High Quality Content by WIKIPEDIA articles! The Hjulstrom curve, named after Filip Hjulstrom (1902–1982), is a graph used by hydrologists to determine whether a river will erode, transport, or deposit sediment. The graph takes sediment size and channel velocity into account. The x-axis shows the size of the particles in mm. The y-axis shows the velocity of the river in cm/s. The three lines on the diagram show when different sized particles will be deposited, transported or eroded. The curve uses a double logarithmic scale. It shows several key ideas about the relationships between erosion, transportation and deposition.

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