Rivers, Floods and Management Flashcards

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1
Q

Drainage basin inputs?

A

Precipitation - rain, hail, snow, frost, dew

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2
Q

Drainage basin storage’s? Give 3?

A

Interception - when precipitation lands on vegetation, buildings or concrete before reaching the soil. This is only temporary because the water evaporates quickly.

Vegetation storage - Water taken up by plants.

Surface storage - Water in puddles, ponds, lakes.

Groundwater storage - Water stored in the ground in soil or rocks. The water table is the top surface of the zone of saturation.

Channel storage - The water held in a river or stream.

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3
Q

What is the technical term for water in puddles?

A

Depression storage.

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4
Q

What is the technical term for water stored in soil?

A

Soil moisture.

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5
Q

Name porous rocks which hold lots of water?

A

Aquifers.

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6
Q

What is the zone of saturation?

A

The zone of soil and rock where all the pores in the soil or rock are full of water.

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7
Q

Drainage basin Flows and Processes? Give 5 examples?

A

Surface runoff - Water flowing over land.

Throughfall - Water dripping from one plant to another.

Stemflow - Water running down a plant stem or tree trunk.

Throughflow - Water moving slowly downhill through the soil.

Infiltration - When water soaks into the soil. Infiltration rates are influenced by soil type and soil structure. During a storm water can’t infiltrate fast enough so flows over the surface.

Percolation - Water seeping down through soil to the water table.

Groundwater flow - Water flowing slowely through permeable rock below the water table.

Baseflow - Groundwater flow that feeds into rivers through river banks and river beds.

Interflow - Water flowing downhill through permeable rock above the water table.

Channel flow - The water flowing in the river of stream itself.

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8
Q

Explain Flows and Processes?

A

The movement of water from one place to another.

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9
Q

What is another name for channel flow?

A

The river’s discharge.

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10
Q

Drain basin Outputs? Give 3 examples?

A

Evaporation - water to water vapour

Transpiration - Evaporation from plant leaves.

Evapotranspiration - The process of evaporation and transpiration together.

River discharge

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11
Q

What does the water balance show?

A

The balance between inputs and outputs.

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12
Q

Define River Discharge?

A

The volume of water flowing in a river.

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13
Q

What do Hydrographs show?

A

The river discharge over a period of time.

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14
Q

In regards to a Hydrograph, what is peak discharge?

A

The highest point of the graph, when the discharge is at its greatest.

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15
Q

In regards to a Hydrograph, what is lag time?

A

The delay between peak rainfall and peak discharge. There is a delay because the water takes time to reach the river.

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16
Q

In regards to a Hydrograph, what is rising limb?

A

The part of the graph up to the peak discharge. Discharge increases as rainwater flows into the river.

17
Q

In regards to a Hydrograph, what is falling limb?

A

the part of the graph after the peak discharge. Discharge decreases because less water flows into the river.

18
Q

Name and explain physical factors which effect a Storm Hydrograph? Name 5?

A

Drainage basin characteristics - effects the lag time and peak discharge. e.g larger drainage basins, steep sided drainage basins, circular basins.

The volume of water that is already present in the drainage basin affects lag time. If the soil is waterlogged then infiltration is reduced and surface runoff is increased.

Rock type - affects lag time and river discharge. Impermeable rock increases surface runoff, reducing lag time and increasing the river discharge.

Soil type - affects lag time and peak discharge. The rates of infiltration differ between soil types.

Vegetation - affects lag time and peak discharge. The more vegetation, the greater the interception and the longer the lag time. A greater number of plants also reduces the water that gets to the river as the plants absorb some for internal processes.

Precipitation - affects peak discharge. The larger the volume of precipitation the greater the river discharge.

Temperature - affects lag time and river discharge. High temperatures increase Evapotranspiration, reducing river discharge.

19
Q

How does human activity affect a hydrograph?

A

In urban areas the soil is convered by impermeable materials such as concrete. The water cannot infiltrate and thus, surface runoff is increased and the water flows into the river more quickly, shortening the lag time and increasing peak discharge.

Man-made drainage systems do the same, they transport the water to the river at a faster rate, reducing lag time and increasing peak discharge.

20
Q

What features of a river can erosion affect?

A

Length, Depth and Width

21
Q

Explain Hydraulic action?

A

The pressure of the water breaks rock particles away from the bed and banks of the river.

22
Q

Explain Abrasion/Corrasion?

A

Eroded rock scrapes against the bed and bank, removing material.

23
Q

Explain Attrition?

A

Eroded rocks smash into each other and break up into smaller fragments.The rock fragments also become more rounded.

24
Q

Explain Cavitation?

A

Air bubbles in turbulent areas of the river implode and send out shockwaves that break rock off the banks and bed.

25
Q

Explain Corrosion/Solution?

A

The dissolving of rock by chemical processes. Carbon dioxide dissolves in the water to create a weak acid which reacts with limestone and chalk.

26
Q

Explain solution?

A

Substances that can dissolve and are carried along by the river.

27
Q

Explain suspension?

A

Very fine material such as silt and clay.

28
Q

Explain saltation?

A

Larger particles such as pebbles or gravel. To heavy to be carried in suspension so instead bounce along the riverbed.

29
Q

Explain traction?

A

Very large particles such as boulders are pushed along the riverbed.