Rivers Fieldwork Flashcards
(35 cards)
quantitative data
numerical data that gives an amount or quantity or a range of figures
qualitative data
measuring the quality of something rather than its quantity. can be in words and descriptions
quantitative data methods
- river width
- river depth
- river velocity
- river discharge
- pebble size and roundness
qualitative data methods
- field sketch
- photographs
types of sampling
- systematic
- random
- stratified
- pragmatic
systematic sampling
collecting data in an ordered or regular way, eg at intervals
random sampling
unbiased as particular people/places/objects are not specifically selected
stratified sampling
dividing sampling into groups eg 3 sites from upper, middle, lower course of a river; or 5 people from each age range
river width (quant) method
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.
river depth (quant) method
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
river velocity (quant) method
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
field sketch (qualit) method
We observed the river landscape and created field sketches at the upper, middle and lower course of the River Chess.
sediment size and roundness (quant) method
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
river width advantages
Professional equipment increased the accuracy of our results as we did not estimate the width, ensuring results were taken to the nearest cm.
river width disadvantages
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.
river depth advantages
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
river depth disadvantages
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.
river velocity advantages
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
river velocity disadvantages
Impeller frequently became stuck or jammed, impacting the time measurement
field sketch advantages
Complimented our methods by allowing us to identify features in the landscape not identified by our quantitative data.
field sketch disadvantages
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.
sediment size and roundness advantages
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
sediment size and roundness disadvantages
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.
river width improvements
Use of pragmatic sampling – chose clear boundaries of river channel