fieldwork - river holford Flashcards

1
Q

what is the title of our physical fieldwork?

A

Exploring downstream changes along the River Holford

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2
Q

benefits of the location

A
  • river had footpaths = safe and accesible
  • accesible car park
  • river showed obvious changes
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3
Q

name 2 risks and ways to prevent them:

A
  1. slipping/tripping - wear appropiate footwear, dont run
  2. drowning - avoid deep fast flowing water
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4
Q

whats the geographical theory?

A

BRADSHAW MODEL
- discharge increases downstream as tribatries join
- velocity increases as there is larger for veloicity of water = more energy & less friction as chanell widens and deepens

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5
Q

hypothesis

A
  1. discharge will increase as we move downstream
  2. velocity will increase as we move downstream
  3. cross section area will increase as we move downstream
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6
Q

what sampling method did we use?

A

stratified & some systamtic
- measuring after tributries and their safety

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7
Q

explain the qualitve method used?

A
  • we used a field sketch/photo and annotated it to higlight key features e.g gradient, pebble size
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8
Q

explain quantative method

A
  • cross sectional area
  • we used a tape measure to measure the width of the wetted edges [stratfied]
  • then divided the width by 10 and used a meter ruler to measure the depth at all 10 points [thin end faced up stream]
    =sytematic
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9
Q

explain quantative method 2 [systematic]

A
  • velocity
  • at each site we measured the width w a tape measure and divided it by 3
  • at each point used a** flow meter **and timed how long it took the impellor to reach the bottom
  • then worked out the mean velocity from 3 readings
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10
Q

secondary data used ?

A
  • geology maps to work out geology of area
  • google maps = to identify safe acsess points
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11
Q

how did we present our data

A
  • line graph
  • ## plot discharge against distance downstream
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12
Q

how was GIS used

A
  • to locate our velocity data onto a map = so we could visually see the change in velocity
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13
Q

what did our results show

A

as we travelled downstream the discharge, cross sectional area and velocity increased

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14
Q

how reliable were our results

A
  • in fast flowing parts = hard to keep tape measure taut may have impacted reading
  • identifying the wetted bank = subjective
  • only took data from 1 day = so the wind direction and weather may of impacted results
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15
Q

what improvements could be made?

A
  • larger sample size
  • gone at different times of year
  • use a dif technique for velocity w low flow
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