黄土高原典型淤地坝淤积机理研究
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国家自然科学基金项目“坡面径流侵蚀输沙动力过程试验研究”(40371075);黄河水利委员会“十五”重大治黄科技项目“大理河流域水土保持生态工程建设的减沙作用研究”(2002SZ08);西安理工大学优秀博士学位论文研究基金资助(106—210622)


Study on Depositing Process of Check Dam on the Loess Plateau
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    摘要:

    在调查典型淤地坝挖取剖面采集土样的基础上,利用库容曲线和实测淤积厚度求得每层淤积泥沙量。根据大水对大沙的原则,反演淤积层所对应的次侵蚀性降雨。通过层淤积量与其相应次侵蚀性降雨的最大30 min降雨强度I30,降雨量P,降雨侵蚀力R,平均降雨强度I等4个指标的相关分析,结果表明,对于无泄洪设施的淤地坝坝地每层淤积量与次侵蚀性降雨的I30,P,R关系密切,并建立了淤积量与I30,P,R的三元回归方程,计算值与实测值拟合较好,从而为淤地坝水毁问题的研究提供了理论基础。

    Abstract:

    The deposited volume of each check dam layer was determined by investigating the status of check dams on the loess plateau , digging typical check dams , carrying out the sectional analysis , utilizing reservoir storage and measuring deposited thickness of a layer. Single erosive rainfall was ascertained according to the principle of“more rain , more sediment yield”. Correlation analyses of deposited volume with the maximum rainfall intensity in thirty minutes (I30) , rainfall amount (P) , rainfall erosivity (R) and average rainfall intensity ( I) were made , the re-sult of which indicated close relationships among them. Relationships between deposited volume and the three in-dexes were then established. A good fitting plot between calculated result and observed data was found. The re-search offers a theory basis for the study of water2induced damage.

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魏霞,李占斌,李鹏,鲁克新,李勋贵.黄土高原典型淤地坝淤积机理研究[J].水土保持通报,2006,(6):10-13,31

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  • 收稿日期:2005-11-20
  • 最后修改日期:2006-09-20
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  • 在线发布日期: 2014-11-26
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