soil : not just ‘ dirt ’

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Soil: Not Just ‘Dirt’

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Soil : Not Just ‘ Dirt ’. What is Soil ?. Soils are a major component of the world’s ecosystems. They form at the interface of the Earth’s atmosphere , lithosphere (rocks), biosphere (living matter) and hdyrosphere (water). What is Soil ?. - PowerPoint PPT Presentation

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Page 1: Soil : Not  Just  ‘ Dirt ’

Soil: Not Just ‘Dirt’

Page 2: Soil : Not  Just  ‘ Dirt ’

What is Soil?

Soils are a major component of the world’s ecosystems.

They form at the interface of the Earth’s atmosphere, lithosphere (rocks), biosphere (living matter) and hdyrosphere (water).

Page 3: Soil : Not  Just  ‘ Dirt ’

What is Soil?

Soil is what forms the outermost layer of the Earth’s surface.

Soil comprise weathered bedrock (regolith), organic matter (both dead and alive), air and water.

LIKE LIVING SKIN OF THE EARTH!

Page 4: Soil : Not  Just  ‘ Dirt ’

What is soil?

Soil has matter in all three states:

• organic and inorganic matter form the solid state

• soil water form the liquid state (precipitation, groundwater and seepage)

• soil atmosphere forms the gaseous state

Page 6: Soil : Not  Just  ‘ Dirt ’

Functions of soil

Page 7: Soil : Not  Just  ‘ Dirt ’

Functions of soil

Soils are important to humans in many ways:• soil is the medium for plant growth,

which most of foods for humans are grown in

• soil stores freshwater, 0.005% of world’s freshwater

• soil filters materials added to the soil, keeping quality water

Page 8: Soil : Not  Just  ‘ Dirt ’

Functions of soil

• soil is nature’s recycling system. Waste and dead matter are decomposed and their nutrients made available for new life.

• soil is the habitat for billions of micro-organisms, as well as other larger animals

• soil provides raw material in the forms of peat, clay, sands, gravel and minerals

Page 9: Soil : Not  Just  ‘ Dirt ’

Functions of soilSoils breathe!

Gases are exchanged between the soil surface and the air. Gases like oxygen and methane are absorbed, while, while gases like carbon dioxide and nitrous oxide are released. The soil provides a valuable carbon sink. The evaporation of soil moisture also affects air temperature and weather patterns.

Page 10: Soil : Not  Just  ‘ Dirt ’
Page 11: Soil : Not  Just  ‘ Dirt ’

Soil Biology

Soil is by far the most biologically diverse part of the earth.

It contains a complex food web of prey, predators and decomposers.

These organisms require the same elements we require: air, water, food and shelter.

Page 12: Soil : Not  Just  ‘ Dirt ’

Soil Biology

Page 13: Soil : Not  Just  ‘ Dirt ’

Soil Biology

One teaspoon of healthy soil may contain:

• Bacteria- 100 million to 1 billion• Fungi- up to 100 yards of fungal hyphae• Protozoa- several thousand• Nematodes- up to several hundred• Arthropods (insects,spiders,centipeds)-500-2000• Earthworms- arid soils may have none to several

Page 15: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

Page 16: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

O – Organic Horizon:

l - undecomposed litterf – party decomposed litterh – well decomposed humus

Page 17: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

A – Mixed mineral-organic Horizon:

h – humusp – ploughed in field or gardeng – gleyed or waterlogged

Page 18: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

E - Eluvial or leached Horizon:

a – strongly leached, and ash colouredb – weakly bleached, light brown

Page 19: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

B – Illuvial or deposited

Fe – iron depositedt – clay depositedh – humus deposited

Page 20: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

C – Bedrock or parent material

r – rocku – unconsolidated loose deposits

Page 21: Soil : Not  Just  ‘ Dirt ’

Soil Horizons

Page 22: Soil : Not  Just  ‘ Dirt ’

Formation of soil

Soil forming process consists of: Gains and losses of material to

and from the profile Movement of water between the

horizons Chemical transformation within

each horizon.

Soil is formed from rocks and decaying plants and animals.

Page 23: Soil : Not  Just  ‘ Dirt ’

Formation of soil

Therefore soils are open systems in a steady-state

equilibrium

Page 24: Soil : Not  Just  ‘ Dirt ’

Formation of soilThe principle processes include

• Weathering• Translocation• Organic changes (degradation, humification, mineralization)• Gleying (waterlogging)

Page 25: Soil : Not  Just  ‘ Dirt ’

Formation of soil

Page 26: Soil : Not  Just  ‘ Dirt ’

Formation of soil

Page 27: Soil : Not  Just  ‘ Dirt ’

Soil Formation

Natural processes can take 500 years to form one inch of top soil.

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Soils are vital to humans, but take a long time to develop, so should be

considered a non-renewable resource

Page 29: Soil : Not  Just  ‘ Dirt ’

Soil Degradation

Page 30: Soil : Not  Just  ‘ Dirt ’

Value of Soil

“The soil is the great connector of lives, the source and destination of all. It is the healer and restorer and resurrector, by which disease passes into health, age into youth, death into life. Without proper care for it we can have no community, because without proper care for it we can have no life.”

― Wendell Berry, The Unsettling of America: Culture and Agriculture

Page 32: Soil : Not  Just  ‘ Dirt ’

Painting with soil

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A little research……..

• What is pedology?• What is compost?• How to make compost? Is it possible to make compost at home or at school?