Ch. 10. - Rivers and Flooding Flashcards

(31 cards)

1
Q

What is a drainage basin?

A

Areas of land that drain all streams/rainfall to a common outlet (reservoir, point in stream, bay) divided from neighbouring basins by ridges and highlands, major drainage basins consist of many small drainage basins

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2
Q

How does a typical drainage basin vary from its highest point to its lowest point?

A

Many small channels and steep slope at the highest point and one large channel, shallow gradient at its lowest point.

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3
Q

What factors natural and human, affect how quickly water will or will not collect in a drainage basin?

A
  1. Permeability of ground - forested vs concrete - infiltration
  2. artificial/natural drainage
  3. rock type
  4. slope steepness
  5. level of urbanization
  6. presence/absence of vegetation
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4
Q

How does a river erode, transport and deposit sediment?

A
  1. Weathering creates sediments
  2. Erosion in a river occurs because of the impact of other moving sediment and hydraulic lift.
  3. Transport a) solution b) suspension c)Saltation (bounces) d) traction
  4. Deposition occurs when water velocity drops. Solution deposition occurs with precipitation
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5
Q

When does a river erode, transport and deposit most of its sediment load?

A

During the rare occasions of high discharge erosion and transport will occur and as water velocity drops deposition occurs

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6
Q

There are two common types of rivers: 1) braided; and 2) meandering. What are some of the key differences between braided and meandering rivers?

A
  1. Number of channels - Braided has more than 1, Meandering has 1
  2. Size of channels - Braided are smaller, Meandering are larger
  3. Channel shape - Braided higher width/depth ratio, Meandering lower width/depth ratio.
  4. Sediment load - Braided coarse, poorly sorted, moving as bed load, Meandering fine, well sorted, moving in suspension
  5. Discharge - Braided variable, Meandering uniform
  6. Gradient - Braided steep, Meandering shallow
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7
Q

What is discharge?

A

The volume of water moving in a river in a certain amount of time.

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8
Q

What is bankfull discharge?

A

The maximum amount of water in the channel

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9
Q

What is dominant discharge?

A

The volume of water in the channel that does the most work. Work is measured by the amount of sediment that is moved. Dominant discharge is often the bankfull discharge

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10
Q

What is base level flow?

A

The minimum amount of moving water in a channel

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11
Q

What is a flood?

A

A flood is an event when there is more discharge than the channel can accommodate. The extra water leaves the channel and goes on to the flood plain.

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12
Q

What is a floodplain?

A

A floodplain is the area of land next to the river channel

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13
Q

What is the purpose of a floodplain? (there are two)

A

The purpose of a floodplain is to store excess water temporarily and sediment longer term

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14
Q

How often do rivers flood?

A

River rarely flood. They only flood during/after a large precipitation event

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15
Q

Based on the results of question 4, which river, braided or meandering is most likely to produce a catastrophic flood and why?

A

Both rivers are capable of creating a catastrophic flooding event. A flood in a braided river may be more violent (faster water) in will be shorter in duration. A flood in a meandering system may be less violent (slower water) but last longer. Also a flood in a braided system will arrive sooner where as in a meandering system it may arriver later after the precipitation event.

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16
Q

Compare and contrast the behaviour of a braided river when it floods with that of a meandering river when it floods?

A

Flooding in a braided system: the excess water of a flood will enter the channel very soon after the rain fall event. Discharge will increase quickly and reach a maximum value quickly. Just as quickly discharge will drop as this excess water passes through the river. Potentially a lot of sediment will be moved. Braided rivers usually lack a flood plain so water and sediment continue to move during a flood.
Flooding in a meandering river: excess water from precipitation will enter the system more slowly. This means that discharge will increase starting later after precipitation reach a lower maximum value over a longer period of time and then decrease slowing over time. In a meandering river less sediment may be removed from the system. More might be deposited or simply moved within the system.

17
Q

Explain the effects that frozen ground has on flooding?

A

During the winter most rivers in Canada are frozen over. They behave like a pipe in that the water moving in them is confined to a fixed channel size.

18
Q

Explain the effects that saturated ground has on flooding?

A

When the ground is saturated with water, any extra water will remain on the surface. As a result it will travel quicker into the river contributing to a more rapid increase in discharge.

