River Holford field work (paper 3) Flashcards

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1
Q

what is the fieldwork title for this assessment

A

investigating downstream change on the river Holford

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2
Q

what is your hypothesis for this assessment

A
  • discharge will increase with distance downstream on the river holdford because more tributries join to creater a larger river so more water
  • velocity will increase with distance downstream on the river Holford because more water and energy with a bigger channel means less friction so water moves more freely
  • cross-section area will increase as we move down stream
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3
Q

how long is the river Holford

A

8km

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4
Q

describe the geologies of the river Holford in the upper, middle and lower courses

A
  • upper = sandstone
  • midde = mudstone
  • lower = limestone
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5
Q

explain the advantage of the fieldwork location used for your enquiry

A
  • accessibly - mainroad ~ A39
  • we can walk along it - good idea of change in a timely manner ~ small river
  • accessable car park
  • previous schools hae studied here so it was safe and legal to do so
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6
Q

what was your chosen sampling method

A

statified = geographical knowledge to choose location (after each tributry)

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7
Q

why was your samplying method appropiate for your enquriy

A

it is feesable in the timelimit, we know where the river changes and we can locate change at those sites and easily collect data

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8
Q

give two risk assessments and how to avoid them

A
  • slipping/tripping = sensible footwear, follow paths
  • drowning = avoid deep fast flowing water, stick to footpaths
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9
Q

what samplying method could have you done instead of stratified

A

systematic # measurements taken every 1km = less bias and manageable

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10
Q

what was your qualitative method of assessment

A

we used a field sketch and annotated around the skets to highlight chacteristics of each site (gradient, pepple size, land use)

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11
Q

what were the two quantitive methods of analysis

A
  • cross section area
  • velocity of water
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12
Q

explain how cross section area was used to assess river Holford

A
  • we used a tape measure to measure the width from wetted edge to wetted edge
  • we divided the width by 10
  • we used a meter ruler to measure the depth at the same points, ensuring the thin side faced upstream to reduce splash and inaccuracy
  • we then used these measurements to calculate the area by multiplying them together
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13
Q

explain how velocity measurement was used to assess river Holford

A
  • we used a tape measure and divided the width by 3 so we could take 3 readings per site
  • we used a flow metre, ensuring the impellor faced upstream
  • we timed how long it took the impellor to reach the base and recorded the value
  • we then calculated the avergae at each site
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14
Q

how did you ensure reliablility for these measurements taken

A
  • width = pull the tape taught and water to water
  • depth = thin end upwards and bottom touching the base of river
  • speed = ensure impellor was not touching base and it was facing upstream
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15
Q

explain why the pattern of your results for cross profile may not be completely accurate

A

we only took 5 measurements along the width and it would be more accurate if we took more as we may of missed a particulary deep or shallow section

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16
Q

explain the advantage of collated the class data

A
  • anomolies wouldnt stand out as much
  • more results recorded on a whole so more reliable
17
Q

explain the overall pattern shown by the discharge measurements you took

A
  • the further the distance downstream the large the volume of discharge gets
  • becasue the river gets wider and deeper due to erosion by abrasion
  • this allows for a larger channel with more discharge
  • and as more tributries join, more water does as well
18
Q

what were you data representations on the river Holford assessment

A
  • cross profiles (width and depth)
  • scatter graph (discharge)
  • GIS location proportional symbols
19
Q

explain the advantages and disadvantages of using cross profiles as a data representation

A
    • easy to read and compare
    • allows a view of depth and width
    • geolocated
    • you can miss points which are more shallow or deeper
20
Q

explain the advantages and disadvantages of using a scatter graph to show discharge along the river Holford

A
    • shows anomolies well
    • allows for estimate of discharge in unassessed areas
    • read off it well
    • not geolocated = cannot tell where the measurements were taken
21
Q

explain the advantages and disadvantages of using GIS location proportional syboms to show the discharge along the river Holford

A
    • geolocated = shows exactly where data is from
    • easy to read the proportional circles
    • can preform spacial analysis
    • cannot get exact values ~ you’re given a range
22
Q

overall how was your presentation of data… effective or ineffective

A

effective becuase we could know where our data was from and allowing us to spacially analysis our results to reach our conclusion

23
Q

describe youre results from the assessment

A
  • as we travelled downstream velocity increased, discharge increase and cross sectional area increased. for instance the average wdith increased from 40cm to 2.1m from site 1 to site 5
24
Q

outline your conclusion from your assessment down the river Holford

A
  • as we travelled downstream, velocity, discharge and cross sectional area increased; supporting the Bradshaw model
  • it was valid because our methods were reliable and we used technical equipment (flow meter)
  • however human error did reduce accuracy as some anomolies were present although we did a line of best fit which supported our hypothesis nevertheless
25
Q

comment on the strenght of your conclusion

A

it is semi-reliable as it fits in the bradshaw model, although the sampling rate is not high enough to fully be reliable

26
Q

give two improvements included in your evaluation

A
  • it would be better is we used a digital flow metre rather than an impellor to increase accuracy
  • it would have been better if we used a laser metre rather than a tape measure to measure the width to increase reliablity
  • we could have used a larger sample size by measuring more sites to increase reliability