physical fieldwork Flashcards

1
Q

what is our physical fieldwork question

A

how does the cross section of the river tarrell change as we move downstream?

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2
Q

what makes our question suitable for a geographical enquiry

A
  • able to collect primary and secondary data > can draw conc.
  • small-scale > short river so can measure along
  • low/manageable risk > shallow
  • clearly a geographical question - ab a place and appears in syllabus > can test Bradshaws theory
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3
Q

how was our fieldwork practical in terms of access

A
  • on public land so we can access river
  • terrain/landscape is not too challenging to walk
  • parts of the river on private land + we have permission to visit so we could access all of the long profile
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4
Q

how was our fieldwork practical in terms of safety

A

relatively shallow so able to take measurements

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5
Q

how was our fieldwork practical in terms of manageability (scale)

A

river is relatively short so can measure long profile and see differences

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6
Q

what was good ab the location of the river in terms of geography

A

able to access river from source to mouth so we could test Bradshaws geographical theories there

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7
Q

what was good ab the location of our river in terms of data

A
  • relatively shallow so easy to measure so data is accurate
  • all rivers in uk have secondary data
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8
Q

who was our theorist

A

bradshaw

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9
Q

what did Bradshaw say

A
  1. width should increase downstream
  2. depth should increase downstream
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10
Q

what were the risks with our fieldwork

A
  1. drowning in river
  2. getting cold from spending day in the field
  3. getting hit by a car
  4. accidents in river
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11
Q

what action did we take to minimise risks

A
  1. areas where the river was too deep we did not take measurements, working in supervised small groups
  2. bringing spare clothes and warm layers
  3. cross at safe locations
  4. bring a first aid kit + mobile phone
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12
Q

justify measuring the width as one of our methods

A

we wanted to see how the cross section of the river tarrell changes downstream because Bradshaw suggests that rivers on average get wider and deeper. so we needed to measure the width of 10 places along the long profile to see if this happened.

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13
Q

what was good ab our width method

A
  • easy to use
  • portable
  • simple (method + equipment)
  • cheap
  • fast
  • can look at past data
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14
Q

what was bad ab our width method

A
  • can be inaccurate:
    > current would sometimes pull the tape measure
    > vegetation in the way so sometimes hard to find edges
    > not measuring from undercut (upper course)
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15
Q

overall judgement of width methodology

A

fairly reliable and successful method w/ accurate data

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16
Q

justify measuring depth as one of our methods

A

we wanted to see how the cross section of the river tarrell changes downstream because Bradshaw suggests that rivers on average get wider and deeper. so we needed to measure the depth of 10 places along the long profile to see if this happened.

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17
Q

what was good ab our depth method

A
  • easy to use
  • portable
  • simple (method + equipment)
  • cheap
  • fast
  • can look at past data
  • taking a mean of depth
  • ruler can float so doesn’t drift away
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18
Q

what was bad ab our depth method

A
  • ruler would often bend at high current areas so the data was unreliable
  • distance between measurements was larger in middle course so data is less accurate
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19
Q

overall judgement on depth methodology

A

fairly reliable and successful method w/ accurate data

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20
Q

justify our use of stratified sampling

A

we needed to cover the whole long profile so we had to choose sites in the upper, middle and lower course but some of the river was too difficult to access or too dangerous to get into because it was too deep or fast-flowing so we had to choose our sites to an extent.

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21
Q

what was good ab our use of stratified sampling

A
  • could choose 10 sites that cover the entirety of the long profile so we could avoid any private land or dangerous parts of the river
22
Q

what was bad ab our use of stratified sampling

A
  • creates a bias as ensuring that it was safe may mean picking shallower sites to take data from which could distort data making our river seem shallower than it is
23
Q

overall judgement of our sue of stratified sampling

A

fairly reliable + successful method b/c it allowed us to access the river safely + answered the question

24
Q

justify our use of secondary data using google earth

A

enables us to see the long profile of the river and plan the sites to show how the cross-section changes downstream - according to Bradshaw, river width and depth should increase downstream

