Callipers provided data taht was accurate to the nearest mm (accurate)
The same method and equipment was used at each site (reliable)
10 pieces of bedload at each site allowed an average to be calculated (accurate)
Data was collected on the same day (reliable)
H2: Velocity
Strengths:
3 measurements were recorded (left, middle, right). An average was calculated (reliable and accurate)
The same method and equipment were used at each site (reliable)
Our data was collected on the same day when there was no rain and the river was not too high/low. A change in weather could have affected the velocity and turbulence levels.
H2: Velocity
Problems:
Floats got stuck and had to be released (less reliable/accurate)
Didn't use the same float every time (inconsistencies)
Human error with start/stop stopwatch (less reliable)
Different groups collected data (inconsistencies)
3 velocity readings in the lower course were not enough (less reliable)
H1: Bedload size:
Problems:
Not all the load could be measured (boulders at site 1/suspended sediment at site 6) (less reliable)
Different groups collected the data at each site (inconsistency)
Number of sites:
2 in upper course 3 in middle course 1 in lower course
Strengths:
allowed us to investigate the long profile of the river and achieve our aim
Problems:
only 1 site in lower course. This made data less reliable for the full length of the river.
Other data that would be useful:
1 additional site in lower course
use systematic sampling to collect data every 1km downstream
Extending scope of study:
We could investigate an additional hypothesis such as bedload shape, gradient or discharge.
We could use systematic sampling to identify 12 sites at equal intervals down the river with 4 in each course.
We could compare our results with the Annalog river which has less development.