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TYPES OF SOILS
Eight major types according to Indian Council of
Agricultural Research (ICAR).
Alluvial soils
Black soils
Red soils
Laterite soils
Desert soils
Mountain soils
Saline and Alkaline soils
Peaty and Marshy soils
ALLUVIAL SOILFormed by deposition of alluvium by rivers.
Occupies 15 Lakh sqkm area in India.
Contribute greatly in agricultural development.
Two types: KHADAR & BHANGAR
KHADAR: Newer alluvium.
Sandy, pale brown composition.
Found in lower areas.
Flooded every year.
ALLUVIAL SOIL
Characteristics: Transported soils.
Coarser in upper section and finest in delta.
Light to dark in colour.
Rich in Potash & Humus.
Poor in Phosphorous and Nitrogen.
Highly fertile, good for all crops (kharif & rabi).
Crops: Rice, Wheat, Sugarcane, Cotton, Jute.
Areas: Punjab, Haryana, U.P, Bihar, W.B, Assam,
Parts of Orissa, delta regions of S.India
BLACK SOIL
Also known as Regur or Black Cotton soil.
Dark grey to Black in colour.
High clay content.
Highly moist retentive.
Develops cracks in summer.
Covers 5.4 lakh sqkm.
Highly suitable for cotton.
Rich in iron, lime, calcium, Magnesium, carbonates, and
alumina.
BLACK SOIL
Poor in Phosphorous, Nitrogen and Organic matter.
The soil is black in colour because it is volcanic in origin
Created from igneous rocks, and is called ‘regur soil’
Areas: Deccan Trap which includes: Maharastra, Wn
M.P, Parts of A.P, Nn
Karnataka, Parts of T.N and
Rajasthan.
Crops: Cotton, Sugarcane, Groundnut, Millets, Rice,
Wheat, Oilseeds.
RED SOIL
Formed due to weathering of old crystalline rocks in the areas of low
rainfall.
More sandy and less clayey.
Rich in iron, small amount of Humus.
Poor in phosphorus, nitrogen and lime.
Slightly acidic and do not retain moisture.
3.5 lakhs sq.km area.
Porous and Friable.
Area :
Tamil Nadu, Southern Karnataka, parts of Madhya Pradesh, Maharashtra, West
Bengal, Eastern Rajasthan, North eastern Sates.
Crops :
Ragi, Groundnut, millet, Tobacco, Potato, Rice, Wheat, Sugarcane.
The red colour is because of the
diffusion of iron in the form of iron
oxide in the crystalline and
metamorphic rocks
It looks yellow
when it is in the
hydrated form
LATERITE SOIL Latin word meaning brick.
 Formed under high temperature and rainfall with wet and dry spell.
 Silica is leached due to high rainfall.
 Remnants of iron and aluminum oxides left behind is know as Laterite.
 Brown to Yellowish colour.
 Becomes hard when exposed to atmosphere.
 Used as building material.
 Rich in Iron.
 Poor in Lime, Potash, & Magnesium.
 Occupies 2.4 Lakh sqkm.
 The humus content in the laterite soil is less because the micro-organisms and
decomposers get destroyed in the high temperature.
 Areas: Parts of Assam, Karnataka, T.N, A.P, M.P, Kerala.
 Crops: After taking soil conservation measures, this soil is suitable for Tea, Coffee,
Cashew, Rubber and Coconut.
Laterite has been derived from the Latin word ‘later’
that means brick.
Laterite Soil
RT SOIL
Contains soluble salts.
Red to brown in colour.
Originated by Mechanical disintegration & wind deposit.
Porous and coarse.
90% sand & 5% clay.
Rich in Nitrates & Phosphates.
Poor in Nitrogen & Humus.
Friable, sandy & low moist content.
1.4 Lakh sqkm.
Areas: Arid and Semi arid regions
of Rajasthan, S
n
Haryana, Punjab,
N
n
Gujarat.
MOUNTAIN SOIL
Found in hill slopes.
Formed by deposition of organic matter from forest.
Rich in humus.
Poor in Potash and Lime.
Areas: Assam, Kashmir, Sikkim & Arunachal Pradesh.
Crops: Tea, Coffee, Spices & Tropical Fruits.
SALINE & ALKALINE SOIL
Contains salts like Sodium, Magnesium, Calcium.
Infertile, unfit for cultivation.
Sandy to loamy in texture.
Areas:
Parts of Gujarat, Rajasthan, Punjab, Haryana, U.P
& Maharashtra.
PEATY AND MARSHY SOIL
Occur in Humid region.
Formed by accumulation of organic matter.
Black in colour.
Highly acidic and heavy.
Areas:
Kottayam & Alleppey in Kerala, Coastal Orissa,
Sundarbans of W.B
SOIL EROSION
 EFFECTS:
Loss of cultivable land.
Reduction in soil fertility.
Causes silting & may change river course.
Results in lots of run off.
Reduces percolation of ground water.
CAUSES:
Deforestation
Overgrazing.
Faulty method of Agriculture.
Erosion by rivers.
Removal of top soil (for bricks, pots, tiles etc)
Shifting cultivation.
SOIL CONSERVATION
Measures For Soil Conservation:
Contour farming.
Mulching ( spreading of grass, leaves on ground).
Afforestation and Reforestation.
Controlled grazing.
Construction of dams and barrages
Crop rotation.
