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Soil profile
A vertical section of soil divided into layers (horizons) according to physical & chemical characteristics
The 5 layers of soil profile
O (humus on organic) →undecomposed litter
A (topsoil) = mixed mineral - organic
E (eluviated horizon)
B (subsoil / illuvial horizon)
C (parent material)
R (bedrock)
Why is soil important?
Most good stuff tar humans is grown in soil
Provides nutrients for producers
Habitat for many organisms
Filters & stores water
Part of nutrient cycle
Provides raw materials - peat, sand, day, etc.
Soil storages
Include;
organic matter
Organisms
Nutrients
Minerals
Air and water
Soil flows:
Include;
precipitation
Irrigation
Infiltration
Overland & groundwater flow
Evaporation
Ploughing /aerating
Flooding
Draining
Weathering
Leaching
Decomposition
Mixing
Erosion
Soil forming
Soil is considered a non-renewable resources due to the long time it takes to develop -succession
Processes involve;
Gains & losses of material to and from the profile
Movement of water between the horizons
Chemical transformations with each horizon
Chemical transformations of soil-forming
Decomposition → changes leaf litter into humus - overtime humus decomposes due to mineralisation, releasing nitrogenous compounds
Weathering
Biological mixing & nutrient cycling
Translocation & leaching → water dissolves materials & carries it downwards (mostly)
Deposition of materials →organic & inorganic
Sail structures →3 particles
Sand (largest) → falls apart easily
Slit → feels slippery & holds together
Clay (smallest) → feels thick & sticky & can form into shapes
Soil texture
The shape and arrangement of individual sail particles
→ is determined by the proportion of the particles present in the soil
Loam
The well-balanced soil with fairly equal portions of each particle.
→ ideal for cultivation (= growing plants)
Soil porosity
The amount of space between each soil particle
Greater porosity = greater water retention
Soil permeability
The ability of air and water to flow from upper layers to lower layers.
Large pore space = faster vale of drainage
The surface area of soil
Determines the amount of water and minerals that can be retained against the force of gravity.
Smaller particles = higher surface area to volume ratio = more water & nutrients retained.
Workability
How much force it takes to pull a slough through the soil. Soils with more clay are more difficult to work/plough
→ soils are ranked light (easy), medium, or heavy (difficult)
Primary productivity of soil depends on:
Mineral content
Air space (porosity)
Drainage (permeability)
Water-holding capacity
Biota (organic material)
Potential to hold organic material
Causes of unsustainable food production
Increase in world population
A shift in diet (away from grains, towards animal products)
Increase in human urbanisation (limiting available arable land)
Degradation of soil
Sustainable good production is influenced by:
Scale
Mechanisation
Fossil fuel use
Seed / crop / livestock choice → native on not
Water use
Fertilisers
Pest control
Pollinators
Antibiotics
Legislation
Levels of commercial vs substances food production
Inequalities in Global food Supply
Exist in food production and distribution around the world
¾ of the human population does not get enough food
1/6 of the population is going hungry
People in LEDCs make up the majority of those people
MEDCs have a surplus of food
Subsidizing
Farmers are paid to let their feed vest
Import tariffs
Makes it harder for LEDCs to sell their food
Export subsidies
Provided by MEDCs to their farmers make farm products from LEDCs uncompetitive
Differing reasons for good waste between MEDCs and LEDCs
LEDCs;
Poor agricultural practices → choosing the wrong thing to grow
Inadequate roadway/railways to transport food
Poor storage facilities
MEDCs;
Sell-by dates at supermarkets
Buy - one - get-one free promotions at supermarkets
Western demand for perfect looking lead
Influences over food production
Cultural significance
Economic factors
Ecological factors
Shifting cultivation
Slash and Burn → an example of extensive subsistence farming. Worked well when population density was low
Commercial farming
Farming to sell
Subsistence farming
Farming to survive
Intensive farming
Farming to compact- many things in a small area
Extensive farming
Farming in a Lange area
Efficiency of food production
We get a lot more from producers than consumers but we need different demands from each
Models
Farm inputs→ machinery, tractors, cows, seeds, slurry, fertilisers
Farm processes → milking cows, spreading slurry, feed animals, ploughing
Farm outputs → beef, pork, milk, eggs, profits
Environmental impacts of feel production systems
Soil degradation from erosion
Desertification
Eutrophication
Pollution from pesticide, and fertilisers
Salination from over-irrigation
Lowered water tables
Loss of valuable habitats
Disease epidemic from increasing density
Ways to increase sustainability
Reduce meat consumption
Increase consumption of seasonal & locally grown products
Increase consumption of sustainably grown products
Plant buffer zones
Improve accuracy of food labels
Improve standards and practices for food production → which is monitored & controlled by governments
Soil degradation
Change through succession. Fertile soil contains a community of organisms that work to maintain functioning nutrient cycles and are resistant to sail erosion
Reduction of soil fertility due to human interaction
Deforestation
Intensive grazing
Urbanisation
Irrigation → when there is too much
Monoculture
Commercial food production
Results of reduced fertility
Soil erosion
Toxification
salination
Desertification
Soil conservation
To limit/ prevent erosion;
Reduce water & wind erosion → physical barriers, contour ploughing, cover crops, minimise tillage/ploughing, mixed cropping
Nutrient management → crop rotation/animal rotation, crop selection (plant native crops), soil conditions/chemicals, mulching, reduce evaporation