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中层温差反坡异重流运动特性试验研究
引用本文:纪道斌,曹巧丽,谢涛,尹卫平,黄钰铃,刘德富.中层温差反坡异重流运动特性试验研究[J].长江科学院院报,2013,30(4):34-39.
作者姓名:纪道斌  曹巧丽  谢涛  尹卫平  黄钰铃  刘德富
作者单位:1.三峡大学 a.水利与环境学院; b.三峡库区生态环境教育部工程研究中心湖北 宜昌 443002; 2.贵州省水利水电勘测设计研究院, 贵阳 550000; 3.湖北工业大学 资源与环境学院,武汉 430000
基金项目:国家自然科学基金面上项目(51179095, 51179205);国家自然科学基金青年基金项目(51009080,51009081,51209123)资助
摘    要:以三峡水库支流库湾长期普遍存在的中层倒灌异重流为背景,构建室内物理模型,以入流量、初始水位、温度差3个主要影响因子,设计系列工况对中层反坡异重流运行特性进行模拟试验研究,分析异重流头部移动速度、交界面高度、头部厚度等主要水力学要素的变化过程及受入流量、初始水位、温度差的影响规律。借助钱宁等有关异重流的头部速度理论公式,计算了各种工况下的中层异重流头部理论速度,对比实际头部速度的实测值与理论值,两者相差不大,相对误差均小于5%。

关 键 词:温差  中层  反坡异重流  试验  
收稿时间:2012-12-18
修稿时间:2013-04-09

Motion Characteristics of Mid-layer Adverse Slope Density Current
JI Dao-bin , CAO Qiao-li , XIE Tao , YIN Wei-ping , HUANG Yu-ling , LIU De-fu.Motion Characteristics of Mid-layer Adverse Slope Density Current[J].Journal of Yangtze River Scientific Research Institute,2013,30(4):34-39.
Authors:JI Dao-bin  CAO Qiao-li  XIE Tao  YIN Wei-ping  HUANG Yu-ling  LIU De-fu
Affiliation:1.College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China; 2.Engineering Research Center under Ministry of Education on Eco-environment in Three Gorges Reservoir Region, China Three Gorges University, Yichang 443002, China; 3.Guizhou Survey & Design Research Institute for Water Resources and Hydropower, Guiyang 550000, China; 4.College of Resources and Environment Sciences, Hubei University of Technology, Wuhan 430000, China
Abstract:With the widespread long-term mid-layer intrusion density flow in the tributary bays of Three Gorges Reservoir as a research background, an indoor physical model was built. Three main factors inflow rate, initial water level, and temperature difference were chosen to design various conditions to simulate and investigate the motion characteristics of adverse slope density current in the mid-layer. The variations of hydraulic elements of the density current such as head moving velocity, interface height and head thickness influenced by inflow rate, initial water level, and temperature difference were analyzed. With Channing’s theoretical formulas, the head velocities of mid-layer density current in different conditions were calculated and compared with the measured values. It was found that the difference between the two was not large, and the relative error was less than 5%.
Keywords:temperature difference  mid-layer  adverse slope density flow  test
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