黄土高原藉河流域1962-2008年径流变化特征
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1. 北京林业大学,水土保持学院,北京,100083
2. 华北电力大学,能源与环境研究中心,北京,102206
3. The Federal Institute of Land and Water Management Research,A-3252,Petzenkirchen,Austria

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S273.29

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国家自然科学基金项目"黄土高原地区典型多尺度耦合流域土地利用/覆被的水文生态响应研究"(40871136)


Runoff Variations in Jihe River Watershed of Loess Plateau from 1962 to 2008
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GUO Jun-ting1,ZHANG Zhi-qiang1,WANG Sheng-ping2,ZHANG Jian-jun1,Strauss Peter3(1.Institute of Soil and Water Conservation,Beijing Forestry University,Beijing 100083,China,2.North China Electric Power University,Energy and Environment Research Center,Beijing 102206,3.The Federal Institute of Land and Water Management Research,A-3252 Petzenkirchen,Austria)

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    摘要:

    采用1962-2008年近50a的径流资料,应用统计分析方法,对黄土高原第三副区藉河流域的径流变化进行了分析.结果表明,流域径流呈明显下降趋势,20世纪70,80,90年代和2000年以来径流分别是60年代的62.3%,61.1%,30.2%和35.2%,年均递增率为-2.1%,年际变差系数为0.75;流域径流年内分配极不平衡,汛期径流占全年总量达50.8%~95.2%,平均76.5%,不均匀系数为1.13;根据径流丰枯等级划分,藉河流域60年代至今分别经历了丰水期、平水期、偏丰期和枯水期,1990年以来流域径流急剧下降,出现连续9a的枯水年,这与流域内近些年大规模水土保持综合治理密切相关,深入分析土地利用/覆被变化的水文要素响应也是该区未来的研究重点.

    Abstract:

    Based on the runoff data during the period between 1962and 2008,runoff variations in the Jihe river watershed(1019km2), located in the third sub-region of the Loess Plateau,were characterized using statistical analysis.The results indicate that the runoff presented a evident decreasing trend during the research period,and the runoff in the 1970s,1980s,1990sand 2000saccounted for 62.3%,61.1%,30.2% and 35.2% of the 1960srespectively,with an annual increasing rate of-2.7%and and a variation coefficient of 0.75.It was observed that inter-annual distribution of runoff was greatly unsteady,and the runoff percentages in flood seasons ranged from 50.8%to 95.2% with an average of 76.5%and a monthly variation coefficient of 1.13.According to wet and drought year classification of the runoff,Jihe river watershed has gone since the 1960s through the periods of wet year,average year,sub-wet year and drought year,respectively.The runoff decreased dramatically after 1990,lasting a nine-year period of drought,in coincidence with the large-scaled implementation of soil and water conservation.Thorough descriptions of the response of hydrological factors to land use and cover changes are another requirement for future study in the watershed.

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李庆云,余新晓,张璐,信忠保,贾国栋,王友生,郑江坤.黄土高原藉河流域1962-2008年径流变化特征[J].水土保持通报,2011,(1):98-102

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  • 收稿日期:2010-07-17
  • 最后修改日期:2010-08-17
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  • 在线发布日期: 2012-10-25
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