Size and settling velocities of cohesive flocs and suspended sediment aggregates in a trailing suction hopper dredge plume
نویسندگان
چکیده
A field experiment was conducted to quantify settling velocities, aggregate states, and flocculation within a hopper dredge plume. Particular interest was in determining the abundance of dense, bed aggregates suspended from the consolidated bed during dredging. A suspended sediment plume from the hopper dredge Essayons was sampled for a period of 90 min after dredging. Settling velocities and suspended particle sizes were quantified through sampling with the Particle Imaging Camera System (PICS) and automated image processing routines. The sediment plume was identified and a profiling instrumentation frame was positioned within the plume using Acoustic Doppler Current Profiler (ADCP) backscatter. Results indicated that suspended bed aggregates (defined by densities of 1200–1800 kg m ) represented 0.2–0.5 of total suspended mass, and flocs (densitieso1200 kg m ) represented 0.5–0.8 of total suspended mass. The peak diameter of bed aggregates and flocs occurred near 90 and 200 mm, respectively, corresponding to peak settling velocities of about 1 mm s 1 in each case. Floc settling velocities increased with particle size d, while bed aggregate settling velocity increased like d. Published by Elsevier Ltd.
منابع مشابه
Erosion Due to High Flow Velocities: a Description of Relevant Processes
Convential models for the erosion of non-cohesive sediments overestimate the erosion rate induced by high flow velocities. These high flow velocities occur, for instance, in breaching of embankments or dunes (flow velocities up to 10 m/s) or in jetting sand with a trailing suction hopper dredger (30 to 60 m/s). At these very large flow velocities the erosion process is significantly influenced ...
متن کاملRapid sediment removal from the Columbia River plume near field
We compute rates of sediment removal from the Columbia River, USA plume near field using a control volume technique. By using data from repeated transect passes along the plume axis, we account for variations in plume width, depth, and velocity, and we construct a framework for determining the dominant terms in the complete sediment balance. The contribution due to turbulent sediment flux is es...
متن کاملSediment transport by liquid surficial flow: Application to Titan
Sediment transport by surficial flow likely occurs on Titan. Titan is thought to have a volatile cycle, such as on Earth and likely in the past on Mars, which would entail surficial liquid flow. And surficial flow is implied in interpretations of Cassini–Hyugens data as showing fluvial channels, which would require sediment transport by surficial flow to form the observable features. We present...
متن کاملWave Glider Monitoring of Sediment Transport and Dredge Plumes in a Shallow Marine Sandbank Environment
As human pressure on the marine environment increases, safeguarding healthy and productive seas increasingly necessitates integrated, time- and cost-effective environmental monitoring. Employment of a Wave Glider proved very useful for the study of sediment transport in a shallow sandbank area in the Belgian part of the North Sea. During 22 days, data on surface and water-column currents and tu...
متن کاملStochastic Flocculation Model for Cohesive Sediment Suspended in Water
Existing flocculation models for cohesive sediments are classified into two groups: population balance equation models (PBE) and floc growth models. An FGM ensures mass conservation in a closed system. However, an FGM determines only the average size of flocs, whereas a PBE has the capability to calculate a size distribution of flocs. A new stochastic approach to model the flocculation process ...
متن کامل