赵景波, 王娜, 龙腾文. 唐代泾河流域洪涝灾害研究[J]. 海洋地质与第四纪地质, 2008, 28(3): 109-113.
引用本文: 赵景波, 王娜, 龙腾文. 唐代泾河流域洪涝灾害研究[J]. 海洋地质与第四纪地质, 2008, 28(3): 109-113.
ZHAO Jing-bo, WANG Na, LONG Teng-wen. RESEARCH ON FLOOD DISASTERS OF JINGHE RIVER VALLEY IN TANG DYNASTY[J]. Marine Geology & Quaternary Geology, 2008, 28(3): 109-113.
Citation: ZHAO Jing-bo, WANG Na, LONG Teng-wen. RESEARCH ON FLOOD DISASTERS OF JINGHE RIVER VALLEY IN TANG DYNASTY[J]. Marine Geology & Quaternary Geology, 2008, 28(3): 109-113.

唐代泾河流域洪涝灾害研究

RESEARCH ON FLOOD DISASTERS OF JINGHE RIVER VALLEY IN TANG DYNASTY

  • 摘要: 通过对历史文献资料的搜集、整理、分析,对唐代泾河流域洪涝灾害进行了研究。结果表明,唐代泾河流域洪涝灾害共发生82次,平均每3.52年发生一次;在唐中期的703840年间,共有洪涝灾害51次,平均2.69年发生一次,占洪涝灾害次数的62.2%;在唐代早期的618702年间和唐代晚期的841-907年间洪涝灾害平均分别为每5.60年和4.13年发生一次,分别占18.3%和19.5%。唐代泾河流域洪涝灾害可分为3个时期,中期为洪涝灾害多发期,早期和晚期为洪涝灾害较少发生期。唐代泾河流域一级轻度涝灾共发生37次,占洪涝灾害发生次数的45.1%;发生二级洪涝灾害34次,占41.5%;发生三级大洪涝灾害8次,占9.6%;发生四级特大洪涝灾害5次,占6.1%。唐代泾河流域持续时间长的大涝灾和特大涝灾的发生主要是当年降水量的明显增加造成的,是当年降水量增加或气候短暂变湿润的结果;持续时间短的轻度和中度涝灾的发生主要是降水量的集中和暴雨引起的,一般不代表年降水量的增加。初步认为,唐代中期降水量较多,气候较早期和晚期湿润。

     

    Abstract: Through collection and analysis of historical materials,changes, ranks and origins of flood disasters in the Tang Dynasty in Jinghe River valley were studied in this paper. The results show that 82 flood disasters occurred altogether in the Tang Dynasty, and averagely occurred once every 3.52 years. Flood disaster in the Jinghe River valley in the Tang Dynasty mainly concentrated in the middle stage (703-840 AD) of the Tang Dynasty, 51 flood disasters occurred altogether in this stage,averagely once every 2.69 years, and accounts for 62.2%. In the early (618-702 AD) and late stages (841-907 AD) of the Tang Dynasty, flood disasters were fewer, and there were 15 and 16 flood disasters respectively, which occurred once every 5.6 and 4.13 years and accounts for 18.30% and 19.52% respectively. The first rank of flood disasters in the Tang Dynasty in this valley takes 45.1%, the second rank is 41.5 Y00, the third and fourth ranks are 9.6% and 6.1% respectively. Of the 82 flood disasters that occurred in Tang Dynasty in this valley,moderate and mild disasters are dominant, big flood disasters come second, and catastrophic flood disasters are much less. The flood disaster rank and frequency indicate that the climate can be divided into three stages in Tang Dynasty in the valley, the early and late stages had small precipitations, and the middle stage had more precipitation. Main reasons for flood disaster occurrence were climate fluctuation, concentrated rainfall and rainstorm. The big and catastrophic flood disasters were caused by obviously increased mean annual precipitation which indicates short moist climate, and the moderate and mild disasters were caused by concentrated rainfall and rainstorm. According to the duration and annual precipitation in recent Weihe River valley, the mean annual precipitation was mostly 900-1 000 mm during the period of catastrophic disaster in the Tang Dynasty and the big flood represented a significant increase in precipitation.

     

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