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B Y - A R T I S I N G H
Soil and its types
Content
 What is soil?
 Soil formation
 Weathering
 Soil development
 Factors influence soil
formation
 Soil Profile
 Soil composition
 Physical properties of
soil
 Soil texture
 Types of soil and
comparison
 Chemical properties
 Humus
 Soil Water
 Soil Air
 Soil reaction
 Soil Organism
 Problems regarding soil
 Conservation of soil
What is soil?
 It is originated from Latin word ‘solum’.
 It is basic natural resources.
 Soil is a mixture of organic matter,
minerals, gases, liquids, and organisms that together
support life.
 The study of soil is called pedology or edaphology.
Soil formation
Soil formation
It can be divided into two major stages-
1. Weathering
2. Soil development
1. Weathering
This process performed by three methods-
Physical Weathering
Chemical Weathering
Biological Weathering
2. Soil development
 It is also called Pedogenesis or Soil Maturation.
 Organisms such as bacteria, fungi, algae, lichens etc.,
help in this process.
 A mixture of Organic and Inorganic substances is
formed by humus. This is called Soil.
Factors
influenced soil
formation
1. 1.Parent rock
2. 2.Climate
3. 3.Relief
4. 4. Time
5. 5. Flora, fauna
and Micro-
organism
Soil profile
 A vertical section of soil in which many horizons of soil
are seen is called Soil Profile.
 Horizon-A (Top Soil)
o O1 Horizon
o O2 Horizon
o A1 Horizon
o A2 Horizon
 Horizon-B (Sub-Soil)
 Horizon-C (Parent Rock)
 Horizon-D (Bed Rock)
Soil composition
Physical properties of soil
1. Soil Colour
It can be different colour in different places but soil colour does
not affect their working system.
2. Porosity
Empty spaces are present among soil particles those have soil
water and soil air.
3. Soil Permeability
The power of soil to allow water to pass through it.
4.Soil texture
Particle size-
Gravel = >5.000mm in diameter.
Fine Gravel = 2.000-5.000mm
Coarse sand = 0.200-2.000mm
Fine sand = 0.020-0.200mm
Silt = 0.002-0.020mm
Clay = <0.002mm
Types of soil
Chemical properties
 Mineral matter or inorganic matter
o Macronutrients
o Micronutrients
 Organic matter or humus
Humus
 It is dark organic matter that forms in
soil when dead plants and animal matter
decays.
Types of Humus-
Soil water
It is the most significant factor because the absorption of
minerals and organic matter through roots takes place by
water only.
Soil water balance
Types of soil
water-
1.Chemically
combined water
2.Hygroscopic water
3.Capillary water
4.Gravitational water
5.Atmospheric water
Soil air
The air present in soil.
Following activities of plant performed by soil air-
 Water absorption
 Growth of roots
 Formation of new root hairs
 Respiration by roots
 Seed germination
Soil reaction
 The soil may be neutral, acidic or basic.
 pH of soil varies from 3-9.
 The value of pH the effects the concentration and
availability of other minerals.
 The plant growth is good between 6 to 7.5 pH.
Soil organisms
 Soil organisms are commonly
divided into five arbitrary
groups according to size, the
smallest of which are
the protists—including bacteria,
actinomycetes, and algae.
Problems of soil
 Soil erosion
 Desertification
 Salinisation and Alkalisation
 Impact of Intensive
Agriculture
 Urbanization and
Contamination
Conservation of soil
There are three main methods-
1.Agronomical measures
• Contour farming
• Strip cropping
• Cover cropping
• Crop rotation
2.Biological methods
 Afforestation
 Trenching
 Ley farming
 Silvi-Pastural Practices
3.Mechanical methods
 Bunding
 Terracing
 Gully control
 Ravine reclamation
THANK YOU

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Soil and its type ppt

  • 1. B Y - A R T I S I N G H Soil and its types
  • 2. Content  What is soil?  Soil formation  Weathering  Soil development  Factors influence soil formation  Soil Profile  Soil composition  Physical properties of soil  Soil texture  Types of soil and comparison  Chemical properties  Humus  Soil Water  Soil Air  Soil reaction  Soil Organism  Problems regarding soil  Conservation of soil
  • 3. What is soil?  It is originated from Latin word ‘solum’.  It is basic natural resources.  Soil is a mixture of organic matter, minerals, gases, liquids, and organisms that together support life.  The study of soil is called pedology or edaphology.
  • 5. Soil formation It can be divided into two major stages- 1. Weathering 2. Soil development
  • 6. 1. Weathering This process performed by three methods- Physical Weathering Chemical Weathering Biological Weathering
  • 7. 2. Soil development  It is also called Pedogenesis or Soil Maturation.  Organisms such as bacteria, fungi, algae, lichens etc., help in this process.  A mixture of Organic and Inorganic substances is formed by humus. This is called Soil.
  • 8. Factors influenced soil formation 1. 1.Parent rock 2. 2.Climate 3. 3.Relief 4. 4. Time 5. 5. Flora, fauna and Micro- organism
  • 9. Soil profile  A vertical section of soil in which many horizons of soil are seen is called Soil Profile.  Horizon-A (Top Soil) o O1 Horizon o O2 Horizon o A1 Horizon o A2 Horizon  Horizon-B (Sub-Soil)  Horizon-C (Parent Rock)  Horizon-D (Bed Rock)
  • 10.
  • 12. Physical properties of soil 1. Soil Colour It can be different colour in different places but soil colour does not affect their working system. 2. Porosity Empty spaces are present among soil particles those have soil water and soil air. 3. Soil Permeability The power of soil to allow water to pass through it.
  • 13. 4.Soil texture Particle size- Gravel = >5.000mm in diameter. Fine Gravel = 2.000-5.000mm Coarse sand = 0.200-2.000mm Fine sand = 0.020-0.200mm Silt = 0.002-0.020mm Clay = <0.002mm
  • 15.
  • 16. Chemical properties  Mineral matter or inorganic matter o Macronutrients o Micronutrients  Organic matter or humus
  • 17. Humus  It is dark organic matter that forms in soil when dead plants and animal matter decays. Types of Humus-
  • 18. Soil water It is the most significant factor because the absorption of minerals and organic matter through roots takes place by water only. Soil water balance
  • 19. Types of soil water- 1.Chemically combined water 2.Hygroscopic water 3.Capillary water 4.Gravitational water 5.Atmospheric water
  • 20. Soil air The air present in soil. Following activities of plant performed by soil air-  Water absorption  Growth of roots  Formation of new root hairs  Respiration by roots  Seed germination
  • 21. Soil reaction  The soil may be neutral, acidic or basic.  pH of soil varies from 3-9.  The value of pH the effects the concentration and availability of other minerals.  The plant growth is good between 6 to 7.5 pH.
  • 22. Soil organisms  Soil organisms are commonly divided into five arbitrary groups according to size, the smallest of which are the protists—including bacteria, actinomycetes, and algae.
  • 23. Problems of soil  Soil erosion  Desertification  Salinisation and Alkalisation  Impact of Intensive Agriculture  Urbanization and Contamination
  • 24. Conservation of soil There are three main methods- 1.Agronomical measures • Contour farming • Strip cropping • Cover cropping • Crop rotation
  • 25. 2.Biological methods  Afforestation  Trenching  Ley farming  Silvi-Pastural Practices
  • 26. 3.Mechanical methods  Bunding  Terracing  Gully control  Ravine reclamation