Examples of 'sediment transport' in a sentence
Meaning of "sediment transport"
Sediment transport refers to the movement and displacement of sediments, such as sand, silt, and gravel, by natural agents like water, wind, or ice. It is an important process in shaping landscapes, river systems, and coastal areas
How to use "sediment transport" in a sentence
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sediment transport
The movement of sediment is called sediment transport.
Sediment transport can be influenced by hydraulic engineering measures.
Measurement of coastal erosion and sediment transport.
Study of sediment transport hydraulics and fluvial morphology.
Beach profile and sediment transport are.
Sediment transport taking accounting for the organic matter.
River bed altered by sediment transport at a later time.
Debouching can generate massive amounts of sediment transport.
Unit stream power for sediment transport in natural rivers.
The trench itself serves as an axis of sediment transport.
Control of sediment transport due to erosion from peat mines.
Ocean circulation and sediment transport.
O fine sediment transport mechanisms.
The influence of morphology is predominant in the dynamic of sediment transport.
Hydrodynamics and sediment transport in the.
See also
The sediment transport implementation is focused only on fine cohesive sediments.
The mound evolution is calculated using sediment transport models.
Results of sediment transport formulas have a dispersion of one order of magnitude.
Determine watershed dynamics that govern erosion and sediment transport.
Various coefficients in sediment transport models must be accounted for.
Sediment transport models.
Dams in particular have upset patterns of sediment transport and deposition.
Only the sediment transport caused by the tidal bore is discussed.
The modification accounts for the influence of waves on sediment transport.
Modeling of sediment transport in such varied morphology faces different problems.
Scour can occur even if there is no actual sediment transport in the watercourse.
Overview of sediment transport evaluation and monitoring in the nile basin.
Underlying processes were then investigated using a numerical model for sediment transport.
All sediment transport models are highly dependent on the forcing hydrodynamics.
Possible changes in patterns of sediment transport and settlement along the coastline.
The sediment transport in lakes is very important and has a broad scope.
These results could help in improving numerical models of natural sediment transport.
Direct measurements of sediment transport are impossible to implement under these extreme hydrodynamic conditions.
The model integrates multiple components for the sediment transport computation.
Wetlands also regulate sediment transport thereby contributing to land formation and coastal zone stability.
Rock armour to stabilize slope and prevent continued erosion and sediment transport.
Plenty of confluences and fronts bars changes sediment transport and local conditions connections.
Erosion and sediment transport mechanisms in drained peatland forest catchments after ditch network maintenance.
It is shown that this asymmetry contributes to the sediment transport in two different ways.
Sediment transport over the tiled plot was normalized against transport over the bare plot.
Diagnosis of the coastal protection structures and sediment transport caused by marine currents.
SPH for sediment transport and morphological dynamics.
Some processes from hydrology are demonstrated in the subsections of sediment transport and seepage flow.
This will characterize the local sediment transport process occurring during the passage of a tidal bore.
Dams altered the river hydrodynamics and the process of sediment transport and deposition.
The sediment transport model Sedtrans.
O Modelling and measurement of cohesive sediment transport processes in aquatic ecosystems.
Conclusions The evidence supports the impact hypothesis that there is no sediment transport.
These waves are causing a large sediment transport along the coastline from west to east.
Clay mineralogy variations in the Gulf of Guinea and implications for sediment transport dynamics.
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