coastal fieldwork Flashcards

(12 cards)

1
Q

hypotheses, conclusion and evidence for shingle ridge

A

hypotheses: the shingle ridge is steeper on the east side of the beach
conclusion: the shingle ridge is somewhat steeper on the east side of the beach
evidence: in the east the maximum slope angle is 35 degrees. in the west it only reaches 22 degrees. finding somewhat supports hypothesis

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2
Q

data collection for shingle ridge

A

data collection: used a clinometer and pointed it at the same place on the same place at one person at 5m intervals.
advantages:
- clinometer- accurate.
- beach profile transects spaced at 5m intervals (systematic sampling)- quite representative data, because of good coverage
disadvantages:
- because of systematic sampling, not all variations between transects captured, limiting representation
- clinometer- difficult to use precisely in windy conditions, better to use poles. so beach gradient not entirely accurate
- measuring tape- not held taught because of windy conditions, distance measured inaccurately.

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3
Q

data presentation and analysis for shingle ridge

A

beach profiles drawn onto the same graph, so easy visual comparison- immediately see which side is bigger and by how much
clearly see differences
generalisation, doesn’t allow for nuances

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4
Q

hypotheses, conclusion and evidence for sediment size

A

hypothesis: sediment size is smaller on the east side of the beach
conclusion: sediment size is much bigger on the west side of the beach than on the east side of the beach
evidence: avg sediment size much bigger on west side (median = 13.5cm) than on east side (median = 4.4cm). strongly supports hypothesis with a difference of 9.1cm

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5
Q

data collection for sediment size

A

data collection: used callipers, on the long axis with random and stratified sampling
advantages:
- callipers- accurate data readings because stone held tightly in place and precise because it shows measurements to 1mm
- large sample size of 100+ after groups collated data, makes it representative
- stratified sampling- efficient strategy, wanted to measure start to end of longshore drift
- random sampling- used a random number generator and a grid, reduce bias and increase reliability
disadvantages:
- long-axis measurements doesn’t allow for most accurate measurements, only captures one dimension. to improve, measure other dimensions
- random sampling- at each grid there were a number of rocks, so bias was likely introduced there

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6
Q

data presentation and analysis for sediment size

A

presentation: dispersion graphs clear, visual way of comparing spread of data at both sides of beaches. same graph and scale, immediately see results and differences- east has larger range of pebble sizes.
proportional symbols map shows immediately and clearly mean pebble size is bigger on the west side of the beach
analysis: calculating mean- allows us to summarise data clearly in a statistic and get rid of anomalies
calculating IQR allows us to identify bigger range of data in east compared to west, more complex than mean suggests

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7
Q

hypotheses, conclusion and evidence for sediment shape

A

hypothesis: sediment shape is rounder on the east side of the beach
conclusion: sediment size overall rounder on east side of the beach than on west
evidence: in east, there are 30 very round pebbles, in west only 5 very round pebbles. strongly supports our hypothesis

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8
Q

data collection for sediment shape

A

data collection: used power’s scale of roundness to judge sediment shape, with random sampling (grid method) and stratified sampling
advantages:
- stratified sampling- efficient strategy, wanted to measure start to end of longshore drift
- random sampling- used a random number generator and a grid, reduce bias and increase reliability
disadvantages:
- random sampling- at each grid there were a number of rocks, so bias was likely introduced there
- power’s scale of roundness very objective, makes it unreliable. to improve- same person making all the judgements to increase consistency, group decides by consensus

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9
Q

data presentation and analysis for sediment shape

A

radial graphs for sediment shape provide a clear comparison of frequency and spread of different categories of sediment roundness

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10
Q

field sketches

A

advantages:
- useful compared to photos, emphasise relevant features and processes
disadvantages:
- very subjective, leads to unreliability

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11
Q

primary data

A

sediment shape
sediment size
beach profile
annotated field sketch

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12
Q

secondary data

A

rose diagram showing wave direction

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