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Coastal Landscapes and Change

Sediment cells: sources, transfers and sinks

  • 3 things to know
  • Paper 1

Overview

Sediment cells and their sources, transfers and sinks, dynamic equilibrium with negative and positive feedback, Portland Bill to Selsey Bill as an example cell, and fieldwork statistics including the Student t-test for pebble size, the Chi-square test for succession zones and an index of diversity.

What you need to know

Answer each one before you reveal it.

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Key term

What are the three components of a sediment cell?

Process

What role do 'transfers' play within a sediment cell?

Key term

Within a sediment cell, what are 'sources'?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is the sediment cell concept in coastal geography?

    Model answer

    The sediment cell concept divides the coast into self-contained units, each with distinct sources, transfers and sinks of sediment, functioning as largely closed systems.

  2. 2

    Within a sediment cell, what are 'sources'?

    Model answer

    Sources are locations where sediment enters the coastal system, such as river inputs, cliff erosion, or offshore sediment supplies.

  3. 3

    What role do 'transfers' play within a sediment cell?

    Model answer

    Transfers are the processes and pathways by which sediment moves through the coastal system, including longshore drift and tidal currents.

  4. 4

    Define 'sinks' in the context of a sediment cell.

    Model answer

    Sinks are locations where sediment accumulates or leaves the system, such as beaches, spits, offshore deposits, or estuaries.

  5. 5

    Why are sediment cells described as 'self-contained' units?

    Model answer

    Because sediment circulates within each cell with minimal exchange between adjacent cells, meaning inputs, movements and outputs occur largely within defined boundaries.

  6. 6

    If cliff erosion increases within a sediment cell, how might this affect the balance of the system?

    Model answer

    Increased cliff erosion adds more sediment to the source component, potentially increasing transfers and accumulation at sinks such as beaches or spits within that cell.

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