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NotesESS HLTopic 5.1The A horizon
Back to ESS HL Topics
5.1.176 min read

The A horizon (ESS HL)

IB Environmental Systems and Societies • Unit 5

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Contents

  • The A horizon at Higher Level
  • What the A horizon is
  • Why most roots and life are in the topsoil
  • Most valuable, most vulnerable
  • Farming, fertiliser and protecting topsoil
  • Exam-style question
The A horizon at Higher Level: This statement is Higher Level only. It explains why the topsoil holds most of the soil's life and roots, why it is both the most valuable and the most vulnerable layer, and how farming can lose it or protect it.

Practise this as you read

  • Explain why most root growth is in the A horizon.
  • Outline ways to protect topsoil on farms.

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The topsoil: The A horizon is the topsoil. It lies just beneath the leaf litter and is dark because it is rich in humus.

The points to remember

  • The A horizon lies just beneath the O horizon (the organic humus layer), where there is one.
  • It is also called the mixed layer or topsoil.
  • It is rich in organic matter: humus mixed with sand, silt and clay.
  • Humus makes it darker than the layers below.
Remember it as: A for 'all mixed': humus and minerals together.

Real example: the chernozem soils of Ukraine have an A horizon that is often more than half a metre deep. This thick, humus-rich topsoil is one reason Ukraine is one of the world's biggest wheat exporters.

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Why do almost all roots, worms and microbes live near the top? Because the topsoil has more of everything they need than the layers below.

Why most life is in the topsoil

  • Topsoil has more oxygen than lower horizons: more air spaces, so roots and microbes can respire.
  • It has more organic matter, which holds water and nutrients.
  • It has more microorganisms (bacteria, fungi) and animals such as earthworms.
  • So there is more nutrient recycling: decomposers release nutrients right where the roots are.
  • Therefore it is where there is most root growth and other biological activity.
Table of typical values under a meadow, A horizon then B horizon: organic matter 5% and 1%; air in the pore spaces 25% and 10% of volume; earthworms 250 and 20 per square metre; share of the plants' roots 70% and 25%
Topsoil beats subsoil on every measure.

A horizon (topsoil)

  • More oxygen
  • More organic matter
  • More microorganisms
  • Fast nutrient recycling
  • Most roots

B horizon (subsoil)

  • Less oxygen
  • Little organic matter
  • Few organisms
  • Slow recycling
  • Few roots

Real example: in 1881 Charles Darwin showed that earthworms in English fields pass so much soil through their bodies that stones and chalk left on the surface slowly sink into the topsoil. That constant mixing is what makes the A horizon the 'mixed layer'.

The A horizon is both the most valuable layer and, with the O horizon, the most at risk, because it is on top.

Most valuable, most vulnerable

  • The A horizon is the most valuable layer for plant growth.
  • With the O horizon, it is also the most vulnerable: it lies at the surface.
  • Erosion: rain and wind carry bare topsoil away.
  • Degradation: compaction by machines, loss of organic matter, salinization, pollution.
  • Soil forms very slowly (up to 1000 years for 1 cm), so lost topsoil is not renewed in a lifetime.
Why this matters for sustainability: Topsoil forms far more slowly than it can be lost. A farm that loses its topsoil in a few decades cannot wait centuries for it to return, so managing soil sustainably means keeping it in place.

Real example: in the 1930s, farmers on the US Great Plains had ploughed up the prairie grass. When drought came, the bare topsoil blew away in huge dust storms, the Dust Bowl. On 'Black Sunday', 14 April 1935, one storm turned day into night.

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Where intensive farming has removed the topsoil, crops depend on fertiliser. The better answer is to protect it. One loess region shows how.

Losing it, and protecting it

  • Intensive farming can remove the A horizon: ploughing, bare soil and erosion.
  • Without topsoil the land needs fertilisers to replace the lost nutrients.
  • Keep it covered: cover crops, mulch and crop residues shield it from rain and wind.
  • Disturb it less: no-till farming keeps its structure and its organisms.
  • Slow the water and wind: contour ploughing, terraces, windbreaks.
  • Feed it: compost and manure add organic matter back.
Remember it as: Cover it, don't disturb it, slow the water, feed it.

Problem

  • Steep, overgrazed and ploughed slopes lost their topsoil to rain; the Yellow River ran thick with it

Terraces

  • From the 1990s, slopes were cut into flat terraces that hold the water and the soil

Cover

  • Trees and grass were planted, and goats and sheep were kept off the steepest land

Result

  • Far less soil washed into the river; farm yields and incomes rose
How this comes up: Paper 2, Section A: data on topsoil and subsoil to compare and explain. Section B (a): outline why the A horizon matters for plants; (b): explain how farming affects it and how it can be protected.
IB-style questionExplain[3 marks]

After a dry spring, strong winds lifted dark topsoil off newly ploughed fields in Lincolnshire, England, while fields under winter crops lost almost none.

Explain why the A horizon is so vulnerable to erosion and why its loss matters.

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IB Exam Questions on The A horizon

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How The A horizon Appears in IB Exams

Examiners use specific command terms when asking about this topic. Here's what to expect:

Define

Give the precise meaning of key terms related to The A horizon.

AO1
Describe

Give a detailed account of processes or features in The A horizon.

AO2
Explain

Give reasons WHY — cause and effect within The A horizon.

AO3
Evaluate

Weigh strengths AND limitations of approaches in The A horizon.

AO3
Discuss

Present arguments FOR and AGAINST with a balanced conclusion.

AO3

See the full IB Command Terms guide →

Related ESS HL Topics

Continue learning with these related topics from the same unit:

5.1.1Soil as a system
5.1.2What soil is made of
5.1.3Soil profiles and horizons
5.1.4Inputs to soil
View all ESS HL topics

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5.1.16Soil horizons in detail
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Factors in soil formation5.1.18

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