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试论清代中晚期汾河上游人类活动与太原水患加剧之关系
引用本文:赵海晓,任伯平,王尚义.试论清代中晚期汾河上游人类活动与太原水患加剧之关系[J].太原师范学院学报(自然科学版),2006,5(4):103-106,136.
作者姓名:赵海晓  任伯平  王尚义
作者单位:1. 山西大学,黄土高原研究所,山西,太原,030012
2. 太原师范学院,历史地理与环境变迁研究所,山西,太原,030012
3. 山西大学,黄土高原研究所,山西,太原,030012;太原师范学院,历史地理与环境变迁研究所,山西,太原,030012
摘    要:作者应用水患频率五年滑动平均数法,分析了清乾隆初年至公元1911年间太原阳曲两县水患频率的增长情况,指出:乾隆初年fd=0.085,fd〈0.2水患较轻,但以后逐步加剧,至清末0-2〈fd〈0.5灾情已相当严重,同频率的特大洪峰增大了一倍以上.分析认为这与汾河上游人口增加、耕地扩张有一定联系.

关 键 词:人类活动  水患  汾河上游  清代中晚期
文章编号:1672-2027(2006)04-0103-05
收稿时间:2006-05-24
修稿时间:2006-05-24

On the Relationship Between Human Activity of the Upper Reaches of Fenhe River in the Middle and Later Periods of Qing Dynasty and the Worsening of Taiyuan's Flood Disaster
Zhao Haixiao,Ren Boping,Wang Sangyi.On the Relationship Between Human Activity of the Upper Reaches of Fenhe River in the Middle and Later Periods of Qing Dynasty and the Worsening of Taiyuan''''s Flood Disaster[J].Journal of Taiyuan Normal University:Natural Science Edition,2006,5(4):103-106,136.
Authors:Zhao Haixiao  Ren Boping  Wang Sangyi
Institution:1. Institute of Loess Plateau,Shanxi University,Shanxi Taiyuan 030012 2. Institule of Historical Geograply and Enviroment Changes,Taiyuan Normal University,Taiyuan 030012,China
Abstract:With the application of five-year slide average of flood frequency alytical method,the authors analyse the flood in Taiyuan and Yangqu from the first years of Qianlong period of Qing Dynasty to 1911. They state that the flood in the beginning of Qianlong period was slighter,but it became more serious increasingly in the end of Qing Dynasty,and the great flood peak of the same frequency became twice as big as that of past time. The result is related to the increasing of the population in the upper reaches of Fenhe River and the extending of plantation there.
Keywords:human activity  flood disaster  upper reaches of Fenhe River  middle and later periods of Qing Dynasty
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