Composition of Soils (Cambridge International IGCSE Environmental Management)
Mineral particles in soil
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Mineral particles are small pieces of weathered rock
- Soils contain a mixture of sand, silt and clay
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Sand—largest particles
- Feels gritty and allows fast drainage of water
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Silt—medium-sized particles
- Feels smooth and holds water better than sand
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Clay—smallest particles
- Feels sticky when wet and holds lots of water and nutrients
Organic content in soil
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Organic content refers to living and once-living material in the soil
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Includes living organisms such as:
- Plants and plant roots
- Animals like insects and worms
- Fungi that break down dead material
- Bacteria that help with decomposition and nutrient cycling
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Also includes organic matter from decomposition
- Dead plants and animals break down to form humus
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Organic content helps soil hold nutrients and water
Gases & water in soil
Gases in soil
- Soil contains air spaces filled with gases
- These air spaces provide oxygen for roots and soil organisms
- They also contain carbon dioxide released by respiration of organisms
- Good aeration helps maintain healthy biological activity in the soil
Water in soil
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Soil holds water between particles and in tiny pores
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Plants absorb this water through their roots
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Water carries dissolved nutrients like nitrates and phosphates
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The amount of water held depends on soil texture
- Clay holds more water; sand holds less
Exam Hint Don’t forget gases when describing soil composition—many students leave this out, but soil must contain air spaces for plant roots to access oxygen for respiration.
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