25
Q

justify using maps in our enquiry

A
  1. familiarise myself w/ area of fieldwork before going on field trip
  2. choose suitable sites for data collection based on accessibility
  3. add to your primary data
26
Q

justify using photos in our enquiry

A
  1. helps familiarise myself w/ area of fieldwork before going on field trip
  2. can show important features
  3. more accurate than a sketch
  4. may be use to make measurements
27
Q

what was good ab using bar chart to represent data

A

same as justify - easy to read the results and see trend

28
Q

what was bad ab using bar chart to represent data

A
  • doesn’t show the cross section of the river
  • can be misinterpreted as it seems the sites are equally spaced out
  • answers half the question
29
Q

overall judgement of bar charts to represent data

A

fairly reliable

30
Q

what was good ab using located cross section to represent data

A

answers question fully and clearly

31
Q

what was bad ab using located cross section to represent data

A

can be hard to observe trend and interpret

32
Q

overall judgement of located cross section to represent data

A

superior presentation technique

33
Q

what did the data show

A
  1. width increases downstream
  2. depth slightly increases downstream
34
Q

how did the data help us answer our question

A
  • our question was how does the cross section of the river tarrell change as we move downstream?
  • Bradshaw said that the width and depth of the river should increase downstream so we expect the cross section to increase downstream
  • our width showed that the river got wider downstream
  • this suggests that Bradshaws model fits the river tarrell
  • our depth showed that the river got slightly deeper downstream
  • this suggests that Bradshaws model generally fits the river tarrell
  • overall the cross section of the river increases as we go downstream,
35
Q

evaluate our width results

A

GOOD:
- easy to collect
- cheap equipment
- past data to compare it too
- 10 sites

BAD:
- downstream river wider and current faster so tape measure would drag
- hard to identify where edge of river was when there was an undercut

36
Q

evaluate our depth results

A

GOOD:
- repeated measurements 5 times and took a mean
- past data to compare it too (acc.)
- easy to collect so can be done in a day

BAD:
- distance between 5 depth points increased as you go downstream so acc. decreases
- for safety picked shallower sites downstream so river seems shallower in lower course
- anyone standing upstream disrupted the depth

37
Q

what was the problem with the width method

A

as the river gets wider the tape measure gets caught in the current

38
Q

what is one improvement we could make to the width method

A

in lower course sites have someone hold the tape measure in the middles the tape remains taut

39
Q

what effect would improving the width method have on our results

A

makes our results more accurate, narrower downstream than we originally thought

40
Q

what effect would improving the width method have on our conclusions

A

makes the conclusion that the width increases more reliable - although narrower downstream, results would still significantly show the river gets wider

41
Q

what was the problem with the depth method

A

further downstream gaps between the depth measurements were much larger as we still only measured 5 points across the river

42
Q

what is one improvement we could make to the depth method

A

as the river gets wider measure the depth at more than 5 times to reduce anomalies

43
Q

what effect would improving the depth method have on our results

A

gives a more acc. cross section and will remove anomalies and give a more acc. depth b/c you’ve taken more measurements

44
Q

what would improving the depth method have on our conclusions

A

makes conc. that the depth got deeper more reliable and will allow us to have a detailed cross-section

45
Q

what are general improvements we could make to the methods

A
  1. more sites - longer stretch of river
  2. do it on a diff. day
  3. compare data w/ previous data collected
46
Q

justify our investigation of human interaction

A

we measured the width + depth of the river under a bridge to see what impact humans might have on these features

47
Q

what were the results of our investigation of human interaction

A

river got narrower but deeper

48
Q

what was good ab our investigation of human interaction

A

results were fairly acc.

49
Q

what was bad ab our investigation of human interaction

A

river was fast flowing here + deep so it was difficult to hold the measuring stick still or read the measurement accurately

50
Q

overall judgement of our investigation of human interaction

A

we were fairly sure that the river got narrower but deeper when humans built bridges