即全新世中期晚期气候恶化转折阶段,对应着我国历史上商末至西周早期。采用古洪水水文学方法恢复古洪水洪峰水位,并且采用比降-面积法计算这一期多次古洪水事件的洪峰流量为 16 110~17 740 m3/s。同时,根据野外调查获得 2012年7月31日黄河上游大洪水的洪痕高程,采用相同参数和方法恢复其洪峰流量,误差仅有 2.7%,表明在该河段对于古洪水水文恢复计算参数选取和计算结果是可靠的。

关键词: 黄河上游, 全新世, 古洪水, 滞流沉积物, 水文学

Abstract:

A systematical field investigation is carried out in the upper Yellow River valley from Jingtai to Jingyuan reach. Palaeoflood slackwater deposits (SWD) are identified at several sites. The Holocene sediment profile at the site of Jinpingcun (JPC) is chosen for a further study on the palaeoflood hydrology. OSL dating and stratigraphic correlation with Jixian (FJJ) site in the middle reach gorge of the Yellow River show that these extreme palaeoflood events occurred during 3 200-3 000 a B.P., at the time when the climate was at the turn from the Middle Holocene climatic optimum to the Late Holocene dry period. This corresponds to the transition period from Shang Dynasty to Western Zhou Dynasty when many serious drought and flood disasters, harvest failures, and major social changes occurred. The palaeoflood stage is obtained by palaeohydrological methods. The reconstructed palaeoflood peak discharges were 16 110-17 740 m3/s using the slope-area method. Reconstruction of current flood (in 2012.07.31) and comparison with the gauged discharge prove that the hydrological method and hydrological parameters used are reliable. These results are very important to establish the relationship between peak discharge and occurrence frequency by 10 000-year time-scale in Lanzhou to Jingyuan reach. The method is very useful in Hydraulic engineering along the upper Yellow River.

Key words: upper Yellow River, Holocene, palaeoflood, slackwater deposit, hydrology

中图分类号: 

  • P476

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