5.1.1 Soil is a dynamic system within the larger ecosystem that has its own inputs, outputs, storages and flows.
5.1.2 Soil is made up of inorganic and organic components, water and air.
5.1.3 Soils develop a stable, layered structure known as a profile made up of several horizons, produced by interactions within the system over long periods of time.
5.1.4 Soil system inputs include those from dead organic matter and inorganic minerals.
5.1.5 Soil system outputs include losses of dead organic matter due to decomposition, losses of mineral components and loss of energy due to heat loss.
5.1.6 Transfers occur across soil horizons, into and out of soils.
5.1.7 Transformations within soils can change the components or the whole soil system.
5.1.8 Systems flow diagrams show flows into, out of and within the soil ecosystem.
5.1.9 Soils provide the foundation of terrestrial ecosystems as a medium for plant growth (a seed bank, a store of water and almost all essential plant nutrients).
5.1.10 Soils contribute to biodiversity by providing a habitat and a niche for many species.
5.1.11 Soils have an important role in the recycling of elements as a part of biogeochemical cycles.
5.1.12 Soil texture defines the physical make-up of the mineral soil.
5.1.13 Soil texture affects primary productivity through the differing influences of sand, silt, clay and dead organic matter, including humus.
5.1.14 Soils can act as carbon sinks, stores or sources, depending on the relative rates of input of dead organic matter and decomposition.
5.1.15 Soils are classified and mapped by appearance of the whole soil profile.
5.1.16 Horizons are horizontal strata that are distinctive to the soil type.
5.1.17 The A horizon is the layer of soil just beneath the uppermost organic humus layer, where present.
5.1.18 Factors that influence soil formation include climate, organisms, geomorphology (landscape), geology (parent material) and time.
5.1.19 Differences between soils rich in sand, silt or clay include particle size and chemical properties.
5.1.20 Soil properties can be determined from analysing the sand, silt and clay percentages, percentage organic matter, percentage water, infiltration, bulk density, colour and pH.
5.1.21 Carbon is released from soils as methane or carbon dioxide.
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