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作 者:王骁 罗红春 冀鸿兰[1] 李扒拴 WANG Xiao;LUO Hongchun;JI Honglan;LI Bashuan(College of Water Conservancy and Civil Engineering,Inner Mongolia Agricultural University,Hohhot 010018,China;Hohhot Togtoh County Rural Revitalization Coordinated Development Center,Togtoh 010200,China)
机构地区:[1]内蒙古农业大学水利与土木建筑工程学院,内蒙古呼和浩特010018 [2]呼和浩特市托县乡村振兴统筹发展中心,内蒙古托克托010200
出 处:《水利水电科技进展》2023年第4期31-36,51,共7页Advances in Science and Technology of Water Resources
基 金:国家自然科学基金项目(51969020,52169017);2018自治区应用技术研究与开发资金项目(201802104)。
摘 要:为分析弯道冰下水流结构与环流分布特征,利用声学多普勒流速剖面仪(ADCP)对什四份子弯道的冰下流场进行了测量,通过测量弯道的冰厚、水深、流速,分析了弯道断面冰情与冰下环流分布情况。结果表明:弯道冰下水流并不完全呈现双螺旋结构,冰封期环流集中在弯顶凹岸侧和弯顶后凸岸侧,易产生在相邻冰塞之间或是冰塞与河岸之间;环流区域环流旋度沿水深线性增大,非环流区域环流旋度则线性减小,同一位置的不同流层环流旋度大小分布基本一致,弯道后半段大于前半段,弯顶前凹岸侧大于凸岸侧,最大环流旋度位于弯顶凹岸侧,约为0.91。In order to analyze the subglacial flow structure and circulation distribution characteristics in a river bend,the flow field in the Shisifenzi bend was measured using acoustic Doppler current profiler(ADCP).By measuring the ice thickness,water depth and velocity of the bend,the ice condition and the distribution of the subglacial circulation in the bend section were analyzed.The results show that the flow under the ice in the bend does not completely present a double helix structure.During the freezing period,the circulation is concentrated on the concave side of the bend top and the convex side of the bend top,which is easy to occur between adjacent ice jams or between ice jams and river banks.The circulation curl in the circumfluence region increases linearly along the water depth,while the circulation curl in the non-circulation region decreases linearly.The distribution of circulation curl in different flow layers at the same position is basically the same.The circulation curl in the second half of the bend is larger than the first half and its value in the concave bank side is larger than the convex bank side,with the maximum circulation curl value of about 0.91 located in the concave bank side of the bend.
分 类 号:TV133[水利工程—水力学及河流动力学]
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