Chapter 5: Soil Systems and Society Flashcards
(33 cards)
Soil
The upper layer of Earth, made up of organic matter, minerals, nutrients, gases, liquids, living organisms, sand, clay, silt
Why is soil important?
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.
Where does soil come from
Weathering
- physical: freeze; water; wind
- chemical
- biological: plants
Levels of soil
Humus (or organic topsoil) Eluviated horizon Subsoil Parent material Bedrock
How does soil form?
Very slow process:
- Weathering of rock (mechanical)
- Deposition of sediments by erosion (mechanical)
- Decomposition of organic matter (chemical)
Soil system
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.
Cycles
Nitrogen and carbon cycles.
Soil diagrams
Triangle diagram showing soil texture based on particles. Can determine how much clay, silt and sand is in the soil.
Soil permeability
The rate at which air and water can flow through the layers of soil.
Soil porosity
The space between the soil particles.
Different soil permeabilities and porosities.
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
Acidification of soil
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
Soil sustainability
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
Commercial agriculture
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
Substinence agriculture
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
Pastoral farming
Raising animals on grass and land not suitable for crops suitable for crops
Arable farming
Growing crops on good soil to eat directly or feed to animals
Mixed farming
Crops and animals
Animal waste used to fertilize crops
Crops used to feed animal
Farming systems in detail
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
Extensive vs. Intensive farming
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.
Terrestial vs. aquatic
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)
Soil degradation
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.
Soil erosion
Movement of soil, especially surface litter and topsoil
Two main agents of erosion
- Wind
- Flowing Water
Sheet wash
Large areas of surface soil are washed away during heaving rain.
Can include landslides