长江科学院院报 ›› 2018, Vol. 35 ›› Issue (6): 60-66.DOI: 10.11988/ckyyb.20161305

• 水力学 • 上一篇    下一篇

非淹没复式断面丁坝区的流速分布规律

钟亮1a,1b,王振志1b,王舒1b,周鑫靖2   

  1. 1.重庆交通大学 a. 国家内河航道整治工程技术研究中心;b.水利水运工程教育部重点实验室,重庆 400074;
    2.重庆市信息通信咨询设计院有限公司,重庆 400041
  • 收稿日期:2016-12-10 修回日期:2017-02-04 出版日期:2018-06-01 发布日期:2018-06-16
  • 作者简介:钟亮(1980-),男,江西赣州人,副教授,博士,主要从事航道整治理论与技术研究工作。E-mail:zlcqjtu@163.com
  • 基金资助:
    重庆市基础科学与前沿技术研究项目(CSTC2017jcyjAX0278);国家自然科学基金项目(51509026)

Flow Velocity Distribution Around Non-submerged Spur Dike with Compound Section

ZHONG Liang1,2,WANG Zhen-zhi2,WANG Shu2,ZHOU Xin-jing3   

  1. 1.National Engineering Research Center for Inland Waterway Regulation, Chongqing Jiaotong University, Chongqing 400074, China;
    2.Key Laboratory of Hydraulic and Waterway Engineering of the Ministry of Education, Chongqing Jiaotong University, Chongqing 400074, China;
    3.Chongqing Information and Communication Consulting and Design Institute Co., Ltd.,Chongqing 400041,China
  • Received:2016-12-10 Revised:2017-02-04 Online:2018-06-01 Published:2018-06-16

摘要: 复式断面丁坝是常见的航道整治建筑物。通过室内水槽试验开展非淹没复式断面丁坝流速分布规律研究。结果表明①表层合流速高速区主要出现在一级丁坝坝头下游外侧,二级丁坝长度b2对高速区流速大小及平面分布形态具有明显影响,而弗劳德数Fr只影响高速区流速大小,表层横向流速平面分布接近扇形,最大横流可达试验流速的0.45倍;②横断面上纵向流速高速区位于一级丁坝坝头附近,强横流区位于二级丁坝前缘,均呈带状分布,b2越大,带宽越小,高速区分布更为集中;③纵剖面上纵向流速最大值出现在丁坝下游靠近水面附近,其沿程位置随b2的增大而上移,横向流速呈先增大后减小的变化,最大值出现在丁坝附近靠近槽底的部位,强横流区呈枫叶型分布。研究结果可为航道整治工程设计和丁坝水毁保护等提供参考。

关键词: 非淹没丁坝, 复式断面, 纵向流速, 横向流速, 分布规律

Abstract: Spur dike with compound section is a common structure used in waterway regulation. In this paper, the law of velocity distribution around non-submerged spur dike with compound section is researched via flume experiment, and the results manifest that I) In surface layer, large resultant velocity appears outside the downstream of the first-stage spur dike head; the length (b2) of the second-stage spur has noticeable impact on the value and morphological distribution of the zone of large resultant velocity whereas Froude number (Fr) only affects the value of velocity; transverse surface velocity distributes in an approximated fan shape, with the maximum value up to 0.45 times of test velocity. (II) In cross-sectional scale, large longitudinal velocity is located in the adjacent of the head of the first-stage spur dike, and intense transverse velocity zone is in the front of the second-stage spur dike, both distributing in a band shape; with the increase of b2, the band width declines, and the distribution is more concentrated. (III) In longitudinal profile, the maximum longitudinal velocity is found in the downstream of the spur dike near water surface, and its position moves up along with the increase of b2; while the transverse velocity increases first and then decreases, with its maximum value arising close to the bottom; intense high transverse velocity zone stretches in a maple leaf shape.The research results provide reference for waterway regulation and spur dike protection.

Key words: non-submerged spur dike, compound section, longitudinal velocity, transverse velocity, distribution law

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