Sediment and Sedimentation Flashcards

1
Q

It is a naturally occurring material that is broken down by processed of weathering and erosion and is subsequently transported by the action of wind, water, or ice and/or by the force of gravity acting on the particle itself

A

Sediment

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2
Q

Sources of sedimentation

A

Land clearing
Unsealed roads
In-stream disturbance
Agricultural activity
Mining
Other activities

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3
Q

Characteristics of sediments (A. Particle classes)

A

Primarily clay, primarily silt, small aggregate, large aggregate, primary sand

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4
Q

Characteristics of sediments (B. At detachment)

A

Distribution of classes function of texture
Diameter of small and large aggregates function of texture

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5
Q

Characteristics of sediments (C. After deposition)

A

Sediment enriched in fines

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6
Q

Flowing water transports sediments as:

A

Bedload
Suspended load
Wash load
Bed material load

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7
Q

grains rolling, sliding, and/or saltating in frequent or continuous contact with bed

A

bedload

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8
Q

it is the transport of sediments by hopping and bouncing along the channel bed

A

saltation

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9
Q

grains in suspension above the bed for extended periods of time

A

suspended load

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10
Q

that part of the suspended load that is not found in the bed

A

wash load

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11
Q

the fine fraction which is mostly in suspension

A

wash load

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12
Q

the coarse fraction normally found in the bed

A

bed material load

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13
Q

concentration of sediments in a stream ____ with distance up from the bed

A

decreases

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14
Q

at any given point, the upward flow of water will have _____ than the downward flow

A

higher sediment concentration

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15
Q

Under steady state condition, the rate of sediment upward flow due to turbulent diffusion is ______ to the downward flow rate due to the ________

A

equal, settling action of gravity

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16
Q

the common methods of estimating the sediment discharges of rivers include:

A
  1. Actual monitoring of the sediment load through sediment sampling
  2. Using sediment discharge formulas
  3. Other sampling technique
17
Q

can be depth-integrated or point sampling (taken at fixed depth from the river bottom)

A

sediment sampling

18
Q

ratio of the dry weight of sediment to total weight of the sample, expressed in parts per million or mg per liter

A

sediment concentration

19
Q

also used to estimate the sediment loads on days when no measurements are available

A

rating curve (relating suspended-sediment discharge and water discharge)

20
Q

what is the formula in getting sediment discharge per unit channel

A

see pdf for details

21
Q

formula in getting the velocity at any depth

A

see pdf for details

22
Q

sediment discharge formulas

A

Meyer-Peter
Schoklitsch
Shields
duBoys
Einstein-Brown
Kalinske

23
Q

the sediment carrying capacity of a stream is proportional to the water discharge raised to a certain power

24
Q

the rate at which the capacity of a reservoir is reduced by sedimentation depends on:

A

*the quantity of sediment flow
*the percentage of this inflow trapped in the reservoir
*the density of the deposited sediment

25
the volume occupied by the sediment in the reservoir will depend on:
the specific weight of the deposited material
26
the exceptionally high sedimentation rate in the mountainous Agno RIver Watershed in the country has affected dam operations on the Ambuklao and Binga reservoirs
share ko lang
27
give up na di lagi ka kapasar
charot