长江流域资源与环境 >> 2014, Vol. 23 >> Issue (s): 6-.doi: 10.11870/cjlyzyyhj2014Z1002

• 自然资源 • 上一篇    下一篇

1990~2013年资水流域汛期径流量变化规律分析

刘培亮,毛德华,周慧,何晴亲   

  1. (1.湖南师范大学资源与环境科学学院,湖南 长沙 410081;2.湖南省水文水资源勘测局,湖南 长沙 410007)
  • 出版日期:2014-11-26

ANALYSIS ON VARIATION LAW OF THE FLOOD SEASON’S RUNOFF IN ZISHUI RIVER BASIN DURING 1990-2013

LIU Peiliang1,MAO Dehua1,ZHOU Hui1,2,HE Qingqin1   

  1. (1.Resources and Environmental Science Institute,Hunan Normal University,Changsha 410081,China; 2.Hydrology and Water Resources Survey Bureau of Hunan Province,Changsha 410007,China
  • Online:2014-11-26

摘要:

分析资水流域汛期径流量变化规律能够为流域水资源开发利用和水旱灾害的防治提供重要的理论依据。根据资水干流主要代表水文站1990~2013年汛期月径流量实测数据,应用分配不均匀系数和变化幅度等方法指标、滑动平均法和MannKendall非参数趋势检验法分析了资水流域汛期径流量的年内和年际变化规律,并应用汛期内分配指标与湖南省水旱灾害状况进行了灰色关联度分析。结果表明:(1)资水流域径流量在汛期内各月之间分配极不均匀,但随时间的推移,逐渐趋向均匀;汛期内各月径流量呈现在波动中递减的趋势;罗家庙站、冷水江站和桃江站各项分配指标值总体呈现下降的趋势。(2) 资水径流量汛期内分配特征指标与流域水旱灾害的灰色关联度极高,并能较好的反映当年流域汛期水旱灾害情况。(3)资水流域汛期径流量呈现先上升,再下降,再上升的变化趋势,但总体呈现下降的趋势。(4)罗家庙站和冷水江站分别于2009年和2010年发生了突变,桃江站未发生过突变

Abstract:

The variation law of runoff has gained increasing attentions in hydrology and water resource research over the past decades,and is the key issue for sustainable use of regional water resources and water conservancy project.Exploration of the variation law of the flood seasons runoff in Zishui River Basin will provide an important theoretical reference in understanding the hydrological characteristics of the Zishui River and the sustainable use of regional water resources.River runoff changes also have some influence to flood and drought disasters of the river basin.Especially the frequency of flood and drought disasters in the southern,which occur in the flood season,is higher.As a typical representative of the southern river,Zishui,in recent years,shows an upward trend of flooding which brings great losses.Studying the variation law of the flood seasons runoff in Zishui River Basin also can provide a scientific basis for preventing flood and drought disasters.Based on monthly runoff data from 1990 to 2013 in the flood season of three representative stations in Zishui River Basin,including Luojiamiao,Lengshuijiang and Taojiang hydrological station,the intraannual changes of runoff in the flood season were analyzed by using nonuniformity coefficient and amplitude of variation; then application of these index values and flood and drought disasters in Hunan province has carried on grey correlation degree analysis; besides,the interannual changes of runoff in the flood season were studied by moving average and the MannKendall mutation test.The results are as follows. (1) During the flood season,the distribution of runoff was quite uneven in the Zishui River Basin,however,the runoff distribution tended to be even with the lapse of time.The monthly runoff showed a decreasing trend with fluctuation.As a whole,the indicators from the three stations presented a decreasing trend.(2) The grey correlation degree of runoff distribution characteristic index value during the flood season and river basins flood and drought disasters was extremely high.The characteristics of annual runoff distribution in the flood season of Zishui River Basin could better reflect the current years flood and drought disasters.The larger the value of the four indicators which reflect the uneven distribution during the flood season was,the more often flood and drought disasters would happen.(3) The distribution of interannual flood seasons runoff of Zishui River Basin was quite uneven,too.At first,it showed an increasing trend,then it fell,and it rose finally.However,in general,it presented a trend of decreasing.(4) Luojiamiao station,Lengshuijiang station and Taojiang station broke through the 95% confidence interval in 2007-2013,1990-1991 and 2010-2013,1990-1991 and 2004-2013,during these annual times the flood seasons runoff showed a trend of a significant reduction.Luojiamiao station and Lengshuijiang station appeared mutational sites in 2009 and 2010.For Taojiang station,UF statistics did not intersect with UB statistics and there have been no mutational site.

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