Soil Profiles (SL IB Environmental Systems & Societies (ESS))

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Alistair

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Alistair

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Biology & Environmental Systems and Societies

Soil Profiles

  • Soil profiles provide a visual representation of the different layers or horizons present in a soil system
    • These horizons reflect the processes and materials that have shaped the soil over time
    • There are six main horizons

5-1-1-soil-profile

A soil profile is a visual representation of the different horizons present in a soil system

O horizon

  • The O horizon, also known as the organic horizon, is the uppermost layer
    • It is composed mainly of organic matter such as leaf litter, decaying plant material, and organic debris
    • It is rich in nutrients and serves as a site for nutrient cycling and organic material decomposition

A horizon

  • The A horizon, also called the topsoil, is a mixed mineral and organic horizon
    • It is usually darker in colour due to the accumulation of organic matter
    • This layer is important for plant growth as it contains nutrients and provides a favourable environment for root development

E horizon

  • The E horizon, also known as the eluvial or leached horizon, is characterised by the leaching or removal of minerals and nutrients due to downward movement of water
    • It often appears lighter in colour than the surrounding horizons

B horizon

  • The B horizon, also called the illuvial or deposited horizon, is the layer where minerals and nutrients leached from the upper horizons accumulate
    • It often exhibits different colours, textures, or chemical properties compared to the horizons above and below it

C horizon

  • The C horizon represents the weathered parent material from which the soil has formed
    • It is typically composed of partially weathered rock fragments and may contain limited organic matter
    • The properties of the C horizon influence the development and characteristics of the upper horizons

R horizon

  • The R horizon, also known as bedrock, is the underlying solid rock that forms the base of the soil profile
    • It is often unweathered
    • It is relatively unaffected by biological activity and represents the original geological material from which the soil formed

  • These layered horizons in a soil profile provide information about the soil's composition, nutrient content, water-holding capacity, and drainage characteristics
  • They help scientists, farmers, and land managers understand the properties and fertility of soils, enabling them to make informed decisions regarding land use, crop selection, and soil conservation practices

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Alistair

Author: Alistair

Alistair graduated from Oxford University with a degree in Biological Sciences. He has taught GCSE/IGCSE Biology, as well as Biology and Environmental Systems & Societies for the International Baccalaureate Diploma Programme. While teaching in Oxford, Alistair completed his MA Education as Head of Department for Environmental Systems & Societies. Alistair has continued to pursue his interests in ecology and environmental science, recently gaining an MSc in Wildlife Biology & Conservation with Edinburgh Napier University.