Paper 3 River Holford Flashcards

1
Q

What is the title of the physical fieldwork?

A

An investigation to explore the changes in the River Holdford downstream.

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2
Q

Why was it a suitable location to use?

A

-close to the FSC
-it was only a short journey
-river had footpaths and was safe and accessible
-there was a car park
-previous school’s have studied here

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3
Q

What were the two risks?

A

Risk 1: Slipping and tripping
-wear sensible footwear, stay on footpaths and don’t run

Risk 2: Drowning
-avoid deep water, stay on footpaths and check weather.

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4
Q

What geographical theory did we use?

A

The bradshaw model

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5
Q

Explain what the Bradshaw model suggests.

A

-discharge increases downstream
-greater volume
-greater cross-sectional area of the channel (erosion)

-velocity increases as there is more energy
-less friction as channel widens and deepens

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6
Q

what were the 3 hypotheses?

A
  1. discharge increases downstream
  2. velocity increases downstream
  3. cross-sectional area increases downstream
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7
Q

What sampling method did we use?
Why?

A

-stratefied sample
-we planned out where we were stopping so it was stratefied.

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8
Q

What qualitative method did we use?

A

-used a field sketch
-annotated around it to highlights it’s characteristics

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9
Q

What first quantitative method did we use?

A

we measured the cross-sectional area
-used a tape measure to measure the width
-used a metre ruler to measure the depth
-used the width and depth to calculate the cross-sectional area

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10
Q

What second quantitaitve method did we use?

A

we measured the velocity
-used a tape measure to measure the width
-used a flow metre - impellor faced upstream, timed how long it took
-calculated the average for each site based on the 3 velocity readings

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11
Q

What primary data did we collect?

A

-velocity
-width
-depth
-cross-sectional area

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12
Q

What secondary data did we use?

A

Geology maps were used to identify the geology of the area beforehand

Google maps was used to identify site selection and safe access points

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13
Q

What data presentation method did we use?

A

A line graph was used to plot discharge against distance downstream.
avg discharge on y-axis and site number on x axis
-we showed how discharge changed along distance
-a line of best fit was used to highlight any anomalies.

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14
Q

What analysis did we do?

A

-discharge data was put in a table before added to a line graph and a line of best fit was drawn

-this was looked alongside annotated photos to show a visual representation of the change

-results were combined with other groups to gather a greater sample size- and compared with previous years to see how reliable the results were

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15
Q

What did we use GIS for?

A

We used GIS to locate our velocity data onto a map, to see how velocity changed across our 5 sites.

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16
Q

What results did we gather?

A

as we travelled downstream:
-velocity increased
-discharge increased
-cross-sectional area increased
e.g. width increased from 40cm to 2.1m

17
Q

what was our conclusion?

A

-as we travel downstream, velocity, discharge and cross-sectional area increase- Bradshaw model
-our methods met the aim of our enquiry- reliable
-we used technical equipment such as a flow metre which made our conclusions accurate
-human error did reduce the accuracy a bit
-there were a few anomalies that the line of best fit showed- however there is still a strong correlation between discharge and distance.

18
Q

How was our accuracy?

A

-an issue is that when the river was flowing fast, it was hard to hold the tape measure straight
-this could have impacted the measurements
-also measuring up to the wetter bank was subjective
-velocity readings weren’t always accurate- of the flow wasn’t fast enough etc

19
Q

How was our reliability?

A

-finding the wetter bank was subjective
-only took measurements on one day-wind and weather conditions could have impacted results.

-however we did take multiple readings and made averages- minus the anomalies- increasing relaibility.

20
Q

What was our overall evaluation?

A

-our conclusions are valid as we used samplong to gain a representative view of the river and to reduce bias.
-measured velocity 3 times and took average
-used same person to identify wetter bank each time
-tape measure was sometimes loose- less reliable
-compared results with other data -increasing accuracy- larger sample size

21
Q

What improvements could have been made?

A

-larger sample size- increasing reliability
-we could use diff techniques to measure velocity to increase accuracy
-gone back at different times in the year to assess how seasons affect the flow
-ensured ruler was facing upstream thin end when measuring depth

22
Q

Practice exam questions- Aims/ location

Explain why this was a suitable title for your fieldwork enquiry?
(2 marks)

A

-we used straefied sampling method to measure how the river holford changed downstream, we measured the depth, velocity and width to find the cross-sectional area and discharge. our fieldwork supported the bradshaw model

23
Q

Explain the advantages of the location used.
(2 marks)

A

-was accessible and safe
-had an accessible car park
-previous schools had used it
-it had footpaths

24
Q

Explain two reasons why particular aims or questions were developed.
(4 marks)

A

Our aims were to support the Bradshaw model which shared how the discharge increases downstream. As well as the cross-sectional area, velocity and width and depth increased.

25
Q

Explain why the chosen location was suitable for the collection of data?
(2 marks)

A

-it was safe and accessible
-had a nearby car park
-nearby facilities
-previous schools had studied their -legal and safe
-it had footpaths
-near the FSC -short distance

26
Q

Geographical theory/ concept:

Explain how this fieldwork enquiry helped your understanding of a geographical concept or theory.
(3 marks)

A

This enquiry helped my understanding of the Bradshaw model, as our results supported the idea that discharge, depth, width, cross-sectional area and velocity increased downstream.
There is greater erosion downstream, meaning the channel widens, causing a greater cross-sectional area and depth.
As well as the larger volume of water contributes to the discharge and velocity increasing downstream.

27
Q

Assess how helpful a geographical theory or concept were in developing your enquiry.
(9 marks + 3 SPag)

A