地理学报 ›› 2012, Vol. 67 ›› Issue (5): 671-680.doi: 10.11821/xb201205009
查小春, 黄春长, 庞奖励, 周亚利
收稿日期:
2011-11-06
修回日期:
2012-02-16
出版日期:
2012-05-20
发布日期:
2012-05-20
基金资助:
ZHA Xiaochun, HUANG Chunchang, PANG Jiangli, ZHOU Yali
Received:
2011-11-06
Revised:
2012-02-16
Online:
2012-05-20
Published:
2012-05-20
Supported by:
摘要: 古洪水水文学是全球变化科学领域的前沿课题。通过对汉江上游的深入调查研究,在郧西段基岩峡谷发现全新世古洪水滞流沉积地层。通过沉积学观察研究,采样分析和与2010年汉江洪水滞流沉积物的粒度、磁化率特征对比,判定为典型的全新世洪水滞流沉积物(SWD)。通过全新世地层对比和光释光(OSL) 测年,确定其记录了全新世时期3200-2800 a BP的特大古洪水事件。在确定了古洪水洪峰水位和相关参数的基础上,采用比降法水文模型推算出该期洪水洪峰流量在48830~51710 m3/s 之间。同时在该断面观测了汉江上游1983 年、2005 年和2010 年洪水洪痕水位,采用相同水文参数和模型,恢复了其洪峰流量,与白河水文站实测流量比较,误差在1.99%~4.21%之间,说明我们对于古洪水水文参数选择与洪峰流量计算结果是合理的。从而将古洪水数据加入洪水频率序列中,建立了万年尺度洪水流量与频率关系。该研究成果为汉江上游水资源水能源开发利用和防洪减灾等,提供了重要的水文资料。
查小春, 黄春长, 庞奖励, 周亚利. 汉江上游郧西段全新世古洪水事件研究[J]. 地理学报, 2012, 67(5): 671-680.
ZHA Xiaochun, HUANG Chunchang, PANG Jiangli, ZHOU Yali. The Holocene Palaeoflood Events in the Yunxi Reach in the Upper Reaches of Hanjiang River[J]. Acta Geographica Sinica, 2012, 67(5): 671-680.
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