River Characteristics Investigation Cross-section - Velocity - Discharge - Gradient - Bedload www.i-study.co.uk Measuring & Calculating the Cross-Section Measuring • Measure the width of the channel, across the surface of the water. • Measure the wetted perimeter (the distance down the banks & across the bed – where water touches land). • Take a metre ruler or ranging pole, stand it upright in the water and measure the depth across the stream at equal intervals (50cm). Quick Calculation A quick method to give an approximate cross-sectional area is to the use the following formular: Average width x Average depth Graphing the cross-section 1. Using graph paper & your field data sheets, decide on a suitable scale. Both axes should be identical in scale. 2. Plot the distance across the stream against depth, just like an ordinary graph. 3. Join the depth points with a flowing line, and shade or colour the land and water. Cross-section of River Site 1 0 50 100 150 200 250 300 350 cm 50 100 depth cm How to calculate the cross-sectional area 1. 2. 3. 4. Using the cross section you have drawn: Add up all the squares above the river bed. What if a square is divided by the bed-line? If it is more than half above the bed-line, include it. If it is more than half below the bed-line, ignore it. Work out what each square is worth in area and add together. www.i-study.co.uk Measuring Flow Velocity 1. 2. 3. 4. 5. 6. Velocity is the speed at which the water is flowing. Measure out a distance of 10 metres, and mark it at either end with a ranging rod. Throw in a float upstream of your first marker. When the float passes the first marker, begin timing its passage downstream When the float passes the second marker, stop timing. Write the time down, and repeat 9 times: -3 times near the left bank -3 times in the centre -3 times near the right bank Calculating Discharge Discharge is the volume of water flowing in a stream at a certain point in time. It’s unit of measurement is cumecs (cubic meters/second) To calculate it use the formular below: Discharge = Cross-sectional Area x Average Velocity Bedload Sampling Take 5 random samples from each site. Collect data on particle size, shape. 1. What is the main type of particle in your sample? • Clay and silt: < 0.075 mm • Sand (Fine, medium & coarse grained) : 0.075 to 4.75 mm • Gravel: 4.75 to 75 mm • Cobbles: 75mm to 300mm • Boulders: > 300mm 2. The measurement of the particle’s long axis. 3. What sort of material is your sample made up of: • is it sedimentary rock, • igneous rock, • organic material etc? 4. Angularity – is your material: • angular, • sub-angular, • sub-rounded or • rounded? www.i-study.co.uk Data Recording Sheet Date: Location: Site No: Cross-section Data Width: Bankfull Width: Distance Depth 1 2 3 4 Intervals: 5 6 7 8 9 Extra depth at bankfull: 10 11 12 13 14 Velocity Data 1 2 3 Average Left Bank Mid-stream Right Bank Gradient: Bedload Sampling Sample Details (long axis, angularity, particle type) 1 2 3 4 5 www.i-study.co.uk
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