Lecture 1 Flashcards

1
Q

What is detachment?

A

separation of soil particle from soil mass.

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2
Q

What is entrainment?

A

Transport of detach particles from the soil surface to a fluid flow. (wind, water, ice).

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3
Q

Transport

A

Transportation of sediment

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4
Q

Disposition

A

transfer of sediment from the sediment lobe to the soil surface.

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5
Q

Definition of shear stress

A

Shear stress is when the direction of stress/force is parallel to the affected surface as opposed to perpendicular

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6
Q

Small impoundments

A

Reduce sediment movement from landscape.
Occurs naturally and constructed.
Almost no transport capacity

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7
Q

What can reduce the erosivity of wind?

A

Vegetation cover, surface roughness reduce erosivity

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8
Q

Three modes of wind transportation

A

1 creep
2 Saltation
3 suspension

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9
Q

jihih

A

bnbn

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10
Q

Infiltration capacity

A

Soils capacity to hold water

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11
Q

Material strength

A

resistance to stress

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12
Q

Types of erosion differentiated on the basis of:

A
  • Location (hillslope, channel erosion)

* Agent (water, wind(deflation), ice(glacier erosion is called denudation)

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13
Q

What cases soil aggregation?

A

Attractive forces among soil particles, (some particles binds stronger than other, the space between aggregate creates pore space for air or water)

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14
Q

Soil permeability

A

Is a measure indicating the capacity of the soil to allow fluids to pass through it.

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15
Q

Erosivity

A

Erosivity is the term used to describe the potential of raindrop impact, runoff from snowmelt, or water applied with an irrigation system rainstorm to detach and erode soil.

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16
Q

Temporal and spatial variability

A

Wetting, drying, freezing, thawing, addition of organic matter

17
Q

Primary factors that influences soil erosin

A

1 Climate
2 Topography
3 Land use and landcover

18
Q

Erodibility

A

The susceptibility of the ground(soil) surface to erosion.

19
Q

Erosivity isn’t always directly related to rainfall amount, aspects to consider

A
  • Spatial variation

- Temporal variation

20
Q

water erosion consist of 3 processes

A

1 detachment
2 transport
3 deposition

21
Q

How to classify soil erosion?

A

You can classify by agent causing erosion –> water, wind

22
Q

Wind abrasion

A

the impact of particles carried by the wind. The wind picks up particles and moves them. When the particles collide with a solid object, the impact causes small pieces of the object to break off.

23
Q

The three processes of wind erosion

A

creep,
saltation
suspension.

24
Q

Mechanical movement of soil

A

Tillage – Tillage lift soil layer, gravity cases downslope movement.
Mass movement – rainfall saturates (mättar) the upper soil layer and reduce soil strength.

25
Q

Deposition occurs when and where…

A

the sediment load si greater than the wind’s capacity

26
Q

Interill + rill areas = overland flow areas of landscape, caused by:

A

Hortonian flow/Horton overland flow which is infiltration capacity + depression storage capacity.

27
Q

Open channels

A

An open channel has free-water surface exposed to atmospheric pressure. Open channels occurs in in rills, streams and gully’s.

28
Q

Pipe flow

A

Pipe flow fills the conduit with water that flows under the hydraulic pressure. (water frequently flows through the soil just below the surface. The soil may contain macropores, other small openings and channels left by for example decaying roots, burrowing insects and animals. These internal open spaces in the soil may become pipes, and pipe flow can erode flow, causing a type of erosion know as piping.

29
Q

Sheet erosion

A

Sheet erosion occurs as a shallow ‘sheet’ of water flowing over the ground surface, which is a uniform to remove removal of soil from surface, is assumed to be the first phase of the erosion process.

30
Q

Catchment sediment yield

A

= the amount of sediment delivered at the outlet of the catchment

31
Q

irrigation

A

Irrigation water is applied to the land by overhead by sprinklers or small pipes, surface applied flow.

32
Q

Does all drops move sediment?

A

No if it’s already water on the ground that’s 3 times deeper than the size of the drop there is no impact.

33
Q

Small impoundments (reservoirs)

A

Reduce sediment movement from landscape
Natural and constructed
Almost no sediment transport