Watershed assessment Flashcards

1
Q

What were some of the findings from Ah’ ta’ ape creek?

A
  • channel aggradation
  • avulsions
  • infilling
  • widening of channel
  • subsurface flow in lower reaches
  • movement of some log jam complexes
  • loss of spawning and rearing habitat
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2
Q

What overarching controls influence channel equilibrium

A
  • local geology (bedrock control)
  • geomorphic/glacial history
  • climate, riparian vegetation and land use
  • geology
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3
Q

watershed

A

-topographic high points where all same water will collect

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4
Q

To understand channels you need to look at?

A
  • land use
  • disturbances
  • sediment
  • slope and grain size
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5
Q

What characteristics influence the amount and rate at which excess rainfall or snowmelt will be delivered to a channel?

A

topographic and physiographic characteristics

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6
Q

small watershed

A

<250 km2
dominant land phase and overland flow
highly sensitive to high intensity short rainfalls

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7
Q

large water shed

A

> 2500km2
well developed channel networks and phases, channel storage
less sensitive to high intensity short rainfalls

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8
Q

what does the gradient say about the channel

A

-steeper, higher bed load, vertical erosion
-less steep, medium to one bed load, lateral erosion wider channel
lower slope more meanders

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9
Q

What is hydraulic geometry?

A

rivers always trying to achieve equilibrium- all of the water and some/all of the sediment
Q=wxdxv
sediment supply=sediment transport

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10
Q

What will rivers adjust to get sediment supply and transport at equilibrium?

A
  • width
  • depth
  • slope
  • grain size
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11
Q

Why is it important to understand sediment in river channels?

A
  • power of stream (greater slope, greater grain size)

- variability of habitat (greater variability the better)

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12
Q

If sediment caliber (grain size- silt to boulders) increases what happens with channel stability and the channel gradient?

A

the channel stability will decrease and the

channel gradient will increase

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13
Q

what happens to channel stability when sediment supply increases?

A

channel stability decreases with sediment supply

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14
Q

What does the number of channels say about the stability?

A

the higher number of channels the more unstable it is

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15
Q

list a few multiple channels

A
  • wandering
  • anastomosed
  • braided
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16
Q

list a couple single channels

A
  • straight

- meandering

17
Q

Channel morphology is based on

A
  • slope
  • sediment supply
  • stability
18
Q

In a single channel stability increases with?

A

sinuosity

19
Q

what happens when sediment supply is higher than transport

A
too high for streams capacity
unpredictable
river is laterally active
bank erosion occurs during blowout events (floods)
avulsion occurs
20
Q

What is more stable a straight or meandering channel?

A

meander because higher sinuosity=high stability

21
Q

What happens when sediment supply increases but water discharge is the same?

A

aggradation, widening of the channel and higher instability

22
Q

what happens when sediment supply stays the same but water discharge increases?

A

narrowing and down cutting of the channel

23
Q

what happens when sediment supply stays the same but water discharge decreases?

A

aggradation, narrower channel, instability

24
Q

What components can we look at to determine the stability of a channel

A
  • w:d:slope
  • sediment supply
  • local geology
  • geomorphic history
  • climate, riparian zone, land use
  • number of channels
  • sinuousity