Chapter 5: Soil Systems and Society Flashcards

1
Q

Soil

A

The upper layer of Earth, made up of organic matter, minerals, nutrients, gases, liquids, living organisms, sand, clay, silt

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2
Q

Why is soil important?

A

It stores and transfers heat and is not renewable – everything comes from it: clothes, crops, food. Natural resources: diamonds, gold, silver, oil, natural gas (methane).
It is a habitat for many organisms and provides nutrients for producers and filters water.

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3
Q

Where does soil come from

A

Weathering

  • physical: freeze; water; wind
  • chemical
  • biological: plants
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4
Q

Levels of soil

A
Humus (or organic topsoil)
Eluviated horizon
Subsoil
Parent material
Bedrock
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5
Q

How does soil form?

A

Very slow process:

  • Weathering of rock (mechanical)
  • Deposition of sediments by erosion (mechanical)
  • Decomposition of organic matter (chemical)
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6
Q

Soil system

A

Soil systems are dynamic.
Storages: organic matter, organisms, nutrients, minerals, air, and water.
Transfers within the soil: biological mixing, translocation (movement of soil particles in suspension), and leaching (minerals dissolved in water move through soil).
Inputs: organic material including leaf litter and inorganic matter from parent material, precipitation, and energy.
Outputs: Uptake by plants and soil erosion.
Transformations: decomposition, weathering, and nutrient cycling.

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7
Q

Cycles

A

Nitrogen and carbon cycles.

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8
Q

Soil diagrams

A

Triangle diagram showing soil texture based on particles. Can determine how much clay, silt and sand is in the soil.

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9
Q

Soil permeability

A

The rate at which air and water can flow through the layers of soil.

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10
Q

Soil porosity

A

The space between the soil particles.

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11
Q

Different soil permeabilities and porosities.

A

Clay soils – High porosity (micropores), low permeability, high nutrients but inaccessible, low leaching.
Sandy soils – lower porosity (fewer macro), high permeability, high leaching
Loam soils – Best of both, ideal for agriculture

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12
Q

Acidification of soil

A

Acid precipitation increases acidity near urban areas
Clay soils often have high acidity due to absorption of water
Causes leaching of potassium, magnesium and ammonium
Causes aluminum and iron to become more available to plants which are toxic

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13
Q

Soil sustainability

A

Fertile soil is a non-renewable resources
Fertile soil has enough nutrients for healthy growth (N,P,K)
Nutrients are leached from soil by water
Nutrients are lost when crops are harvested
Replace nutrients with fertilizers
More sustainable method of replacing nutrients is by crop rotation, planting legumes and using organic fertilizers

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14
Q

Commercial agriculture

A

large scale production of crops and livestock for sale

Production for profit
Maximizing yield
High level of technology
Monocultures
High inputs of energy
Extensive- more land with lower planting
Intensive – use land more intensively
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15
Q

Substinence agriculture

A

farming for self-sufficiency to grow enough for a family

Production food for family
No surplus
Human and animal labor
Mixed crops
Low inputs of energy
Cash cropping
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16
Q

Pastoral farming

A

Raising animals on grass and land not suitable for crops suitable for crops

17
Q

Arable farming

A

Growing crops on good soil to eat directly or feed to animals

18
Q

Mixed farming

A

Crops and animals
Animal waste used to fertilize crops
Crops used to feed animal

19
Q

Farming systems in detail

A

Inputs – fertilisers, water, pest control, labour, seed etc.
Outputs – food quality, yield, pollutants, transport, processing, packaging etc.
System characteristics – diversity, sustainability etc.
Environmental impacts – pollution, habitat/biodiversity loss, soil erosion/degredation, desertification, disease etc.
Socio-economic factors – Subsistence/commercial, traditional?, local/export, quality/quantity

20
Q

Extensive vs. Intensive farming

A

Intensive Farming is a farming method that uses higher inputs and advanced agricultural techniques to increase the overall yield. In contrast, Extensive Farming is one in which more and more land is brought under cultivation to increase the output produced.

21
Q

Terrestial vs. aquatic

A

Terrestrial is a more efficient use of solar energy (1st/2nd trophic level)
Less solar energy reaches aquatic systems (reflection and absorption by water)
Aquatic often higher trophic level (4+)
Aquatic systems more efficient in terms of passing energy along food chain
More skeletal waste in terrestrial (terrestrial animals need more substantial bones to support themselves on land)

22
Q

Soil degradation

A

Processes that take away the soil (erosion).

  • No or little vegetation on the soil.
  • Wind and water.

Processes that make the soil less suitable for use.

  • Loss of chemicals/nutrients (leaching)
  • Addition of chemicals (pollution)

Generally commercial industrialized food production systems reduce soil fertility more than small-scale subsistence farming.

23
Q

Soil erosion

A

Movement of soil, especially surface litter and topsoil

Two main agents of erosion

  • Wind
  • Flowing Water
24
Q

Sheet wash

A

Large areas of surface soil are washed away during heaving rain.
Can include landslides

25
Q

Gullying

A

Channels develop on hillsides following rainfall.

Over time they get deeper and deeper.

26
Q

Wind erosion

A

Drier soils have the top layers consistently removed

27
Q

HUman activities that lead to soil degradation.

A
Overgrazing
Overcropping
Deforestation
Unsustainable agriculture
Urbanization
28
Q

Monoculture farming

A

Monoculture farming is a form of agriculture that is based on growing only one type of a crop at one time on a specific field. In contrast, a polyculture system assumes that a field is sown with two or more crops at a time

29
Q

The pedosphere

A

The pedosphere is the skin (or the soil cover) of the Earth and only develops when there is a dynamic interaction between the atmosphere (air in and above the soil), biosphere (living organisms), lithosphere (unconsolidated regolith and consolidated bedrock) and the hydrosphere (water in, on and below the soil).

30
Q

The Green Revolution

A

the set of research technology transfer initiatives occurring between 1950 and the late 1960s, that increased agricultural production worldwide.

31
Q

Example of desertification

A

The Sahel Draught (Case study)

32
Q

Transfer within soil profile

A

biological mixing by soil animals/earthworms / leaching / seepage / capillary action / drainage / percolation / infiltration / eluviation / absorption of minerals/water by living organisms.

33
Q

Transformations within soil profile

A

decomposition;
humus formation/humification of organic matter;
weathering of primary minerals/parent rock;
nutrient cycling/nitrogen fixation/nitrification/denitrification/ammonification;
evaporation;
rusting soil.