1st fieldwork trip Flashcards

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1
Q

what is the hypothesis??

A

as velocity increases across a channel, erosion increases across the channel on the river.

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2
Q

why this location?

A

it was close to be able to go there and collect enough data in a day. river is low risk. there is a coach parking so we didn’t have to walk far.

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3
Q

person A stands one side of the river holding the tape and person B holds the tape measure on the other side. person C uses a meter stick and records the depth every metre along the tape measure =

A

Method 1 - river depth
sampling method - systematic, 10 times at each site

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4
Q

strengths of measuring river depth =

A
  • easy to conduct.
  • simple to record the measurements.
  • water shallow enough to carry out measurements safely.
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5
Q

weaknesses of measuring river depth =

A
  • big rocks prevents metre stick touching river bed.
  • raking accurate measurements across river channel sometimes hard if tape not pulled taught.
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6
Q

aim for measuring the river depths =

A

to investigate if erosion is occurring on the river bed.

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7
Q

10 rocks from the river to be picked up and measured with a ruler =

A

Method 2 - sediment size.
sampling method - systematic, 10 each site.

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8
Q

strengths of measuring the sediment size =

A
  • cover the whole river channel rules out bias.
  • easy method to measure rocks.
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9
Q

weaknesses of measuring the sediment size =

A
  • not accurate.
  • sometimes rocks cant be picked up.
  • sometimes might pick up small rocks only making sample bias.
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10
Q

aim for measuring the sediment size =

A

to investigate the effects erosion on the sediment size.

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11
Q

using a float students record how long the float takes to travel 1m =

A

Method 3 - velocity
sampling method - systematic, 10 at each side.

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12
Q

strengths of measuring the velocity =

A
  • simple.
  • covers all the sides of the river to create an average and repeated measurements.
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13
Q

weaknesses of measuring the velocity =

A
  • float can get stuck.
  • wind can affect the float.
  • human error with time.
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14
Q

aim for measuring the velocity =

A

to investigate the velocity of the river to compare with the erosional data.

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15
Q

risk factors =

A

injury - students could trip = first aid kit with teachers and students should wear suitable footwear.
drowning - students could slip and drown = only go in if supervised and not too deep.
weather - wet weather (slippery ground), hot weather (leads to dehydration) = lots of water and sun cream, appropriate clothes and footwear.

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16
Q

Evaluation = time of year -

A

river was lower than expected so the results are not accurate. going multiple times over the year would’ve gave us more accurate data.

17
Q

Evaluation = lack of equipment -

A

a flow meter would’ve provided more accurate data.

18
Q

strengths of using bar chart to present the river depths =

A

very clearly shows the depth of the river at each side. shows discrete data.

19
Q

weaknesses of using bar chart to present the river depths =

A

needs to be compared with velocity to prove / disprove the hypothesis.

20
Q

strengths of using a scatter diagram to present the river depths =

A

easy to see clear positive correlation between the velocity and river depth. easy to anomalies.

21
Q

weaknesses of using a scatter diagram to present the river depths =

A

doesn’t consider human errors could be responsible for anomalies.

22
Q

positive correlation between the velocity and the river depths -

A

suggest higher velocity causes more erosion which proves the hypthesis.