降水一水土保持一径流统计模型在潮河流域的应用
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“十一五”国家科技支撑计划项目“华北土石山区防护林体系空间配置与结构优化技术研究”(2006BAD03A0201);“十一五”国家水体污染控制与治理科技重大专项“典型北方缺水城市湖泊水质水量保障与生境改善技术”(2008ZX07106-003-1)


Application of a Rainfall一Soil and Water Conservation一Runoff Statistical Model in Chaohe River Basin
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    摘要:

    以密云水库以上的潮河流域作为研究区域,对流域1961-2005年的还原年径流量、年降水量、年水土保持措施(水平梯田和造林)面积数据进行了多元回归分析。建立基于降水-水土保持-径流之间关系的统计模型,定量评估了该区水土保持措施对流域年径流量的影响程度。模型评估结果表明,1961-1970年,1971-1980年,1981-1990年,1991-2000年,2001-2005年,流域水土保持措施的年均减水效应分别为2.54%,3.52%,28.71%,6.87%和48.02%;1981-2005年,流域水土保持措施的年均减水效应比较显著为22.96%。2001-2005年的年均减水效应最大,1981-1990年的年均减水效应次之,1991-2000年的年均减水效应最小。水土保持措施对枯水时段的减水效应更为突出。

    Abstract:

    Taking the Chaohe River Basin above the Miyun Reservoir as a study area,the influence of soil and water conservation measures on annual runoff was assessed quantitatively by the rainfall-soil and water conservation-runoff statistical model established on the basis of multiple regression analysis using historical annual runoff,annual precipitation and areas of soil and water conservation measures in the drainage basin during 1961-2005.The results showed that during 1961-1970,1971-1980,1981-1990,1991-2000 and 2001-2005,the average annual runoff-reduction effects were 2.54%,3.52%,28.71%,6.87% and 48.02%,respectively,with an average of 22.96% during 1981-2005.The average annual runof-freduction effect was the greatest during 2001-2005,intermediate during 1981-1990,and the smallest during 1991-2000.The runoff reduction effects of soil and water conservation measures were more profound in the drier period.

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李子君.降水一水土保持一径流统计模型在潮河流域的应用[J].水土保持通报,2011,(3):136-139

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  • 收稿日期:2010-10-06
  • 最后修改日期:2010-11-30
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  • 在线发布日期: 2014-11-26
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