Fieldwork Methods (Edexcel GCSE Geography B)
Revision Note
Written by: Bridgette Barrett
Reviewed by: Jenna Quinn
River Fieldwork Methods
Data Collection Methods
The data collection methods will depend on the aims/hypothesis of the fieldwork
The starting point with most river fieldwork is to measure the width and depth
Data collection should include both quantitative and qualitative methods
The collection of quantitative data can be completed in several ways in a river study
Width
The measurement of width is taken where the water surface comes into contact with the river banks.
To take an accurate measurement:
Measure from the point where the dry bank meets the water on one side to the point where the dry bank meets the water on the opposite side
Ensure that the tape is held taut and does not touch the water this could affect the reliability of the data
Depth
The measurement of depth should be completed at regular intervals across the width
This ensures a full picture of the changes in depth across the whole channel width is recorded
It also allows a mean depth to be calculated to use in the calculation of river discharge
To take an accurate depth measurement:
Work out the distance apart each depth measurement needs to be
Place a meter rule into the water at the correct point
Ensure the meter rule is placed sideways with the flat side facing the banks: this reduces any impact on the water height ensuring more accurate measurements
Record the distance from the bed to the surface of the water
Repeat this across the width of the river
Velocity
The velocity is the speed at which the river flows
This can vary across the channel width as well as along the course of the river so velocity should be recorded in three positions: towards the left bank, centre and towards the right bank
Using a flow meter velocity can be easily measured by:
Taking readings at three equal distances across the river width
Placing the flow meter into the water at least 3cm below the surface
Three readings should be taken at each of the three places across the channel to allow the calculation of a mean
To take an accurate measurement using a float:
Measure a set distance upstream - for example, 10 meters
Drop a float at the start of the 10 meters
Time how long it takes for the float to travel the distance using a stopwatch
Repeat at each position three times to allow the calculation of a mean
Discharge
The discharge of the river is calculated rather than measured
The first step is to calculate the cross-sectional area:
Cross-sectional area (m2) = width (m) x mean depth (m)
The second step is to calculate the velocity:
If a flow meter the mean velocity should be calculated by adding the velocity measurements and dividing by the number of measurements
If a float has been used and a distance of 10m then the meantime should be divided by 10 to calculate the time taken to travel 1m
Discharge (m3/s) = cross-sectional area (m2) x velocity (m/s)
Gradient
As it moves downstream rivers decrease in height
This is the gradient of the river
The gradient is measured over a 10 meter stretch of river with a ranging pole placed at 0m and another clinometer at 10 meters
A clinometer is then used to measure the difference in height between the two poles
Photographs and Field Sketches
Photographs and field sketches are qualitative data
Just as with any data collection and presentation they have strengths and weaknesses
In a river enquiry photographs and field sketches can be used to show landforms and particular features such as bed load
Photographs are also ideal for illustrating the data collection methods used
Worked Example
You have carried out your own fieldwork investigating the influence of drainage basin and channel characteristics on flood risk.
Explain one method that you used to collect your primary data
(2 marks)
Answer
We measured depth using a tape and metre rule (1) taking measurements at x sites upstream/downstream from our access point (1)
We measured width using a tape (1) taking measurements at x sites upstream/downstream form our access point (1)
We measured gradient using a clinometer, a tape and ranging poles (1) both upstream and downstream from our point of access (1)
Examiner Tips and Tricks
Annotations and labels are not the same. A label is a simple descriptive point. For example, 'meander'. Whereas an annotation is a label with a more detailed description or an explanatory point. For example, 'slip off slope where the material has been deposited due to slower flow'
River Enquiry Data Presentation
Data presentation can take many forms
Primary Data
Much of the primary data collected in a river enquiry will be presented in the form of a graphs
Each type of graph is suitable for particular data sets
The graphs also may have strengths and limitations
Suitable graphs include:
Line graphs for river channel cross-sections
Bar graphs to compare different sites
Scattergraphs to show the relationship between two sets of data. For example, the river width and discharge
Examiner Tips and Tricks
In the exam, you will not be asked to draw an entire graph. However, it is common to be asked to complete an unfinished graph using the data provided. You may also be asked to identify anomalous results or to draw the best fit line on a scattergraph.
Take your time to ensure that you have marked the data on the graph accurately
Use the same style as the data which has already been put on the graph
Bars on a bar graph should be the same width
If the dots on a graph are connected by a line you should do the same
Secondary Data
Any fieldwork should include secondary data as well as primary data
In a river enquiry suitable secondary data may include:
River discharge data from the Environment Agency
Weather data from the Meteorological Office (Met Office)
Old photographs of the river sample site
Newspaper articles/websites about the river
Ordnance Survey maps to identify the sample sites
Geology maps
Aerial photographs
Analysis
Once data has been collected and presented it needs to be analysed
The data which is collected from the river such as width, depth, velocity is quantitative data and will need to be analysed using statistical methods
One of the main statistical methods used in a river enquiry will be the mean where mean depth or velocity needs to be calculated
Geographical theories and case studies can also be used in the analysis to explain whether the data collected was as would be expected based on knowledge from those theories/case studies
Analysing Photographs and Field Sketches
Use of photographs and field sketches is a qualitative analysis
Photographs can be used in a river enquiry to analyse a number of features:
Landforms and their formation
Data collection techniques
Worked Example
Analyse Figure 1 which is the data collected by a group of students studying changes in river characteristics
Describe the relationship between river gradient and velocity
(4 marks)
Answer
In general the steeper the gradient the lower the velocity (1) so at site 1 4.5o and 14.5 cm/sec (1)
Site 3 looks to be an anomaly (1) the gradient at this site is 3o but the velocity is much lower at 8 cm/sec compared to other sites with similar gradients(1)
Sites 6,7 and 8 also pose some problems (1) but gradient differences are very small indeed (1)
Conclusion
Once the data collected has been analysed, conclusions can be reached
This should state whether the hypothesis has been proved or disproved
Identify and explain anomalies such as:
Decreasing average depth or width with distance downstream at one site
Decreased velocity at a particular site
Anomalies may just occur or may be the result of incorrect recording or human error reading equipment
Evaluation
The final stage of the river enquiry is the evaluation where you note how successful, or not, the river investigation was and what you would do differently next time
Next time I would take measurements over a longer period of time to ensure the reliability of data...
My equipment failed and I would make sure to bring a spare next time...
I think my investigation went well and I would like to repeat this after a storm event to see how much erosion has taken place...
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