Rivers Fieldwork Flashcards

(35 cards)

1
Q

quantitative data

A

numerical data that gives an amount or quantity or a range of figures

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2
Q

qualitative data

A

measuring the quality of something rather than its quantity. can be in words and descriptions

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3
Q

quantitative data methods

A
  • river width
  • river depth
  • river velocity
  • river discharge
  • pebble size and roundness
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4
Q

qualitative data methods

A
  • field sketch
  • photographs
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5
Q

types of sampling

A
  • systematic
  • random
  • stratified
  • pragmatic
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6
Q

systematic sampling

A

collecting data in an ordered or regular way, eg at intervals

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7
Q

random sampling

A

unbiased as particular people/places/objects are not specifically selected

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8
Q

stratified sampling

A

dividing sampling into groups eg 3 sites from upper, middle, lower course of a river; or 5 people from each age range

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9
Q

river width (quant) method

A

We measured the width of the river from bank to bank at each of the three sites we visited. The aim was for the sites to be representative of each course of the river. We made sure to measure straight across the river channel by pulling the measuring tape tight. The measuring tape did not fall below the water mark.

This measurement was only taken once at each site.

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10
Q

river depth (quant) method

A

Using the result we got for the river width, we divided the width of the river by 10. At every tenth interval, we measured the depth of the river using a rigid meter stick. This was placed in the river and we measured the water mark on the stick

Sampling method = systematic

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11
Q

river velocity (quant) method

A

A hydroprop was placed underneath the surface of the water. As soon as the hydroprop was submerged, the stopwatch timer was started. The impeller was placed against the flow of the river to ensure the speed was measured accurately.

We measured the speed three times – on the far bank, middle and near bank of the river

Sampling method = systematic

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12
Q

field sketch (qualit) method

A

We observed the river landscape and created field sketches at the upper, middle and lower course of the River Chess.

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13
Q

sediment size and roundness (quant) method

A

We selected 12 pieces of sediment at random. Discarded the largest and smallest sediment to remove anomalies. Using a pair of a callipers, we measured each pebble along the longest axis with a ruler and noted down the length in cm. We calculated the mean pebble size

We then compared each sediment to Powers Index of Roundness to give the pebbles a score according to their shape

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14
Q

river width advantages

A

Professional equipment increased the accuracy of our results as we did not estimate the width, ensuring results were taken to the nearest cm.

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15
Q

river width disadvantages

A

No guarantee that the results were reliable as we only measured the width once. This may reduce our ability to confidently answer our enquiry question, exploring how the River Chess varied with distance downstream.

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16
Q

river depth advantages

A

Increased reliability of results, as we took multiple measurements at each site and therefore could calculate the mean depth.

Use of professional equipment increased the accuracy of our findings

17
Q

river depth disadvantages

A

Large boulders could have interfered with our readings making the depth less accurate. Furthermore, groups had difficulty reading the water mark due to the weather conditions on the day.

18
Q

river velocity advantages

A

Use of professional equipment made it easy to collect data to aid the answering of our enquiry question

By measuring the internal velocity three times at each site, the reliability of our investigation was increased

19
Q

river velocity disadvantages

A

Impeller frequently became stuck or jammed, impacting the time measurement

20
Q

field sketch advantages

A

Complimented our methods by allowing us to identify features in the landscape not identified by our quantitative data.

21
Q

field sketch disadvantages

A

Open to interpretation – we may have picked up on certain aspects of the environment that other groups did not. We did not have enough specific understanding of the plant types/build use to support our investigation beyond the variables collected.

22
Q

sediment size and roundness advantages

A

Increased reliability of results, as we measured 10 pieces of sediment at each site and therefore could calculate the mean sediment size

More reliable to categorise sediment using Powers Index of roundness as allows for fair comparison across the sites

23
Q

sediment size and roundness disadvantages

A

Selection of pebbles may have been biased as we may have selected sediment, we could easily pick up reducing the accuracy of results.

Categorisation of sediment may be objective, and interpretation could vary at different sites.

24
Q

river width improvements

A

Use of pragmatic sampling – chose clear boundaries of river channel

25
river depth improvements
Increase sample size – number of intervals to measure depth
26
river velocity improvements
Repeat the measurement so that it is accurate Use systematic sampling – measure intervals across channel to increase sample size
27
field sketch improvements
Annotated photographs instead
28
sediment size and roundness improvements
Work in pairs to agree classification and keep the same people deciding pebble roundness at each site.
29
river width accuracy and reliability
Not reliable – only measured width once and it was hard to tell the edge of the channel Partially accurate – vegetation in the way whilst measuring width
30
river depth accuracy and reliability
Reliable as measured depth at every 10th interval – systematic sampling (large data set) Accurate as measured systematically and we used professional equipment (metre stick)
31
river velocity accuracy and reliability
Somewhat reliable as measured internal velocity three times at each site, however impeller would become stuck increasing time recordings Use of hydroprop increased the accuracy of results and repeated measurements reduced risk of anomalies, measurements were taken from different points of the river.
32
field sketches accuracy and reliability
Cannot draw conclusions from qualitative data alone. Did provide us with information to support understanding May not be accurate/reliable if drawing skills not good
33
sediment size and roundness accuracy and reliability
Partially reliable as sample size was large enough to be representative of the whole Somewhat inaccurate as subject to human error.
34
River Chess conclusions and summary
The purpose of the investigation was to find out if the chosen valley and channel characteristics vary along the River Chess. In conclusion, the river valley and channel characteristics do vary along the River Chess. More specifically, the River Chess does vary with distance downstream: the width and depth of the river increases and the mean velocity and discharge increase. Moreover, for each of these variables, it increased in size as moved from Site 1, in the upper course of the river, to Site 3, close to the river’s confluence with the River Colne. For example, we found that the width increased from 3.24m at Site 1 to 7.68m at Site 3. Data generally supports the Bradshaw Model with only a few anomalies identified. For example, site 2 had anomalous results for discharge and internal velocity. This may be due to several reasons. It may be due to the way the investigation was undertaken by a third party who may have used different methods and therefore not accurate or comparable. Furthermore, it may be due to human influences such as flood defences or urbanisation that have led to the unexpected results.
35
Bradshaw Model
illustrates what should happen in theory, and what usually happens, as a river travels downstream from source to mouth