Fieldwork Flashcards

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1
Q

Enquiry question

A

Does flood risk along the river wear increase as you go downstream

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2
Q

Why is bedburn beck a suitable location

A

Easily accessible - could travel to and from the study location within a school day

The was was shallow enough to investigate safely

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3
Q

Each of the sites were appropriate because

A

They were accessible by minibus - car parks close by

Sites were far apart enough to show changes in channel and drainage basin characteristics

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4
Q

Limitations of chosen site

A

Only investigates sites in the upper course of a tributary of the river wear

Means that we could not look at flood risk downstream in urban areas such as Durham and Sunderland

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5
Q

What is Primary data

A

Information date that you collect yourself eg photographs

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6
Q

Examples of primary date

A

Field sketch

Depth

Sediment survey

Gradient

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7
Q

What is secondary date

A

Info that someone else has previously collected made available eg on the internet

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8
Q

What secondary data could use as to support our investigation on river characteristics and flood risk

A

Land use map

Geology map

OS map

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9
Q

Human and physical reasons why there’s a higher flood risk in some parts of the wear

A

Areas such as old Durham have a higher flood risk because of impermeable and permeable rocks. Steeper relief encourages run off (physical)

urbanisation (human) -

River Discharge increase (physical)

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10
Q

2 types of errors that can occur when collecting primary data

A

Measurement errors - mistakes made by using equipment incorrectly

Operator error - caused by person collecting date

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11
Q

What is accuracy

A

How precise the data is

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12
Q

What is the reliability

A

If you were to repeat the method how likely it is to record the same results

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13
Q

General condition of fieldwork visit

A

22nd June hot dry day that was warmer than average

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14
Q

Method of measuring width

A

Stretched a tape measure from one can’t to another holding it taught above the surface of the water

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15
Q

Explanation of width

A

Measured to calculate discharge the wider the river the greater the discharge

Where discharge is high flooding is likely

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16
Q

Evaluation of width

A

Sometimes the tape measure sagged in the middle reducing the accuracy of data

17
Q

Method for depth

A

Different meter sticks to measure the depth at 10 different points. Divided the width by 10 to use a systematic sample

18
Q

Explanation of depth

A

Measured to calculate discharge the deeper the river the greater the discharge. Where discharge is high flooding is likely

19
Q

Evaluation of depth

A

The meter stick sank into the soft mud in the river bed reducing the accuracy of the depth data

20
Q

Method of velocity

A

We used the float method to measure the speed of the river. Placed 2 ranging poles 2 metres apart and timed the ball

21
Q

Explanation of velocity

A

Measured to calculate discharge the faster the river the greater the discharge

Where discharge is high flooding is likely

22
Q

Evaluation of discharge

A

We did 3 velocity reading at each site and calculated an average . This improved the accuracy of the data

Sometimes the balls got stuck on the banks a float meter would’ve been more accurate

23
Q

Method of gradient

A

Measured the distance of 2m using a tape measure and marked it using 2 ranging poles. We used a clinometer to measure the gradient in degrees

24
Q

Explanation gradient

A

The steeper the gradient of the drainage basin the less infiltration there is and the quicker rainwater gets into the river increasing flood risk

25
Q

Evaluation gradient

A

We had never used a clinometere before so many have used it incorrectly

Sometimes the ranging poles were tilted instead of vertical

Factors that reduce accuracy

26
Q

Sediment survey method

A

We selected one rock next to each depth reading and measured its longest edges (y axis) we then used powers scale of roundness to categorise the rocks into class 1-6

27
Q

Explanation of sediment survey

A

The smaller and rounder the sediment the more erosion is taking place where there is a lot of erosion the river has more energy and therefore is more likely to flood

28
Q

Evaluation of sediment survey

A

There were operator errors (subjective) because people were more likely to pick up larger rocks and gbere was some disagreement about powers class which reduces accuracy

29
Q

Drainage basin characteristics method

A

Observed the river from each site and drew its main features . We added annotations to describe the environment

30
Q

Drainage basin characteristic explanation

A

Land use shows the value of land the higher value land the greater risk if it is flooded. The vegetation cover shows how much interception will take place more vegetation reduces the risk of flooding

31
Q

Drainage basin characteristics evaluation

A

A sketch allows you to focus on specific features that are relevant to your study

They also provide a visual reminder when analysing results

32
Q

Flood risk map source and and info obtained

A

Environment agency and OS

Shows that flood risk increases from low/medium to high as you go further downstream

Urban areas are most likely to flood because of tarmac

33
Q

How do channel characteristics influence flood risk of the river wear - how does discharge influence flood risk

A

Discharge increases down stream and the channel becomes wider and deeper

This increases flood risk because the larger the volume of water the more likely it is to flood

34
Q

How does sediment size influence flood risk

A

Sediment size decreases downstream this tells us attrition is taking place

This means there is less friction in the channel so the river can flow more quickly

35
Q

How does drainage basin characteristics influence flood risk over the river wear - does geology influence flood risk

A

Most of the best rock in the west basin is sandstone, mudstone and coal . These rocks are permeable and allow water to perculate

This reduced surface run off flood risk

36
Q

How does gradient influence flood risk

A

Gradient decreased downstream this reduces flood risk because of infiltration and perculation take place faster on gentle slope

Where slopes are steeper more surface run off happens

37
Q

Land use at rivers

A

Upstream is rural - permeable vegetation with coniferous forests that intercept rainwater

Downstream - urban - higher flood risk because of drains and concrete eg Durham