19
Q

What is a hydrograph?

A

A hydrograph is a way to compare changes in river discharge over time.

20
Q

How does the crest of a flood behave over time?

A

The crest of a flood is the highest expected point that water will go. A flood will crest - reach its highest point soon after a precipitation event then decrease back to normal levels in the following days.

21
Q

Explain the difference between a rural flood hydrograph and an urban flood hydrograph?

A

An urban setting is less permeable. In an urban setting there are many land surfaces that prevent water from infiltrating into the ground. In addition there is artificial drainage (sewers) that will channel water quickly into a river. These both contribute to sudden increases and decreases in discharge.

In a rural setting there are a lot of permeable surfaces (fields, forests) that allow water to infiltrate into the ground. There is also little or no artificial drainage that will move water quickly. There is also lots of vegetation which can slower water down.

22
Q

Explain the unique circumstances surrounding the behaviour of a north flowing river in the northern hemisphere when it floods. Give an example.

A

In Canada many rivers flow north. As they flow north the landscape changes; permafrost is encountered. Permafrost makes the ground impermeable. Precipitation is therefore quickly channeled into the river adding to a faster increase in discharge. Also if there is flooding this excess water will remain on the surface making the flood worse. During the winter most rivers in Canada are frozen over. They behave like a pipe in that the water moving in them is confined to a fixed channel size. In spring north flowing rivers in Canada thaw first in the south. Here the extra water from snow melt eventually flows into a channel to the North that is still sealed with ice. Here water velocity increases. At the same time water pressure under the ice increases eventually causing the ice to break, sometimes suddenly and violently.

23
Q

Describe in detail three flood control measures in common use. Be sure to explain what they are, what they are intended to do and the impact they often have on a river system.

A
  1. Artificial Levees - Raised banks of the river channel intended to increase the size of the channel and keep what in it.
  2. Artificial Channels - Extra river channels made to accommodate excess water and keep it moving.
  3. Flood Plains - The large areas of land next to the active channel intended to store water temporarily.

All three of these control measure may alter the river system by either changing the size or shape of the channel, the number of channels, or the nature of the whole system including the flood plain.

24
Q

What is a levee?

A

A bank or a levee is a the raised portion of the flood plain next to the channel.

25
What are the three ways that water can escape a river channel during a flood?
1. Over the top the bank (levee). Once the bank full discharge is reached and exceeded water spills out of the channel over top of the bank. 2. Through the bank. Water exits the channel through a breech in the bank. 3. Underneath the bank as groundwater. Water exits the channel as ground water because of the weight of the higher water in the channel pushing outward
26
What is avulsion and what type of landform does it create?
When flood water leaves the channel through a break in the bank it is called an avulsion. The deposit that's created by an avulsion is a crevasse-splay. This is a fan shaped deposit that is thicker and courser near the breach changing to thinner and finer away from the channel.
27
What is channelization?
The modification of a natural river channel so as to control the flow of water in it. This may include straightening the channel. Channelization can also mean changing the banks and bottom of a channel.
28
What affect does channelization have on stream flow?
Straightening a channel will make it shorter, straighter, steeper and the flow of water will be faster. Adding a concrete liner will create a rigid, fixed channel separator from the surrounding ground. Ground water cannot enter the channel nor can river water leave as groundwater.
29
What affects do fire, logging and animal grazing have on stream behaviour?
Fire, logging and agriculture alter vegetation. Most often this means vegetation is removed. Once vegetation is gone, there is nothing to intercept precipitation and nothing to keep this water from rapidly collecting on and moving across the land surface. More surface water means more sediment that eventually reaches the river channel. A larger sediment load in a river can alter the river system .
30
What affects does streamed sand and gravel mining have on the behaviour of the stream?
Sediment sand and gravel mining of a river bed changes the size and shape of the channel and the flow condition in it.
31
What effect does stream flow have on a concrete pillar that has been placed in a river channel?
At (A) as water moves around the concrete pillar in the river, turbulence increases and water velocity drops on the levee side or down current side. At (B) water velocity increases as it accelerates around the post. The end result is scouring (erosion) of sediment away from the front of the position and deposition of a pile of sediment behind it.