Some students were studying how the characteristics of a river change downstream. They decided to focus their fieldwork investigation on a local river to see if it had some characteristics of a text book example. These characteristics are shown in Fig. 8 (Insert). The students agreed to investigate two hypotheses: Hypothesis 1: The width, depth and cross-sectional area of the river increase downstream. Hypothesis 2: Velocity is greater where the river is deeper.
- (a)(i)The students wanted to take measurements at six study sites along the river. Suggest why it was important that they took all their measurements on one day.[1]
- (a)(ii)Suggest two other things they had to consider in choosing their investigation sites.[2]
- (a)(iii)In preparation they visited a local stream to do a pilot study. Give two advantages of doing a pilot study.[2]
- (b)(i)The students measured the width of the river channel and the depth of the river at points across the channel. They used the following equipment: : tape measure or rope, metre rule or 30 cm ruler. Describe how the students would make their measurements.[3]
- (b)(ii)Having made their measurements and recorded them, the students drew a cross-section of the river channel at each site. The cross-section at Site 1 is shown in Fig. 9 (Insert). The results of measurements made at Site 4 are shown in Table 3 below. Table 3 Distance from left bank (m) 0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 1.6 1.8 2.0 2.2 Depth (m) 0.02 0.08 0.12 0.15 0.22 0.28 0.32 0.38 0.46 0.50 0.46 0.41 Distance from 2.4 2.6 2.8 3.0 3.2 3.4 3.6 3.8 4.0 4.2 4.4 left bank (m) Depth (m) 0.37 0.34 0.28 0.21 0.18 0.16 0.12 0.08 0.06 0.05 0.01 Use the results shown in Table 3 to add the following information to Fig. 10 opposite: • complete the cross-section of the channel, • shade in the cross-sectional area of the river channel.[3]
- (b)(iii)The students also calculated the cross-sectional area of the channel at each site. Their calculation for Site 1 is shown below. Calculation of cross-sectional area at Site 1 Cross-sectional area = width of river (metres) × average depth of river (metres) = 2.6 x 0.14 = 0.36 sq metres The width of the river at Site 4 was 4.4 metres and the average depth was 0.23 metres. Using this data calculate the cross-sectional area at Site 4 below. Calculation of cross-sectional area at Site 4 Cross-sectional area width of river (metres) x average depth of river (metres)[2]
- (b)(iv)Describe two differences between the cross-sections at Sites 1 shown in Fig. 9 (Insert) and Site 4 shown in Fig. 10.[2]
- (b)(v)The summary table of measurements made at the six sites is shown in Table 4 below. Insert your answer from (b)(iii) into the table. Table 4 Site | Distance from source (km) | Width of river (m) | Average depth (m) | Cross-sectional area (sqm) 1 | 2.60 | 2.6 | 0.14 | 0.36 2 | 6.00 | 3.1 | 0.16 | 0.50 3 | 11.40 | 3.6 | 0.20 | 0.72 4 | 14.60 | 4.4 | 0.23 | 5 | 16.40 | 4.4 | 0.27 | 1.19 6 | 22.00 | 7.3 | 0.25 | 1.83 Do these results agree with Hypothesis 1: The width, depth and cross-sectional area of the river increase downstream? Identify a result that does not fit the general pattern.[2]
- (c)(i)Choose one of these methods and describe how the students would do the investigation.[3]
- (c)(ii)For the method which you did not choose, give one advantage and one disadvantage of this method.[2]
- (c)(iii)The students' results are shown in Table 5 below. Table 5 Study site | Average depth (m) | Average velocity (metres per second) 1 | 0.14 | 0.44 2 | 0.16 | 0.51 3 | 0.20 | 0.60 4 | 0.23 | 0.62 5 | 0.27 | 1.20 6 | 0.25 | 1.30 The students plotted these results on a scatter graph, Fig. 11 below. Complete Fig. 11 by adding the results for sites 5 and 6.[2]
- (c)(iv)To what extent do you agree with Hypothesis 2: Velocity is greater where the river is deeper? Use the information in Fig. 11 to help you to answer.[3]
- (d)Whilst making their measurements, one observant student noticed how the river valley was different at the six sites. How could the student record these differences during fieldwork?[3]
This question uses a diagram from the original paper, which isn't shown here. Open the full paper from the past papers archive to see it.
