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Dynamics of Moving Water

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... the first type of erosion is splash erosion. Raindrop impacts reduce infiltration rate because the soil particles become more compacted movement of material ... – PowerPoint PPT presentation

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Title: Dynamics of Moving Water


1
Dynamics of Moving Water
CGF3M
2
Dynamics of Moving Water
  • The Hydrosphere
  • Hydrologic Cycle
  • Infiltration
  • Runoff
  • Stream Flow
  • Velocity
  • Discharge
  • Flow

3
Hydrologic Cycle
Condensation Precipitation Infiltration Runoff Eva
poration
4
Hydrologic Cycle
  • Infiltration precipitation that seeps into the
    ground.
  • Factors affecting infiltration
  • Interparticle size the size and connectedness
    of the particles in the ground, eg., sand vs clay
  • Vegetation (associated organisms) loosen the
    soil.
  • Rainfall intensity
  • Seasonal factors, eg., freezing of the ground
  • Permafrost is there any, its depth
  • Urban landscape - paving, buildings, etc.

5
Hydrologic Cycle
  • Infiltration cont
  • When rain falls, the first type of erosion is
    splash erosion.
  • Raindrop impacts reduce infiltration rate because
    the soil particles become more compacted

movement of material downhill.
6
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7
Hydrologic Cycle
  • Runoff flow of water from the land as both
    surface and subsurface discharge.
  • Occurs when rate of precipitation is greater than
    rate of infiltration.
  • Usefulness recreational, sewage disposal,
    domestic, irrigation, food source, hydroelectric
    power, etc.

8
Hydrologic Cycle
  • Runoff Categories
  • Surface Runoff/Overland flow
  • excessive overland flow can lead to sheet erosion
    forming small rills or tiny rivers.
  • can include Channel Flow (water traveling in a
    river or stream).
  • Subsurface Runoff/Ground Water
  • travels beneath the surface towards a body of
    water.

9
Stream Flow
  • The velocity (speed) of flow in a river is
    controlled by
  • Gradient
  • Friction due to resistance of water on the bed of
    the channel.
  • Volume

10
Stream Flow
  • Discharge volume of water that flows past a
    given point can be determined by the following
    factors
  • Q A x V
  • Q is discharge
  • A is cross-sectional area of stream
  • V is mean velocity (in m3/sec usually)

11
Stream Flow
  • Load ability of a stream to carry load of solid
    material varies with discharge, velocity and
    particle size.

12
The End!
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