Use the materials above to answer the questions below in detail and using diagrams to help.
What is the Bradshaw Model? How does it help us understand how a typical river is expected to change from source to mouth?
How can a simplified model help us to study and understand the real world?
For each aspect of the Bradshaw Model describe the following using diagrams to help: how does the Bradshaw Model suggest it will change as a river moves downstream? Why are these changes expected? How would you measure this in the field to see if it applies to a particular river (use the file below to help).
How to measure river characteristics
1. Channel Width This is measured using a tape measure stretched across the channel. Measure the width across the surface of the water. Record the measurement on the recording sheet. 2. Channel Depth Take the width of the channel and divide it into 11 equal parts. Measure the depth at the ten points across the channel. Always start from the same side; left or right when looking downstream. Record the measurements on the recording sheet.
3. Cross-sectional area To calculate this you use the formula below:
Cross sectional area (m2) = Width of river (m) x Mean depth of river (m)
To measure velocity we use a flow meter.
Using the flow meter measure the speed of the river flow at 5 equally spaced points across the channel.
At each point measure the speed at the surface, half way between the surface and the bed and at the river bed.
Record the measurements on the recording sheet.
5. Discharge To measure discharge you must first have calculated the cross-sectional area using your as above. To calculate the discharge use the formula below:
Discharge (CUMECS) = Cross sectional area (m2) x Mean velocity ms-1
6. Sediment size Sediment carried by the river is called its load. This will vary in size and shape depending on the hardness of the rocks and the time they have been in the river and affected by erosion (attrition).
Sediment can be measured with rulers or calipers.
Measure and record the length of the A, B and C axes (see diagram below).
Calipers for measuring sediment size
7. Sediment shape Particle shape is determined by the rock type (geology) and the length of time erosion has been operating on it. Particle shape is measured by observation. It is therefore somewhat subjective. A sample of sediment is taken and the number of particles of different shapes and of particular roundness is recorded. They can be classified according to their roundness according to the Power’s Scale of Roundness, below:
8. Gradient The gradient is the slope of the channel bed. This is important for river velocity and the flow characteristics of the channel.
To measure gradient take two ranging poles and place them in the channel at a distance of 10 meters apart. Use a clinometers to measure the angle between them.
Measure the angle three times and calculate an average to avoid measurement errors.