Mark scheme
Marking points from the official mark scheme (Oct/Nov 2010). The mark or mark type is shown in brackets.
- [1] (a) (i) To ensure consistency of results. River conditions may change from one day to next. No variation in the river / to keep the river the same. Weather conditions may change.
- [2] (a) (ii) Accessibility from road / school (Access must be qualified). Safety - e.g.; strong current (Safety must be qualified). Equally distant from other investigation sites. Away from human impact which may affect results. 2 @1 = 2
- [2] (a) (iii) Practise fieldwork techniques. Test equipment. Agree methodology to ensure consistency / get the right idea. 2 @ 1 = 2
- [3] (b) (i) Max 2 for either width or depth; Stretch measuring tape / rope across channel from one bank to the other. Measure across the rope using the tape measure. Use rule / ruler to measure depth of river. Rest rule / ruler on river bed. Measure at regular intervals across river (every 20cm). Record measurement in metres. 3 @ 1 = 3
- [3] (b) (ii) Completion of cross-section (2 marks) (2 at 0.46; 2.2 at 0.41). Tolerance for 2 is 0.45 to 0.47; tolerance for 2.2 is 0.42 to below 0.4. Shade in cross-sectional area (1 mark). (2 @ 1) + 1 = 3
- [2] (b) (iii) 4.4 x 0.23 Figures must be these as they are given (Can reverse); = 1.01 / or 1.012 sq metres (must have sq. metres or m2). 1 mark for knowing method; 1 mark for correct answer. No other figures are acceptable for either mark. 1+1=2
- [2] (b) (iv) Must be clear which site/figure referring to; if not = 0. (Site 1 = Fig 2; Site 4 = Fig 3). Differences must be comparative. Cross section at Site 1 is more uneven /irregular / Site 4 is smoother; Smaller cross-sectional area at Site 1 / larger at Site 4. Cross-section is wider at Site 4 / narrower at Site 1; Cross-section is deeper at Site 4 / shallower at Site 1; 2 @ 1 = 2
- [2] (b) (v) Can be given the anomaly mark here even if disagree with hypothesis; True/agree for width and cross-sectional area (1) Tick HA Reserve mark; Site 5 or 6 is an anomaly for depth / does not fit general pattern (1); Width stays same between Sites 4/5 (1); 1+1=2
- [3] (c) (i) Flow meter: put flow meter below surface/in river (Not on river); Propeller must be facing upstream; Record / read / take reading; Calculate average; OR; Floats & stopwatch: measure set distance between two points along river. Float orange / dog biscuit and time over distance. Repeat several times across river and calculate average. Calculate velocity by dividing distance by average time. 3 @ 1 = 3
- [2] (c) (ii) If method chosen is same as (i) NO MARKS – be careful to check!; Flow meter: Advantage - accuracy of reading / digital reading / quicker; Disadvantage – expensive / less accurate in low flow conditions / battery may go flat / less easy to buy; OR; Floats & stopwatch: Advantage - cheap / no specialised equipment needed; Disadvantage – less accurate / takes longer / need to do calculation of velocity / floats affected by wind or vegetation / only measures surface velocity; 1+1=2
- [2] (c) (iii) Plotting points on scatter graph; no tolerance; Site 5 = 0.27 at 1.2; Site 6 = 0.25 at 1.3 - must be in the square; 2 @ 1 = 2
- [3] (c) (iv) Hypothesis 2 is true/mostly or partially true/agree = Tick HA (1). No marks at all if say it is untrue/disagree = X HA. Give 1 for evidence to support Hypothesis and 1 for anomaly. Agree / Velocity does increase with depth (1) at Sites 1-4 / overall (1) or data evidence (1). Anomaly mark (1 max); But velocity at sites 5 & 6 is much greater than would be suggested by graph (1); But river is deeper at site 5 than site 6 but velocity is greater at site 6 (1); 1+1+1=3
- [3] (d) Sketches of six sites; Photographs of six sites; Annotations to show changing landscape of valley; Measure and record gradient of the bed; Measure cross-profile at the six sites; Describe changes in vegetation DO NOT CREDIT refs to rocks/soil; Describe differences in human activity in the valley; Record dimensions on paper / in a table / make notes (NOT draw graphs during fieldwork). 3 @ 1= 3
Write your answer and get it marked
On Oracle Prep you can write or photograph your own answer and have it marked by AI against this mark scheme, with feedback on what you missed.
Sign up free →