self-contained, closed systems (as most sediment movement is contained within the cell
How many sediment cells are there around the English and Welsh coastline?
11
they are divided into sub-cells where the inputs, transfers, stores and outputs within the system can be identified
What are sources of sediment?
cliff erosion
eroding beaches
eroding spits
eroding wave cut platforms
fluvial sediment
eroding spits
What are sources?
locations where sediment is generated
What are transfers?
locations where sediment is moving alongshore through longshore drift and offshore currents
What are sinks?
locations where the dominant process is deposition and depositional landforms are created such as spits and offshore bars
What is the sediment budget?
the amount of sediment available to the sediment cell
What are permanent stores?
estuary
dredging
offshore bars
What are temporary stores?
beaches
dunes
spits
Why are beaches, dunes and spits temporary stores/sinks?
as over time the sub-sinks will erode and the sediment will re-enter the cell's system
the sediment cell will produce depositional features which are in equilibrium with the amount of sediment available (sediment budget)
what occurs if the sediment budget is decreased?
the waves will continue to move sediment causing erosion in some areas???
what occurs if the sediment budget is increased?
more deposition is likely
what effect do groynes have on sediment cells?
groynes block the movement of sediment, which can lead to beach erosion further downdrift
there is less sediment to protect against erosion
why are groynes used?
to trap sediment in areas where a beach is considered essential either for leisure or the protection of cliffs
this causes terminal groyne syndrome: causes sediment build up on one side of the groyne, but starves an area of sediment on the other side making it more vulnerable to erosional processes
what is the effect of dams on sediment cells?
reduce the volume of fluvial sediment entering the coastal system
the coastal system is a complex and dynamic system which will adapt according to wave energy levels and sediment supply
a change in one part of the system causes the whole system to work to compensate for the change to achieve equilibrium
sediment is constantly generated in the source region and deposited in the sink region
dynamic equilibrium is reached when inputs of sediment from the source region are balanced by the amount being deposited in the sinks