River Holford field work (paper 3) Flashcards
what is the fieldwork title for this assessment
investigating downstream change on the river Holford
what is your hypothesis for this assessment
- discharge will increase with distance downstream on the river holdford because more tributries join to creater a larger river so more water
- velocity will increase with distance downstream on the river Holford because more water and energy with a bigger channel means less friction so water moves more freely
- cross-section area will increase as we move down stream
how long is the river Holford
8km
describe the geologies of the river Holford in the upper, middle and lower courses
- upper = sandstone
- midde = mudstone
- lower = limestone
explain the advantage of the fieldwork location used for your enquiry
- accessibly - mainroad ~ A39
- we can walk along it - good idea of change in a timely manner ~ small river
- accessable car park
- previous schools hae studied here so it was safe and legal to do so
what was your chosen sampling method
statified = geographical knowledge to choose location (after each tributry)
why was your samplying method appropiate for your enquriy
it is feesable in the timelimit, we know where the river changes and we can locate change at those sites and easily collect data
give two risk assessments and how to avoid them
- slipping/tripping = sensible footwear, follow paths
- drowning = avoid deep fast flowing water, stick to footpaths
what samplying method could have you done instead of stratified
systematic # measurements taken every 1km = less bias and manageable
what was your qualitative method of assessment
we used a field sketch and annotated around the skets to highlight chacteristics of each site (gradient, pepple size, land use)
what were the two quantitive methods of analysis
- cross section area
- velocity of water
explain how cross section area was used to assess river Holford
- we used a tape measure to measure the width from wetted edge to wetted edge
- we divided the width by 10
- we used a meter ruler to measure the depth at the same points, ensuring the thin side faced upstream to reduce splash and inaccuracy
- we then used these measurements to calculate the area by multiplying them together
explain how velocity measurement was used to assess river Holford
- we used a tape measure and divided the width by 3 so we could take 3 readings per site
- we used a flow metre, ensuring the impellor faced upstream
- we timed how long it took the impellor to reach the base and recorded the value
- we then calculated the avergae at each site
how did you ensure reliablility for these measurements taken
- width = pull the tape taught and water to water
- depth = thin end upwards and bottom touching the base of river
- speed = ensure impellor was not touching base and it was facing upstream
explain why the pattern of your results for cross profile may not be completely accurate
we only took 5 measurements along the width and it would be more accurate if we took more as we may of missed a particulary deep or shallow section