Largest soil particle [0.005− 2 mm], highest porosity, poor water retention
Silt
Particle size between sand and clay, porosity and water retention between the two
Loam soil
Combination of the three soil types, ideal for agriculture due to high porosity, high water and nutrient retention, and easy aeration
Soil texture triangle
Demonstrates any combination from the soil types
Humus
An essential component of most fertile soils, made from living and decaying organic matter
Soil profile layers
OrganicLayer
Topsoil
Subsoil
ParentMaterial
Bedrock
Organic Layer (O-Horizon)
Dark colour due to humus, most easily eroded
Topsoil (A Horizon)
Dark appearance due to humus, soft, porous, retains more water
Subsoil (B Horizon)
Contains clay and mineral deposits, less organic material, harder, more compact, lighter in colour
ParentMaterial (C-Horizon)
Lumps of rocks with cracks and crevices, also known as regolith
Bedrock (R-Horizon)
Extremely hard, rocky composition, not considered a soil layer
Soil quality
How well soil does what we want it to do, sustain plant and animal life, maintain/enhance water and air quality, support human health and habitation
Imperativequalitiesforsoil
Arable for agriculture
Regulation of water and filtering of potential pollutants
Nutrient cycling
Foundation and support
Mineral deposits
Afforestation
Planting or adding of trees in an area where there was never a forest or plantation, to create a new forest
Reforestation
Replanting of trees in an area where there was once a forest which was destroyed or damaged
Exogenic processes
Geological phenomena and processes originating externally to the Earth's surface, driven by solar energy and other external influences, shaping landforms created from endogenic processes
Exogenicprocesses
Weathering
Erosion
Deposition
Endogenic processes
Geological phenomena and processes originating within the Earth's surface, responsible for tectonic changes on the surface by releasing energy from within