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汉江上游郧西段全新世古洪水水文学研究

, PP. 55-62

Keywords: 滞流沉积物,古洪水,汉江,全新世

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Abstract:

通过对汉江上游的考察,在郧西段归仙河口(GXHK)发现了典型的全新世古洪水滞流沉积剖面。采集滞流沉积层样品,进行粒度、磁化率等分析,证明研究地点具有典型的古洪水滞流沉积层。通过地层学对比分析,确定两次古洪水事件分别发生在3000-2700aB.P.和公元100-200年(即1850-1750aB.P.)。利用沉积学、水文学方法计算出GXHK的古洪水流量介于63090~64320m3/s之间。用2010年、2011年大洪水洪痕的现代水文学验证和美国学者Baker提出的河流流域面积与大洪水洪峰流量关系进行对比分析,证明古洪水水文学计算结果合理可靠,从而为汉江上游的工程建设及沿岸地区的防洪减灾提供参考。

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