Chapter 13 Flashcards

mid-term review

1
Q

Where does channel flow come from?

A

from direct
precip, overland flow, soil
throughflow, or seepage from
groundwater.

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2
Q

What is energy?

A

the fundamental motive force

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3
Q

How much energy is used overcoming
frictional drag of the channel margin? What is it converted to? What is a major component of kinetic energy?

A

More than 95% of energy is used overcoming
frictional drag of the channel margin. Converted
to heat and lost to surroundings
* Velocity is a major component of kinetic energy
and is closely related to discharge

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4
Q

influent channel

A

above the water table: losing water (can be dry during a dry season if it is feeding groundwater and is being fed only by precipitation)

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5
Q

effluent channel

A

below the water table: gaining water (gaining water from groundwater)

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6
Q

What does a hydrograph show?

A

-direct and indirect runoff; rising limb, recession curve

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7
Q

How does impervious surfaces affect the hydrograph?

A

-additional impervious surface shortens the time and raises the peak

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8
Q

Why does lag time occur

A

-lag occurs because it takes time for infiltration to occur before water begins to peak

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9
Q

the larger the drainage area the ___

A

larger the discharge

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10
Q

Channel dynamics

A

-resistance to flow is not only at the channel boundary but also within the fluid mass itself
-laminar flow: parallel flow lines
-turbulent flow: water travels obliquely to the general direction of flow (well mixed, more activity is going on and particles are changing more often, tends to move water faster (due to increased velocity, faster dissipation of energy than laminar flow) ; higher velocity = turbulent flow

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11
Q

laminar flow

A

the property of fluid particles in fluid dynamics to follow smooth paths in layers, with each layer moving smoothly past the adjacent layers with little or no mixing

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12
Q

turbulent flow

A

-turbulent flow: water travels obliquely to the general direction of flow (well mixed, more activity is going on and particles are changing more often, tends to move water faster (due to increased velocity, faster dissipation of energy than laminar flow) ; higher velocity = turbulent flow

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13
Q

hydraulic radius

A

-measure of channel efficiency
Amount of water in contact with channel cross section
-amount of water in contact with channel cross section
-Higher hydraulic radius means more efficient channel
-R= A/2d+w

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14
Q

a wide shallow channel is ___ than a compact one

A

-a wide, shallow channel is less efficient than a more compact one

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15
Q

How can the flow of fluid in an open channel be expressed?

A

Flow of fluid in an open channel can be
expressed as a balance between the impelling
forces and resisting forces
-Manning equation
-velocity is function of channel roughness (n), hydraulic radius (R), and slow (s)
-n varies from 0.03 to 0.10 in natural streams
-easier to measure it today

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16
Q

Stream power

A

-rate at which energy is expended
-increased mass and velocity of water result in greater capacity for work
-stream power is rate at which energy is expended
-most work is carried out at times of high discharge

17
Q

How can material in the channel be carried? (3 ways)

A

bed load: rolling along the channel floor
-suspended load: carried in suspension in the water (floating down the stream)
-solution load: minerals dissolved in the water (could be salts dissolved or oxygen dissolved in the water)

18
Q

At higher discharge: sediment concentration is __ and solute concentration is __

A

-sediment concentration is higher (figure a)
-solute concentration is lower (figure b)

19
Q

Stream power and critical power threshold

A

-power is greatest at higher gradients
-Downcutting: stream power > critical power
-lateral erosion
-alluviation: stream power < critical power

20
Q

alluviation

A

the process by which deposits of clay, silt, sand, or gravel occur in rivers, estuaries, or along shores of lakes or seas where velocity decreases
-process of depositing sediment

21
Q

Discharge equation

A

Discharge (Q) = wdv (m3 sāˆ’1 where Channel width (w)
* Channel depth (d)
Velocity of flow (V) (m sāˆ’1

22
Q

channel form changes

A

change in channel form that increases hydraulic radius makes discharge more efficient
-energy dissipation of stream: how energy in the streams is moving from faster waters to slower moving waters