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Land use & soil

"Dirt cheap" is exactly wrong. Soil is a thin, living, slow-made skin — centimetres that take centuries — and almost all our food grows in it. This powerbook follows three ways human land use destroys it faster than it can rebuild: salt rising to the surface, topsoil washing away, and metals poisoning the ground — and what it takes to heal each.

3
ways we damage soil
centuries
to form, fast to lose
5
short sections
Land use & soilSection 1 of 5
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This book has 5 short sections. Read each one, answer the check, then use Next to move on — the bar above tracks how far you've come.

Soil is not just dirt

We treat soil as the cheapest thing there is — "dirt cheap", literally. Yet almost all the food humanity eats grows in a thin surface layer of it, and that layer is one of the slowest things on Earth to replace. Soil is not lifeless dust. It is a living mixture: weathered mineral grains from broken-down rock, dark organic matter (humus) from decayed plants and animals, plus water, air, and a teeming population of bacteria, fungi, worms and roots.

Making it takes a very long time. Rock has to be weathered into mineral particles, and generations of living things have to live and die to build up the humus that makes soil fertile. A few centimetres of good topsoil can take centuries to form. On any human timescale, soil is effectively non-renewable — lose it, and you do not get it back in a lifetime.

And the richest, most fertile part — the topsoil — sits right at the surface, exactly where human land use can damage it. This chapter is about three ways our use of land degrades that precious layer: it can grow salty, it can wash and blow away, and it can be poisoned — and what it takes to heal it afterwards.

A soil profiletopsoil — rich, alive, thinsubsoilweathered rockbedrockminerals + humus+ water, air, lifecentimetres of topsoil can take centuries to form
Topsoil is a thin, living layer of weathered rock and decayed life — the richest part, and the slowest to replace.
New words
soil
A living mix of weathered rock, organic matter, water, air and organisms — slow to form.
humus/HYOO-mus/
Dark, decomposed organic matter that makes topsoil fertile.
topsoil
The rich, living top layer where most roots grow — and the first lost to damage.
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Why is soil described as effectively non-renewable on a human timescale?

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Quick reference & sources

The interactive book above is the lesson. What follows is a plain recap you can revise from, plus the sources and how this maps to the syllabus.

Salinity: clearing and irrigation

The salt is usually already stored deep; land use mobilises it. Land clearing removes deep-rooted plants, so less water is used, the water table rises, and it carries stored salt up — dryland salinity. Irrigation raises the table too, and its dissolved salt is left behind as water evaporates, building up in the root zone.

Erosion and its prevention

Erosion strips fertile topsoil by wind and water; it accelerates on bare, cleared, over-grazed or ploughed ground. Prevention keeps the ground covered and slows the flow: cover crops, stubble and mulch, contour ploughing, terracing on steep land, and windbreaks.

Contamination and rehabilitation

Heavy metals (lead, cadmium, mercury, arsenic) from mining, industry, old paint/petrol and sludge are elements — they do not break down, are taken up by plants, and bioaccumulate up the food chain. Rehabilitation answers the cause: replant to lower a saline water table, restore cover to halt erosion, and remove, cap or treat contaminated soil — all slow, so prevention wins.

For HSC students

This powerbook covers the Salinity and Erosion thread of Module 4 (Human Impacts), framed by the inquiry question how does human use of land affect soil? Working through it, you should be able to:

  • explain the causes of salinisation, including land clearing and irrigation;
  • describe how salinity-affected areas are rehabilitated (a basis for a case study);
  • account for soil erosion and evaluate prevention methods (a basis for the practical investigation);
  • investigate sources and effects of soil contamination, including heavy metals.

The next chapter looks at introduced species and their effects on Australian ecosystems. Explanations here are original and are a study aid, not a copy of the syllabus.

Sources

  • Australian and state agriculture/environment departments — dryland and irrigation salinity, causes and rehabilitation.
  • CSIRO and Landcare resources — soil erosion processes and prevention, and land rehabilitation.
  • Environmental-protection authority guidance — soil contamination, heavy metals and their effects.
  • NSW NESA Earth and Environmental Science Stage 6 Syllabus (2017) — used only to scope the Module 4 content; explanations above are original.

Soil is the cheapest thing we own and one of the hardest to replace. Salt it, strip it or poison it in a season, and the land takes centuries to forgive us.

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