Photo 2
There have some tree trunks across the river and there have erosion on the both side.
Photo 3
There have a lot of plants beside the river. This will make the plants luxuriant.
Photo 4
In this site, there is a lot of erosion outside of the meander.
Photo5
This photo show one side of the valley is slumping and the other side is smoothly.
Photo6
There have so many cows on the valley beside the river.
A result table
Channel cross-section
Site name: Caxton
A result table
Channel cross-section
Site name: Toft
A result table of Stream velocity
Site no.1
Site no.2
Result presentation
Results analysis
The average pebble size at each site
The average pebble size of Caxton is 5.06cm
The average pebble size of Toft is 3.89cm
The Average time of velocities result table
Site no.1
Site no.2
A Fieldwork Measurements
Width of channel (cm) 1000
Distance from left bank (cm)
Depth of water
Recorded times for orange over 10 metre distance (in second)
Run: 1 2 3
Time:169 116 161 total: 446 Average time: 148.6
B Discharge Calculations
The stream cross-section is plotted on graph paper (as above) Cross-section area: 160 squares X 23 square cm = 4000 square cm = 4000/10
= 0.4 square
Velocity in per second = 10/148.6 = 0.067m per second
Discharge = 0.067 X 0.4 = 0.0268 cumecs
Average discharge = 0.0268 X 0.8 = 0.02144 cumecs
A Fieldwork Measurements
Width of channel (cm) 1000
Distance from left bank (cm)
Depth of water
Recorded times for orange over 10 metre distance (in second)
Run: 1 2 3
Time:161 166 142 total: 344 Average time: 114.6
B Discharge Calculations
The stream cross-section is plotted on graph paper (as above) Cross-section area: 160 squares X 23 square cm = 4000 square cm = 4000/10
= 0.4 square
Velocity in per second = 10/114.6 = 0.087m per second
Discharge = 0.087 X 0.4 = 0.034 cumecs
Average discharge = 0.034 X 0.8 = 0.027 cumecs
The river changed over the length, it got deeper and wider, also the river moved faster. It is because so much water will need more space to go through the river. The bed load didn’t change anything. The pebbles get rounder and smaller because the current is swift.. The erosion will get more seriously. And there will have more deposition. If the water getting fast, the If the water getting fast, the momentum can make the erosion be serious. More water also will take more deposition. The valley changed from a steep v to a gently sloping one.