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soil
Topic # 1
soil formation
• Soil :
“ the upper layer/weathered layer of earth crust
is called soil”
• Edaphology :
“ the study of soil is called edaphology “
How soil formed :
Over million of years, the forces of weathering and
erosion, slowly but constantly have produced a layer of
broken pieces of rock all over the earth’s surface. The
size of these rock pieces varies from boulders to the
finest bits. The layer composed of pieces of rock is
called ROCK MANTLE.
As the forces of wind and water go on breaking and
decomposing the rock mantle, a layer of fine loose
materials is formed. This is referred to as SOIL. It is
made up of tiny grains of rocks and materials.
• The natural processes of weathering and
erosion bring about important changes on the
surface rock. These processes consistently
break, carry off and deposit loose surface
materials from where they are formed to
other places. The continued action of water
and wind changes the rock pieces into finer
particles, thus forming boulders, gravel, sand
and clay.
• To these surface materials are added the
decayed remains of plants and animals called
HUMUS. Organic substances are returned into
the soul after they decompose. Because of
their finer texture, these enable the soil to
hold much water.
How soil is formed ?
Soil is formed by weathering
“the breakdown of soil is called weathering “
There are two types of weather
1. Mechanical weather
2. Chemical weather
Mechanical weathering
• Mechanical weathering includes processes that break rocks
to pieces without changing their chemical composition.
“the breakdown of rock by cracking through various agencies
is called mechanical weathering”
 It is brought about by severe environmental conditions
such as
I. Temperature
II. Rain water
III. Snow
IV. Wing
V. Plants and animals
Mechanical weathering
1. Temperature
Temperature influence the breaking of rock by expanidation an contraction of
rocks .During the day the rock are heated and then expand. At night, they are
cooled and then contract. Since rocks are composed of minerals, these
minerals expand and contract too. This alternate expansion and contraction
causes the rocks to crack, especially if the minerals expand and contract in
unequal amounts.
.
Mechanical weathering
.
water freezing also increase
Weathring .
Water may enter the cracks or crevices in rocks. When it freezes
it expands by about 9% of its volume, causing the rock to split.
Sometimes this alternate expansion and contraction may cause the rocks to peel off
in thin sheets. This peeling off process is called exfoliation
Mechanical weathering
• 2. Rain water
The rain water flowing on the rock also cause
the break down of this rock
Mechanical weathering
• 3. snow :
• Snow moves down the rocks from glaciers and
grinds the underlying particles and change to
soil
Mechanical weathering
• 4. wind :
• Wind carries small fragments of rocks from
one place to other and it help in soil formation
Mechanical weathering
• 5. plants and animals :
• Plant root grow inside rock and break it to
form soil
• Animal burrows which disintegrate the rocks
Chemical weathering
In chemical weathering, the composition
of the rock is altered. A new product which
easily crumbles to pieces is formed.
Chemical weathering is brought about by a
chemical reaction between the minerals in
the rocks and carbon dioxide, oxygen or
water.
Chemical weathering may cause due to
I. Hydrolysis
II. Hydration
III. Carbonation
IV. Oxidation
V. Solvent action
Chemical weathering
• Hydrolysis :
Break down of rock mineral by the action of water
• Hydration
Water dissociate into ions and H and OH reacts with different
compounds , and reaction cause the break down of rock
• Carbonation :
Water and CO2 react to form carbonic acid which alter the
composition of rock
• Oxidation
Rock which contain iron undergo oxidation which make it porous and
break able
• Solvent action
Water as a universal solvent dissolve some minerals and cause the
breaking of soil

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Soil formation by weathering by Tasssanam Naz

  • 2. Topic # 1 soil formation • Soil : “ the upper layer/weathered layer of earth crust is called soil” • Edaphology : “ the study of soil is called edaphology “
  • 3. How soil formed : Over million of years, the forces of weathering and erosion, slowly but constantly have produced a layer of broken pieces of rock all over the earth’s surface. The size of these rock pieces varies from boulders to the finest bits. The layer composed of pieces of rock is called ROCK MANTLE. As the forces of wind and water go on breaking and decomposing the rock mantle, a layer of fine loose materials is formed. This is referred to as SOIL. It is made up of tiny grains of rocks and materials.
  • 4. • The natural processes of weathering and erosion bring about important changes on the surface rock. These processes consistently break, carry off and deposit loose surface materials from where they are formed to other places. The continued action of water and wind changes the rock pieces into finer particles, thus forming boulders, gravel, sand and clay.
  • 5. • To these surface materials are added the decayed remains of plants and animals called HUMUS. Organic substances are returned into the soul after they decompose. Because of their finer texture, these enable the soil to hold much water.
  • 6. How soil is formed ? Soil is formed by weathering “the breakdown of soil is called weathering “ There are two types of weather 1. Mechanical weather 2. Chemical weather
  • 7. Mechanical weathering • Mechanical weathering includes processes that break rocks to pieces without changing their chemical composition. “the breakdown of rock by cracking through various agencies is called mechanical weathering”  It is brought about by severe environmental conditions such as I. Temperature II. Rain water III. Snow IV. Wing V. Plants and animals
  • 8. Mechanical weathering 1. Temperature Temperature influence the breaking of rock by expanidation an contraction of rocks .During the day the rock are heated and then expand. At night, they are cooled and then contract. Since rocks are composed of minerals, these minerals expand and contract too. This alternate expansion and contraction causes the rocks to crack, especially if the minerals expand and contract in unequal amounts. .
  • 9. Mechanical weathering . water freezing also increase Weathring . Water may enter the cracks or crevices in rocks. When it freezes it expands by about 9% of its volume, causing the rock to split. Sometimes this alternate expansion and contraction may cause the rocks to peel off in thin sheets. This peeling off process is called exfoliation
  • 10. Mechanical weathering • 2. Rain water The rain water flowing on the rock also cause the break down of this rock
  • 11. Mechanical weathering • 3. snow : • Snow moves down the rocks from glaciers and grinds the underlying particles and change to soil
  • 12. Mechanical weathering • 4. wind : • Wind carries small fragments of rocks from one place to other and it help in soil formation
  • 13. Mechanical weathering • 5. plants and animals : • Plant root grow inside rock and break it to form soil • Animal burrows which disintegrate the rocks
  • 14. Chemical weathering In chemical weathering, the composition of the rock is altered. A new product which easily crumbles to pieces is formed. Chemical weathering is brought about by a chemical reaction between the minerals in the rocks and carbon dioxide, oxygen or water. Chemical weathering may cause due to I. Hydrolysis II. Hydration III. Carbonation IV. Oxidation V. Solvent action
  • 15. Chemical weathering • Hydrolysis : Break down of rock mineral by the action of water • Hydration Water dissociate into ions and H and OH reacts with different compounds , and reaction cause the break down of rock • Carbonation : Water and CO2 react to form carbonic acid which alter the composition of rock • Oxidation Rock which contain iron undergo oxidation which make it porous and break able • Solvent action Water as a universal solvent dissolve some minerals and cause the breaking of soil