不同泥沙含量水体光谱特性分析   总被引：1，自引：0，他引：1  

方圣辉  张加晋 《测绘信息与工程》2007,32(6):47-49

研究了不同的观测角度下水体光谱反射率与泥沙含量之间的变化关系,提出了差分泥沙光谱指数建立泥沙反演模型,确立了在不同角度下对水体泥沙含量的定量分析模型.  相似文献   

高浓度悬浮泥沙的声学观测   总被引：13，自引：0，他引：13  

张叔英  钱炳兴 《海洋学报》2003,25(6):54-60

在分析高浓度悬浮泥沙的声衰减机理和进行实验研究的基础上,研制了两种型号的超声波观测仪器(UBD-500/1500超声重度计)用于悬浮泥沙浓度剖面的连续和实时观测,并且已经在长江口航道的浮泥探测、黄河小浪底水库的泥沙观测中得到应用.讨论了测量原理和仪器的设计、标定等问题.这种基于声衰减测量原理的观测仪器的主要优点是标定简便和稳定,含沙量观测范围为10～800kg/m3,标定后的测量误差可达±5%(F.S).  相似文献   

PROCESS-BASED MODEL OF GRAIN LIFTING FROM RIVER BED TO ESTIMATE SUSPENDED-SEDIMENT CONCENTRATION IN A SMALL HEADWATER BASIN     

YOSHIMASA KURASHIGE 《地球表面变化过程与地形》1996,21(12):1163-1173

Suspended sediment is supplied from river bed sediment in Hiyamizusawa Brook, Hokkaido, Japan, during the early snowmelt season. The stirring up of fine grains from the river bed is an important control of the time variation of suspended-sediment flux. In this stream, about 10 per cent of the river bed is covered with sand sediment, 80 per cent with cobbles and/or pebbles and the remaining 10 per cent is exposed bedrock. A model previously used to explain the stirring up of fine grains within a cobble and pebble bed is applied to a sand bed, with the modification that fine grains in a sand bed are assumed to be stirred up from the tractive layer formed on the surface, whereas those in a cobble and pebble bed are assumed to be stirred up from the gaps formed by the selective movement of pebbles on the river bed. The lift force acting at the river bed is estimated from the bed shear stress, and the maximum grain size capable of being stirred up was calculated from the lift force. Consequently, the amount of fine material stirred up from the river bed is estimated from the grain size distribution of river bed sediment, and the suspended-sediment flux is thus calculated. All stirred-up fines are assumed to become suspended sediment. The simulated time variation of suspended-sediment concentration was similar to that obtained in the field study. The calculated grain size of suspended sediment was also equivalent to the field data.  相似文献   

Combined Use of Remote Sensing and Continuous Monitoring to Analyse the Variability of Suspended-Sediment Concentrations in San Francisco Bay, California     

C. A. Ruhl  D. H. Schoellhamer  R. P. Stumpf  C. L. Lindsay 《Estuarine, Coastal and Shelf Science》2001,53(6):801

Analysis of suspended-sediment concentration data in San Francisco Bay is complicated by spatial and temporal variability. In situ optical backscatterance sensors provide continuous suspended-sediment concentration data, but inaccessibility, vandalism, and cost limit the number of potential monitoring stations. Satellite imagery reveals the spatial distribution of surficial-suspended sediment concentrations in the Bay; however, temporal resolution is poor. Analysis of thein situ sensor data in conjunction with the satellite reflectance data shows the effects of physical processes on both the spatial and temporal distribution of suspended sediment in San Francisco Bay. Plumes can be created by large freshwater flows. Zones of high suspended-sediment concentrations in shallow subembayments are associated with wind-wave resuspension and the spring-neap cycle. Filaments of clear and turbid water are caused by different transport processes in deep channels, as opposed to adjacent shallow water. Crown  相似文献   

Numerical Study on Seasonal Transportation of the Suspended Sediments in the Modern Yellow River Mouth Effected by the Artificial Water and Sediment Regulation     

WANG Nan  QIAO Lulu  LI Guangxue  ZHONG Yi  SONG Dehai  DING Dong  GAO Fei  JI Fengying 《中国海洋大学学报(英文版)》2019,(1):20-30

Since 2002, an artificial water and sediment regulation(AWSR) has been carried out, which largely reduced water and sediment discharged from the Yellow River into the Bohai Sea. Although the sediment transport in the Yellow River Mouth(YRM) has been observed and modeled intensively since AWSR, but preferentially for the non-storm conditions. In this study, a three-dimensional current-wave-sediment coupled model, DHI-MIKE numerical model, was used to examine the seasonal suspended-sediment transport in the YRM after the AWSR. Results show that the seasonal distribution of suspended-sediments in the YRM is dominated by wind and wave rather than river input. The major transport pathway of suspended-sediments is from the western Laizhou Bay to the Bohai Strait during the winter monsoon, especially in storm events. In addition, about 66% of the river sediments deposit within 30 km of the YRM, which is smaller than previous estimations. It suggests that the YRM has been eroded in recent decades.  相似文献