Sediment Transport Flashcards

1
Q

The process of eroding sediment from one place, transporting it in the flow and depositing it in another place.

A

Sediment Transport

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2
Q

Occurs when the shear stress applied on
the sediment bed exceeds the critical shear stress

A

Erosion

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3
Q

It takes place when the transport capacity of the flow is exceeded.

A

Deposition

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4
Q

(4) Basic sediment process

A

Resuspension
Transport
Settling
Consolidation & compaction

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5
Q

Sediment process is dependent on

A

1)Flow hydrodynamic conditions
2) Sediment Properties (size, shape, density, composition)

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6
Q

It is most fundamental property
governing the motion of the
sediment particles in water.

A

Particle Settling

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7
Q

Defined as the terminal velocity at which a single particle falls through quiescent water and depends on the particle’s size, shape, and density along with the water’s viscosity and density.

A

Settling Velocity

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8
Q

True/False

For Sediment Transport Modeling, the settling velocity of particles and their resistance to resuspension under shear
stress are the most significant.

A

True

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9
Q

True/False

PARTICLE SETTLING CHARACTERISTICS vary as they respond to hydrodynamic conditions in the water body.

A

True

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10
Q

True/False

Once near the bottom, DEPOSITION governs their removal from the water column.

A

True

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11
Q

2 major mechanisms for sediment transport

A

Currents & Wind waves

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12
Q

True/False

Sediment transport is significantly
influenced by the instability of the near-bed flows.

A

True

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13
Q

True/False

Sediment is moved either only suspended or bed load.

A

False (and/or)

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14
Q

Calculation of total sediment load

A

Suspended load + Bed load

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15
Q

It is the portion of the sediment load that is transported in suspension in the water column which includes:
sediments resuspended from the bed and wash load brought from upstream.

A

Suspended Load

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16
Q

It is used to analyze contaminant transport since contaminants are often attached to and transported by sediments in suspension.

A

Total Suspended Load

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17
Q

It has relatively fine material in near-permanent suspension
that is transported through the system without deposition.

A

Wash Load

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18
Q

It is comprised of particle sizes finer than those found in the
bed.

A

Wash Load

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19
Q

True/False
Cohesive sediments can be transported as suspend load and bed load.

A

False

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20
Q

True/False

Cohesive sediments can be transported as suspended and or bed load.

A

False (only as suspended load)

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21
Q

True/False

Cohesive sediments can be transported as suspended and or bed load.

A

False (only as suspended load)

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22
Q

True/False
Non-cohesive sediment can only be transported as bed load.

A

False (both suspended and bed load)

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23
Q

The 2 mechanism of transporting cohesive as suspend load:

A

Advection
Dispersion

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24
Q

It is a mechanism where the cohesive sediment is carried with the ambient water at the flow velocity.

A

Advection

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25
It is a mechanism of transport where cohesive sediment is moved from an area of high to low sediment concentration.
Dispersion
26
It is a type of load where it is comprised of particles that move on/ near the bead by Saltation, rolling, or slid8ng in the bed layer.
Bed Load
27
True/False The bed load movement occurs intermittently in a thick layer; on or in close contact with the bed.
False (thin)
28
It is a process by which individual sediment grains make isolated or serial jumps along the bed?
Saltation
29
t provides a transition from bed-load transport that takes place immediately above the bed to suspended-load transport that takes place in the overlying water column.
Saltation
30
It is defined as the frictional force per unit of bed area exerted on it by the flowing water.
Shear Stress
31
It is an important factor in the movement of bed material and is a useful parameter in describing sediment transport as well as erosion and deposition.
Shear Stress
32
True/False Shear stress is exerted on the bed when water flows over it, as either steady flow or oscillatory flow under tides and waves.
True
33
True/False Shear stress moves bed particles in a sliding motion downstream.
False (rolling)
34
True/False If the shear stress is greater than the critical shear stress, only a fraction of the suspended material will be deposited.
True (higher shear stress-sediment go up)
35
True/False If the shear stress is less than the critical shear stress, suspended sediment will be deposited on bed gradually.
True
36
(3) bottom shear stress mechanism vary
Temperature Topography Salinity
37
3 Bottom shear stress mechanism vary
Temperature Topography Salinity
38
3 Bottom shear stress mechanism vary
Temperature Topography Salinity
39
4 Sources of sediment transport
Point discharges Land surface runoff Bank erosion Bed scour
40
4 Predominant factors responsible for sediment transport
Currents Winds Inflows Tides (in estuaries and coastal waters)
41
Major Mechanism of sediment transport
Currents & Waves
42
A major mechanism dominant in rivers.
Currents
43
A major mechanism that is dominant in lakes, especially during storm.
Wind wave
44
The two mechanism that is dominant estuaries.
Wind & tidal waves
45
True/False In Steps 1 and 2, the predominant mode of transport is sediment grains moving along the bottom in the form of bed load. Particle movement begins as a sliding or rolling motion.
True
46
True/False In Step 3, some particles also may move above the bed surface through saltation. These movements result in frequent contact of the moving particles with the bed and are transported as bed load.
True
47
In Step 4, particles begin to be suspended and are subject to _______ forces as the flow velocity and shear stress increase. Particles are thrown up into suspension and are transported as suspended load.
turbulent
48
(2) Difficult to separately identify the phase of resuspension and deposition in natural waterbodies
Resuspension & Deposition
49
It determined the critical shear stress for erosion as a function of depth and the erosion rate as a function of both shear stress and depth. (Designed by McNeil)
SEDflume
50
It measures the erosion of sediments at high shear stresses and with sediment depth.
SEDflume
51
It is controlled primarily by BOTTOM SHEAR STRESS and also SITE-SPECIFIC BED PROPERTIES for erosion rates and scour depths.
Sediment Resuspension
52
True/False Sediment on the bed will be eroded and transported when the bottom shear stress EXCEEDS A CRITICAL VALUE.
True
53
[Sediment RESUSPENSION] The Immersed particle weight is the main stabilizing force.
Non-cohesive sediment
54
True/False [Sediment RESUSPENSION] For sediment with bulk density close to the water density, the main forces are interparticle adhesion and organic binding.
True
55
True/False [Sediment RESUSPENSION] Beds are layered with density and shea strength decreasing downward.
False (increasing)
56
True/False Sediments move whenever the shear stress caused by water flow and wind waves REACHES A CRITICAL SHEAR STRESS FOR RESUSPENSION that is EQUAL TO THE SHEAR STRENGTH "HOLDING" the sediment to the bed.
True
57
A process by which suspended sediments LEAVE the water column, either temporarily or permanently, and become part of the bottom sediments.
Sediment Deposition
58
True/False [Sediment DEPOSITION] With non-cohesive sediment, the critical shear stress is only slightly less than that for erosion. Particles settle to the bed almost as soon as the shear stress is too small to erode it.
True
59
True/False [Sediment DEPOSITION] With cohesive sediment, critical shear can be much greater than that for erosion.
False (smaller)
60
It can be estimated as the product of the settling velocity and the probability of deposition on contact with the bed, which is 0 for very turbulent systems and 1 for stagnant ponds.
Deposition Rate
61
True/False For depostion, particles must overcome RESISTANCES due to: Turbulence in the Water Column Thin Viscous Sublayer at the Interface Chemical or Biological Activity at the Bottom
True
62
True/False Probability of deposition depends on: Bottom Shear Stress Suspended Sediment Size Cohesiveness of the Sediment
True
63
True/False Once in SUSPENSION, sediments will settle out at a rate determined by the sediment concentration, the settling velocity, and the turbulence intensity.
True