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
胡贵明, 黄春长, 周亚利, 庞奖励, 查小春, 郭永强
Hu Guiming, Huang Chunchang, Zhou Yali, Pang Jiangli, Zha Xiaochun, Guo Yongqiang
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。
中图分类号:
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