Sub soiling.
Terrace farming.
SOILS OF INDIA

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SOILS OF INDIA

  • 1.
  • 2. TYPES OF SOILS Eight major types according to Indian Council of Agricultural Research (ICAR). Alluvial soils Black soils Red soils Laterite soils Desert soils Mountain soils Saline and Alkaline soils Peaty and Marshy soils
  • 3. ALLUVIAL SOILFormed by deposition of alluvium by rivers. Occupies 15 Lakh sqkm area in India. Contribute greatly in agricultural development. Two types: KHADAR & BHANGAR KHADAR: Newer alluvium. Sandy, pale brown composition. Found in lower areas. Flooded every year.
  • 4. ALLUVIAL SOIL Characteristics: Transported soils. Coarser in upper section and finest in delta. Light to dark in colour. Rich in Potash & Humus. Poor in Phosphorous and Nitrogen. Highly fertile, good for all crops (kharif & rabi). Crops: Rice, Wheat, Sugarcane, Cotton, Jute. Areas: Punjab, Haryana, U.P, Bihar, W.B, Assam, Parts of Orissa, delta regions of S.India
  • 5. BLACK SOIL Also known as Regur or Black Cotton soil. Dark grey to Black in colour. High clay content. Highly moist retentive. Develops cracks in summer. Covers 5.4 lakh sqkm. Highly suitable for cotton. Rich in iron, lime, calcium, Magnesium, carbonates, and alumina.
  • 6. BLACK SOIL Poor in Phosphorous, Nitrogen and Organic matter. The soil is black in colour because it is volcanic in origin Created from igneous rocks, and is called ‘regur soil’ Areas: Deccan Trap which includes: Maharastra, Wn M.P, Parts of A.P, Nn Karnataka, Parts of T.N and Rajasthan. Crops: Cotton, Sugarcane, Groundnut, Millets, Rice, Wheat, Oilseeds.
  • 7. RED SOIL Formed due to weathering of old crystalline rocks in the areas of low rainfall. More sandy and less clayey. Rich in iron, small amount of Humus. Poor in phosphorus, nitrogen and lime. Slightly acidic and do not retain moisture. 3.5 lakhs sq.km area. Porous and Friable. Area : Tamil Nadu, Southern Karnataka, parts of Madhya Pradesh, Maharashtra, West Bengal, Eastern Rajasthan, North eastern Sates. Crops : Ragi, Groundnut, millet, Tobacco, Potato, Rice, Wheat, Sugarcane.
  • 8. The red colour is because of the diffusion of iron in the form of iron oxide in the crystalline and metamorphic rocks It looks yellow when it is in the hydrated form
  • 9. LATERITE SOIL Latin word meaning brick.  Formed under high temperature and rainfall with wet and dry spell.  Silica is leached due to high rainfall.  Remnants of iron and aluminum oxides left behind is know as Laterite.  Brown to Yellowish colour.  Becomes hard when exposed to atmosphere.  Used as building material.  Rich in Iron.  Poor in Lime, Potash, & Magnesium.  Occupies 2.4 Lakh sqkm.  The humus content in the laterite soil is less because the micro-organisms and decomposers get destroyed in the high temperature.  Areas: Parts of Assam, Karnataka, T.N, A.P, M.P, Kerala.  Crops: After taking soil conservation measures, this soil is suitable for Tea, Coffee, Cashew, Rubber and Coconut.
  • 10. Laterite has been derived from the Latin word ‘later’ that means brick. Laterite Soil
  • 11. RT SOIL Contains soluble salts. Red to brown in colour. Originated by Mechanical disintegration & wind deposit. Porous and coarse. 90% sand & 5% clay. Rich in Nitrates & Phosphates. Poor in Nitrogen & Humus. Friable, sandy & low moist content. 1.4 Lakh sqkm. Areas: Arid and Semi arid regions of Rajasthan, S n Haryana, Punjab, N n Gujarat.
  • 12. MOUNTAIN SOIL Found in hill slopes. Formed by deposition of organic matter from forest. Rich in humus. Poor in Potash and Lime. Areas: Assam, Kashmir, Sikkim & Arunachal Pradesh. Crops: Tea, Coffee, Spices & Tropical Fruits.
  • 13. SALINE & ALKALINE SOIL Contains salts like Sodium, Magnesium, Calcium. Infertile, unfit for cultivation. Sandy to loamy in texture. Areas: Parts of Gujarat, Rajasthan, Punjab, Haryana, U.P & Maharashtra.
  • 14. PEATY AND MARSHY SOIL Occur in Humid region. Formed by accumulation of organic matter. Black in colour. Highly acidic and heavy. Areas: Kottayam & Alleppey in Kerala, Coastal Orissa, Sundarbans of W.B
  • 15. SOIL EROSION  EFFECTS: Loss of cultivable land. Reduction in soil fertility. Causes silting & may change river course. Results in lots of run off. Reduces percolation of ground water. CAUSES: Deforestation Overgrazing. Faulty method of Agriculture. Erosion by rivers. Removal of top soil (for bricks, pots, tiles etc) Shifting cultivation.
  • 16. SOIL CONSERVATION Measures For Soil Conservation: Contour farming. Mulching ( spreading of grass, leaves on ground). Afforestation and Reforestation. Controlled grazing. Construction of dams and barrages Crop rotation. Sub soiling. Terrace farming.