Topic 6- Rivers Flashcards
Main hypothesis
Width, depth, discharge and velocity will increase travelling downstream from the source
Flood risk for a site around the river will be greater if there is:
More development
Steeper slopes
Impermeable geology
Method
Sampling strategy (stratified) Picked own points so we could access all of them and get better results
Quantitative - primary
Measurements fo width and depth (systematic intervals)
- metre ruler, tape measure
Cross sectional area =
Width x depth
Quantitative - primary
Measurement of velocity using hydroprop impeller
- at 3 points across the river (to get an average)
Discharge=
Cross sectional area x velocity
Qualitative
field sketch to show main features of both sites and to identify anything that might increase flood risk
Secondary data (3)
Flood risk map
Geology map
Land use map
Flood risk map
Small area of flood risk compared to the river wey
Slight greater area of land at risk around gomshall
Geology
Majority of catchment is permeable so low risk
Land use map
Catchment is mainly woodland so low risk
Patches of urban areas e.g gomshall
- this would then increase flood risk
Data presentation and analysis
Scatter graph
Field sketch
Field sketch
Cross ways farm - less built up
-less flooding
Baigner hammer - surrounded by main street
- more flooding
Conclusion
Discharge and velocity
They will increase- proven from scatter graph
Conclusion
Flood risk for a site
Will be greater if there is more development, more steeper slopes, more impermeable surfaces
Flood risk greater at abinger hammer - shown by flood risk map as it was more built up shown by land use map and sketch map