剪切流作用下浮泥层悬扬速率计算方法综述
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  • 英文篇名:Review on calculation methods for the entrainment rate of fluid mud
  • 作者:郁李丽 ; 许春阳 ; 陈永平 ; 高翔宇
  • 英文作者:YU Li-li;XU Chun-yang;CHEN Yong-ping;GAO Xiang-yu;Jiangsu Key Laboratory of Coast Ocean Resources Development and Environment Security;College of Harbor,Coastal and Offshore engineering,Hohai University;State Key Laboratory of Estuarine and Coastal Research,East China Normal University;Nanjing Hydraulic Research Institute;
  • 关键词:浮泥层 ; 剪切流 ; 悬扬速率 ; 紊动动能平衡方程 ; Richardson数
  • 英文关键词:fluid mud layer;;shear flow;;entrainment rate;;balance equation for TKE;;Richardson number
  • 中文刊名:NSYJ
  • 英文刊名:Journal of Sediment Research
  • 机构:江苏省海岸海洋资源开发与环境安全重点实验室;河海大学港口海岸与近海工程学院;华东师范大学河口海岸学国家重点实验室;南京水利科学研究院;
  • 出版日期:2019-03-29 15:39
  • 出版单位:泥沙研究
  • 年:2019
  • 期:v.44
  • 基金:河口海岸学国家重点实验室开放基金资助项目(SKLEC-KF201711);; 国家重点研发计划课题(2017YFC0405401);; 国家自然科学基金青年项目(51709084);; 中国博士后科学基金资助项目(2017M620187);; 江苏省海洋资源开发与环境安全重点实验室基金资助项目(JSCE201702);; 港口航道泥沙工程交通部重点实验室资助项目
  • 语种:中文;
  • 页:NSYJ201902008
  • 页数:8
  • CN:02
  • ISSN:11-2532/TV
  • 分类号:58-65
摘要
浮泥的悬扬速率是反映其悬扬特性的重要指标,针对剪切水流作用下浮泥的悬扬过程,总结了表征悬扬强度的临界水动力指标,如悬扬流速、临界水流剪切力等;并进一步阐述了反映变化过程的悬扬通量计算模式,包括根据TKE方程建立悬扬模型,及基于Richardson数推算无量纲悬扬速率E,在此基础上分析了黏性、屈服应力、悬沙沉降、边壁阻力等因素对悬扬速率的影响。更深入的研究可从絮凝作用、盐度、生物扰动等多因素耦合影响或界面波的发展规律等问题展开,以期提高悬扬模型的计算精度。
        The entrainment rate of fluid mud is one of the key variables describing the entrainment process. The critical hydraulic parameters describing the entrainment rate by critical entrainment velocity and critical shear stress are reviewed. Calculation methods of the process-oriented entrainment flux are elaborated, for example, using the balance equation for turbulent kinetic energy(TKE) of the upper layer to model this entrainment process or to calculate the non-dimensional entrainment rate E with Richardson number. On this basis, the influences of factors such as viscosity, Bingham yield stress, settling velocities of suspended sediment particles and the side wall friction, are further illustrated. To improve the accuracy of existing entrainment models, further study can be conducted on the coupling effects of different factors such as the flocculation, salinity and bioturbation or to understand the evolution of interfacial waves.
引文
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