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NotesESS HLTopic 5.1Soil as a system
Back to ESS HL Topics
5.1.16 min read

Soil as a system (ESS HL)

IB Environmental Systems and Societies • Unit 5

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Contents

  • Soil as a system at Higher Level
  • Soil is an open system
  • Soil is an ecosystem
  • A dynamic system that varies
  • Exam-style question
Soil as a system at Higher Level: The same system idea as SL, with different real cases: Scotland's Flow Country peat, clover and its nitrogen-fixing bacteria, and the US Corn Belt's lost topsoil. At HL, use the system idea to explain why a soil is building up or running down.

Practise this as you read

  • Sort every process into input, output, storage or flow.
  • Judge whether a soil's inputs or outputs are winning, and why.

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Soil is a system: A system has inputs, outputs, storages and flows. Soil has all four, so it can be studied as a system.

The points to remember

  • Soil is an open system: matter and energy cross its boundary.
  • Inputs: rain, dead leaves and dung, minerals from weathering of rock, gases from the air.
  • Outputs: water lost by evaporation, minerals lost by leaching and erosion, nutrients taken up by plants.
  • Storages: organic matter (humus), minerals and nutrients such as nitrates, water, air.
  • Flows inside the soil: decomposition turns dead matter into nutrients; water moves down the soil.
  • In an answer, name the process and what it moves: 'minerals are lost by leaching', not just 'minerals'.
Remember it as: In, out, kept, moved: inputs, outputs, storages, flows.
Systems diagram of a soil. Inside a dashed boundary: storages of organic matter, soil water, minerals and nutrients, and soil air. Inputs: dead leaves and dung from plants and animals, rain from the atmosphere, weathering of parent rock. Outputs: uptake by roots, evaporation, carbon dioxide from respiration, leaching to groundwater. Inside: decomposition from organic matter to minerals
Arrows across the boundary are inputs and outputs.
Name the thing, then the process: An output to the air is the carbon dioxide or the nitrogen gas, not 'respiration' or 'denitrification' on their own. And an input or output is not a transfer: water seeping down to the B horizon stays inside the soil.

Real example: in Scotland's Flow Country, a huge peat bog, dead moss is added faster than it decays in the wet, airless soil. The storage of peat grows by about 1 mm a year.

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An ecosystem has living and non-living parts that interact. Soil has both, so it is an ecosystem in its own right.

Why soil is an ecosystem

  • Like any ecosystem, soil has biotic parts: bacteria, fungi, earthworms, insects, plant roots.
  • ... and abiotic parts: sand, silt, clay, water, air and heat.
  • The parts interact: decomposers recycle minerals; bacteria in bean roots fix nitrogen.
  • Soil supports other systems: plants grow in it, animals burrow in it, people farm and build on it.
  • For each feature, add an example of it: 'biotic parts, such as earthworms'.

Biotic: living

  • Bacteria and fungi (decomposers)
  • Earthworms, mites, insects
  • Plant roots

Abiotic: non-living

  • Sand, silt and clay
  • Water and air in the gaps
  • Heat from the Sun

Real example: clover and beans have small swellings on their roots called nodules. Inside, Rhizobium bacteria turn nitrogen gas from the soil air into nitrates the plant can use: a plant, a bacterium and the air interacting.

One feature, one example: Write each feature in its own sentence, then give its example: 'soil has abiotic parts, such as clay and water'. A list of examples with no feature named does not show how soil is like an ecosystem.
A system that keeps changing: Soil is a dynamic system: its storages grow or shrink as the balance of inputs and outputs changes. It is also part of a bigger system, the ecosystem above and around it.

The points to remember

  • Dynamic: the soil is always changing, as inputs and outputs change its storages.
  • If inputs are bigger than outputs, a storage grows: more humus, a deeper soil.
  • If outputs are bigger, it shrinks: erosion or leaching drain the soil.
  • Soil sits within the larger ecosystem: changes in plants, climate or farming change the soil.
  • Soils are a resource for life and they vary widely from place to place.
Remember it as: Inputs bigger: the soil builds. Outputs bigger: the soil drains.

Real example: a 2021 study of satellite images found that about a third of the farmland in the US Corn Belt has lost all of its dark, carbon-rich topsoil since ploughing began, mostly on hilltops, to erosion.

Soils vary widely

  • Deep and dark under grassland
  • Thin and stony on mountains
  • Red and leached in the wet tropics

... and are a resource for life

  • Most of our food grows in soil
  • Soil stores and cleans water
  • Soil is home to countless species

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How this comes up: Paper 2, Section B (a): show how soil is like an ecosystem, one feature per point, each with an example.
IB-style questionOutline[4 marks]

Soil scientists in the Amazon rainforest have found thousands of species of bacteria, fungi and insects in a single hectare of forest soil.

Outline how soil can be viewed as an ecosystem.

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Rothamsted's Broadbalk field in England has been farmed for wheat since 1843, and some plots get farmyard manure every year.

between an input and a storage in this soil system, with an example of each.
[2 marks]

Related ESS HL Topics

Continue learning with these related topics from the same unit:

5.1.2What soil is made of
5.1.3Soil profiles and horizons
5.1.4Inputs to soil
5.1.5Outputs from soil
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