文章摘要
齐璞,姬美秀,孙赞盈.利用水库泄空冲刷形成高含沙水流的机理[J].水利学报,2006,37(8):906-912
利用水库泄空冲刷形成高含沙水流的机理
Formation mechanism of hyper-concentrated sediment flow caused by scouring of reservoir emptying
投稿时间:2005-07-25  
DOI:
中文关键词: 水库淤积物  饱和状态  抗剪强度  泄空冲刷  高含沙水流
英文关键词: reservoir sediment  saturated  shear strength  scouring of reservoir emptying  high concentrated sediment flow
基金项目:国家自然科学基金重大项目(598902000);水利部重点项目
作者单位
齐璞 黄河水利科学研究院河南 郑州 450003 
姬美秀 浙江大学 建筑工程学院浙江 杭州 310027 
孙赞盈 黄河水利科学研究院河南 郑州 450003 
摘要点击次数: 1773
全文下载次数: 215
中文摘要:
      利用黄河干支流水库运用的实测资料,对高含沙水流的产生条件进行了研究。结果表明,水库水位的迅速下降并泄空,可使水库的淤泥流动并产生高含沙水流。水库淤土抗剪强度参数(C和Φ)依排水条件而异,抗剪强度一般不排水不固结的最小。水库淤积物在水下处于饱和状态,库水位迅速降低时,淤土中的孔隙水来不及排出,摩擦角值低,Φ=0,只要下滑的剪力大于黏着力淤泥便开始流动。当库区淤积物抗冲性较强时,溯源冲刷纵剖面调整又具有自动调整的特性,使冲刷以“局部跌坎”的形式向上游发展,使水流能量集中,加强冲刷能力,随着主槽冲深,滩槽差增大,促使淤土向主槽内滑塌,为高含沙水流形成创造了有利条件。
英文摘要:
      The formation condition of hyper concentrated sediment flow is investigated based on the operation practice of reservoirs in Yellow River. Generally, the sedimentation in reservoir is always saturated and unconsolidated. The pore water will not be drained when the water level is rapidly dropped. Under this condition, the interior friction angle of the sediment is approximately equal to zero, so that the shear strength of soil is approximately only dependent on the bounding coefficient of the soil. If the sliding force due to water level dropping is higher than the shear strength the movement of sediment will occur. In case the erosion resistance of the sedimentation is high the retrogressive erosion of the river may concentrated to the main stream and forming a deep channel. The elevation difference between the floodplain and deep channel results in the sliding of the sediment towards the main channel and forms the high concentrated sediment flow.
查看全文   查看/发表评论  下载PDF阅读器
关闭