长江口北槽抛泥流速和悬沙浓度时空分布观测
Field observations of current and suspended sediment concentration during sediment disposal in the Changjiang (Yangtze) Estuary
-
摘要: 河口泥沙运动有其独特的规律,需要采用高分辨率的观测手段进行系统的现场观测,以此发现河口流速和泥沙分布结构,进而探讨其形成机制,应用声学多普勒流速剖面仪和声学悬浮泥沙观测系统,通过定点和走航式观测长江河口不同潮型和流态下流速和悬浮泥沙浓度时空分布发现:(1)不同潮型出现高浓度“事件”的次数和成因存在差异,中潮型出现高浓度“事件”的可能性最大;(2)抛泥泥沙浓度垂向分布至少有3种结构类型,即上小下大的“L”型、指数型和上大下小的“漂浮”型;(3)受抛泥泥沙输移的影响,断面流场形成低流速区,它们的强度随落潮流的扩散逐渐减弱;(4)不同潮型的落潮流表现出不同的输移行为,大、小潮型落潮流偏北,中潮型落潮流偏南;(5)在落潮流和颗粒重力共同作用下抛泥泥沙同时存在输移扩散和沉降过程,小潮型抛泥泥沙主要就近扩散和沉降,中潮和大潮型抛泥泥沙输移扩散范围较远。Abstract: Acoustic Doppler current profile and acoustics concentration profiler are applied respectively via fixed-point serial and sailing observations to measure temporal and spatial variations of current and suspended sediment concentration at the North Passage in the Changjiang (Yangtze) Estuary.Field observations show that(1) near-bed high concentration events occur in various tides,with different frequencies and formation mechanisms.They take place frequently in a moderate tide,especially at the slack or maximum tides.(2) At least three types of vertical profiles of suspended sediment concentration are found out,that is,L-type with the upper concentration smaller and the lower larger,exponential type,and floating type with the upper concentration larger and the lower smaller.(3) low-velocity zones occur owing to the effect of dredged sediment disposal on the flow,which are located at the surface column or through the whole column,for the latter case,forming flow fronts.The intensity of the zones tends to decrease with the diffusion and settling of the disposal sediment.(4) The behavior of ebb currents differs at various tidal phases.The ebb currents are directed mainly to the north in the spring and neap tides,while they are directed mainly to the south in the moderate tide.(5) Both sediment transport diffusion and settling coexist during dredged sediment disposal,under the combined action of ebb current and gravity.Disposal sediment deposit is immediate in the neap tides,and it disperses far away in the moderate and spring tides.
-
倪晋仁,王光谦,张红武.固液两相流基本理论及其最新应用[M].北京:科学出版社,1991. NI Jin-ren,WANG Guang-qian.Vertical sediment distribution [J].J Hydraulic Eng,ASCE,1991,117(9):1 184-1 194. 杨美卿.河流与海岸动力学引论[M].北京:水利水电出版社,1993. 黄胜,卢启苗.河口动力学[M].北京:水利水电出版社,1995. FAAS R W.Time and density-dependent properties of fluid mud suspensions,NE Brazilian continental shelf [J].Geo-Mar Lett,1984,4:147-152. ODD N V M,BENTLEY M A,WATERS C B.Observations and analysis of the movement of fluid mud in estuaries [A].MEHTA A J.Nearshore and Estuarine Cohesive Sediment Transport:Coastal and Estuarine Studies:Vol.42[C].Washington:AGU,1993.430-446. WREN D G,BARKDOLL B D,KUHNLE R A,et al.Field techniques for suspended-sediment measurement [J].J Hydr Eng,2000,126(2):97-104. 张叔英,李允武.声学悬浮泥沙观测系统的研制和应用[J].海洋学报,1998,20(5):114-119. 张叔英,李允武.悬浮泥沙声学观测的原理分析[J].声学学报,1999,24(3):269-274. 郭纪捷,任来法,李允武.声学悬浮泥沙观测数据现场定标研究[J].海洋学报,1998,20(5):120-125. SHI Zhong,REN Lai-fa,LIN Hong-lie.Vertical suspension profile in the Changjiang Estuary [J].Mar Geol,1996,130:29-37. SHI Zhong,REN Lai-fa,Zhang Shu-ying,et al.Acoustic imaging of cohesive sediment resuspension and re-entrainment in the Changjiang Estuary,East China Sea [J].Geo-Mar Lett,1997,17:162-168. SHI Zhong,REN Lai-fa,HAMILTON L J.Acoustic profiling of fine suspension concentration in the Changjiang Estuary [J].Estuaries,1999,23(3A):648-656. HAMILTON L J,SHI Zhong,ZHANG Shu-ying.Acoustic backscatter measurement of estuarine suspended cohesive sediment concentration profiles [J].J Coast Res,1998,14(4):1 213-1 224. URICK R J.Principles of Underwater Sound [M].New York:McGraw-Hill Book Co,1983.
计量
- 文章访问数: 748
- HTML全文浏览量: 10
- PDF下载量: 953
- 被引次数: 0