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11 Cards in this Set

  • Front
  • Back

Movement of soil occurs in 3 stages

- detachment


- movement


- deposition

Types of Water Erosion

- sheet


- rill


- gullies


- streambank


Erosion damage

- soil loss


- texture change


- plant nutrients are removed


- soil is less compact, less fertile


- soil is less permeable


- yields are reduced

Structural Damage

- loss of surface soil results in coarser material overall


- raindrops disintegrate aggregates on the soil surface initiating crust formation


- surface becomes compacted


- soils that experience significant crusting also experience greater amounts of erosion

water erosion: two causes

- falling raindrops


- running water

Features of slope that effect erosiveness

- slope gradient


- slope length


- slope shape

sand

- can be deposited from fast-moving streams

silt

- will settle out in quantities only as the stream's gradient levels off

clay

settles out in significant quantities only when the water is still or when the clay flocculates as the stream enters a body of salt water

Erodibility affected by the following properties

- soil structure


- soil detachability


- permeability


- organic matter


- transportability

Principles to reduce erosion

- reduce raindrop impact on the soil


- reduce runoff volume and velocity


- increase the soil's resistance to erosion