physical fieldwork Flashcards
what is our physical fieldwork question
how does the cross section of the river tarrell change as we move downstream?
what makes our question suitable for a geographical enquiry
- able to collect primary and secondary data > can draw conc.
- small-scale > short river so can measure along
- low/manageable risk > shallow
- clearly a geographical question - ab a place and appears in syllabus > can test Bradshaws theory
how was our fieldwork practical in terms of access
- on public land so we can access river
- terrain/landscape is not too challenging to walk
- parts of the river on private land + we have permission to visit so we could access all of the long profile
how was our fieldwork practical in terms of safety
relatively shallow so able to take measurements
how was our fieldwork practical in terms of manageability (scale)
river is relatively short so can measure long profile and see differences
what was good ab the location of the river in terms of geography
able to access river from source to mouth so we could test Bradshaws geographical theories there
what was good ab the location of our river in terms of data
- relatively shallow so easy to measure so data is accurate
- all rivers in uk have secondary data
who was our theorist
bradshaw
what did Bradshaw say
- width should increase downstream
- depth should increase downstream
what were the risks with our fieldwork
- drowning in river
- getting cold from spending day in the field
- getting hit by a car
- accidents in river
what action did we take to minimise risks
- areas where the river was too deep we did not take measurements, working in supervised small groups
- bringing spare clothes and warm layers
- cross at safe locations
- bring a first aid kit + mobile phone
justify measuring the width as one of our methods
we wanted to see how the cross section of the river tarrell changes downstream because Bradshaw suggests that rivers on average get wider and deeper. so we needed to measure the width of 10 places along the long profile to see if this happened.
what was good ab our width method
- easy to use
- portable
- simple (method + equipment)
- cheap
- fast
- can look at past data
what was bad ab our width method
- can be inaccurate:
> current would sometimes pull the tape measure
> vegetation in the way so sometimes hard to find edges
> not measuring from undercut (upper course)
overall judgement of width methodology
fairly reliable and successful method w/ accurate data
justify measuring depth as one of our methods
we wanted to see how the cross section of the river tarrell changes downstream because Bradshaw suggests that rivers on average get wider and deeper. so we needed to measure the depth of 10 places along the long profile to see if this happened.
what was good ab our depth method
- easy to use
- portable
- simple (method + equipment)
- cheap
- fast
- can look at past data
- taking a mean of depth
- ruler can float so doesn’t drift away
what was bad ab our depth method
- ruler would often bend at high current areas so the data was unreliable
- distance between measurements was larger in middle course so data is less accurate
overall judgement on depth methodology
fairly reliable and successful method w/ accurate data
justify our use of stratified sampling
we needed to cover the whole long profile so we had to choose sites in the upper, middle and lower course but some of the river was too difficult to access or too dangerous to get into because it was too deep or fast-flowing so we had to choose our sites to an extent.
what was good ab our use of stratified sampling
- could choose 10 sites that cover the entirety of the long profile so we could avoid any private land or dangerous parts of the river
what was bad ab our use of stratified sampling
- creates a bias as ensuring that it was safe may mean picking shallower sites to take data from which could distort data making our river seem shallower than it is
overall judgement of our sue of stratified sampling
fairly reliable + successful method b/c it allowed us to access the river safely + answered the question
justify our use of secondary data using google earth
enables us to see the long profile of the river and plan the sites to show how the cross-section changes downstream - according to Bradshaw, river width and depth should increase downstream