Soils Flashcards

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1
Q

Soil function- hydrological buffer

A

regulating water, helps control where rain and snowmelt water goes. Water dissolved solutes flow over land or into soil

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2
Q

Soil function- food, biodiversity and habitat

A

the diversity and productivity of living things on soil

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3
Q

Soil function- nutrient cycling

A

cycling nutrients, carbon, nitrogen and many other nutrients stored

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4
Q

Soil function- filtering and buffering

A

Minerals/microbes are responsible for filtering, buffering and detoxing organic/inorganic materials including industrial by products

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5
Q

Soil function- physical stability and support

A

Soil structure provides a medium for plants/rocks

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6
Q

Zonal soil

A

Take hundreds of years to form and consist of weathered rock, organic material, water and air. A soil which has experienced max effect max effect of the climate+natural vegetation upon the parent rock assuming there are no extremes of weathering relief or damage

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7
Q

Horizons

A

(layers) that are distinguishable from the initial material as a result of additions, losses, transfers

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8
Q

Soil

A

Soil is made up of a mixture of soils e.g. organic matter, liquids and gases that occur on the land surface.

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9
Q

Humus (O)

A

It is a thin layer of rotting vegetation- such as grass and leaves. The nutrients in it return to the soil

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10
Q

Topsoil (A)

A

This layer is rich in humus, and the minerals from the rock- so good for growing crops

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11
Q

Subsoil (B)

A

It has little humus but it is rich in minerals and tree roots reach this layer

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12
Q

Rock being weathered (C)

A

It has been broken down into chunks and there is little sign of life

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13
Q

Bedrock (D)

A

Solid rock, not yet weathered but will one day

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14
Q

Water erosion- river bank erosion

A

Soil washed away by unmanaged rivers as they meander floodplains

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15
Q

Water erosion- gully erosion

A

If rills are unattended to grow into gullies affected land cant be used for growing crops- hazard for machinery

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16
Q

Water erosion- rill erosion

A

they are short-lived streams water can gather on surface/run downhill forming channels of water

17
Q

Water erosion- sheet erosion

A

Overflow can transport topsoil in a uniform fashion

18
Q

Wind erosion- saltation

A

Main process of soil transportation suspended particles are lifted by wind then fall back to ground so they bounce/hop along surface

19
Q

Wind erosion- creep

A

Movement occurs when particles are usually top heavy to be lifted by wind

20
Q

Wind erosion- suspension

A

Small particles that have been lifted into the air remain suspended as dust and taken away

21
Q

Wind erosion- abrasion/attrition

A

Suspended particles cause abrasion of soil surface when fall back to ground. Also hit into other particles and break away

22
Q

Repeated erosion reduces fertility of soil by:

A

Removal of topsoil
Reduction in depth of soil
Reducing infiltration
This leads to loss of seeds, fertilisers and pesticides and increased difficulty of field operations

23
Q

Impacts of soil erosion- damage to environment

A

Leads to deposition of sediment onto roads and neighbouring lands, damage to qual of water resources and sediment in rivers damaging spawning grounds

24
Q

Wind erosion control measures:

A

Increasing soil cohesion by applying organic matter to soil, increasing roughness of soil surface and increasing plant cover so that surface wind spread will be cut

25
Q

Salinization

A

It is a build up of salts in soil, eventually leading to toxic levels for plants. Rainwater also contains some salts ad evap of this water from the dry surface leaves the salts behind. Likely to become a prob on soils where the groundwater is within 3m or less of surface- in such cases water rises to surface by capillary action rather than percolating down through soil profile. Affected farmland of this prob globally is up to 20%

26
Q

Granular and crumb structures

A

Individual particles of sand, silt and clay grouped together in small nearly spherical grains. Water circulates very easily through this soil and found in topsoil profile

27
Q

Blocky structures

A

Soil particles that sling together in nearly square blocks. Relatively large blocks indicates that the soil resists penetration and movement of water. Commonly found in lower parts of soil where clay has accumulated

28
Q

Prismatic and columnar structures

A

Soil particles which have formed into vertical columns or pillars separated by vertical cracks. Water circulates with great difficulty.

29
Q

Platy structures

A

Made up of soil particles aggregated in thin plates or sheets piled horizontally on one another. Plates often overlap, greatly impairing water circulation. Commonly found in forests and high latitude soils.

30
Q

Gleying

A

Process of soil formation when conditions are waterlogged. Pore spaces is filled with water and become de-oxygenised

31
Q

Solutions to soil erosion

A

Fertilizers- increase nutrients and organic encourage soil organisms and improve retention.
Afforestation- stabilises the soil and organic matter is returned through leaf litter
Farming practices- crop rotation replenishes nutrients, replacing hedge grows to reduce wind erosion, ploughing across slopes to prevent gullying and having controlled grazing

32
Q

Soil structure

A

Manner in which individual particles aggregate together, called peds. The shape and alignment determine the pore spaces which water, air and roots penetrate

33
Q

Soil degradation is caused by:

A

over- cultivation and compaction which reduces the infiltration and water flows as surface run off leading to erosion

34
Q

Latosol- Tropical climate

A

Acidic and infertile. Found in hot/wet areas and the climate zone is humid without seasons. There is nutrient rich material but once vegetation is removed this deteriorates. There is a rapid nutrient cycle and is high in biodiversity, so if the forest is cleared and the humus is removed nutrients are lost through leaching or soil erosion. These areas get cleared for logging, settlements and crops

35
Q

Podsol

A

Subarctic areas such as N.A/Europe between tundra and grasslands. Harsh winters and cool summers restrict growth. Poor nutrient cycle and acid humus due to the pine needles being low in nutrients. clear difference between horizons . Coniferous trees can shelter the soil- water can infiltrate and percolate. Human uses include sheep farming and logging.