Soils Resources of India Notes with PDF

These notes are your ultimate revision weapon to revise Soils Resources of India . We’ve distilled years of previous exam questions (PYQs) into one powerful, concise resource. Everything you need to know, nothing you don’t.

  • PYQs, Decoded: All key concepts from past exams, organized and simplified.
  • Revise in Record Time: Short, precise, and designed for last-minute review.
  • Focus on What Matters: Master high-probability topics and boost your confidence.
  • Free PDF to download.

1. Black Soil (Regur Soil)

Origin and Formation

  • Formed from the weathering of fissure volcanic rock (basaltic lava).
  • Specifically created from the breakdown of Deccan Trap rocks in the northwest Deccan plateau.
  • Also referred to as Lava Soil, found in regions like the Malwa Plateau.

Characteristics and Properties

  • Colour: Black.
  • Texture: Clayey with high iron content.
  • Moisture: Highly retentive of moisture.
  • Cracking: Develops deep cracks when dry.
  • Swelling: Swells and becomes sticky when wet.
  • Nickname: Known as “self-ploughed” soil because the cracking and swelling action naturally aerates the land.

Chemical Composition

  • Rich in: Alumina, iron, lime, magnesium carbonates, and potash.
  • Deficient in: Phosphorus, nitrogen, and humus.

Other Names and Classification

  • Also known as Regur soil or Black Cotton soil.
  • Classified by Krabs as essentially a mature soil.

Distribution in India

  • Most widespread in: Maharashtra.
  • Also found in: Gujarat (Saurashtra), Madhya Pradesh, Karnataka, Chhattisgarh, and the valleys of the Godavari and Krishna rivers.
  • NOT found in: The Himalayan region.

Agricultural Significance

  • Ideal for cotton cultivation, hence the name ‘Black Cotton soil’.
  • Highly responsive to irrigation.
  • Suitable for crops in low-rainfall areas due to its excellent moisture retention.

2. Laterite Soil

Formation & Characteristics

  • Formation Process:
    • Forms in tropical climates with high temperatures and heavy rainfall.
    • The process of leaching during alternating wet and dry seasons washes away silica and lime.
    • Leaves behind a soil rich in iron and aluminum compounds.
  • Physical Properties:
    • Generally red in colour due to high iron oxide content.
  • Chemical Properties / Fertility:
    • Generally low in fertility.
    • Deficient in: Humus, nitrogen, phosphorus, and lime.
    • Rich in: Iron and aluminum.
    • The presence of excess iron is a key reason for its infertility.

Distribution in India

  • Primary States: Kerala, Maharashtra, Karnataka, Andhra Pradesh, Odisha, West Bengal, Assam, Jharkhand, Meghalaya.
  • Specific Regions: Western Ghats, Eastern Ghats, and the Malabar Coastal Region (Kerala coast).
  • Largest Coverage: The state with the largest area of Laterite soil is Maharashtra.

Agricultural Use

  • Generally not very suitable for widespread agriculture due to poor fertility.
  • Crops that grow well: Tapioca (Cassava) and Cashew nuts.

Clarifications

  • The soil of most of Andhra Pradesh is not laterite; the state has Red and Alluvial soils.
  • Laterite soil is not rich in lime, nitrogen, or potash.
  • It is not well-developed in Rajasthan, Uttar Pradesh, Himachal Pradesh, or Punjab.
  • It is distinct from Alluvial soil.

3. Alluvial Soil

General Importance & Characteristics

  • Considered the most productive and fertile soil in India.
  • It is the largest and most widespread soil group in India.
  • Covers approximately 11 lakh square kilometers (about 33.5% of India’s total land area).
  • A major contributor to India’s agricultural production.
  • Generally has low nitrogen content.
  • Rich in phosphoric acid, potash, and alkalis.

Origin and Formation

  • Primarily formed from sediments deposited by the Himalayas.
  • Also formed in coastal areas when the sea recedes (coastal alluvium).

Geographical Distribution

  • Found extensively in the Indo-Gangetic plains (from Punjab to West Bengal and Assam).
  • Present in the deltas of major rivers like Mahanadi, Godavari, Krishna, and Cauvery.
  • Also found in the valleys of the Narmada and Tapi rivers.
  • Specific example: The districts of Muzaffarpur, Darbhanga, and Champaran in Bihar have newer alluvium soil.

Classification (Khadar and Bhangar)

  • Khadar (Newer Alluvium): Found in floodplains.
  • Bhangar (Older Alluvium):
    • Found in areas above the flood level.
    • Has a pale reddish-brown colour.
    • Contains kankar (calcium carbonate nodules).
    • Also known as “Old Kachhari clay” in the Gangetic plain.

4. Soil Properties (General)

Water Retention Capacity

  • Water holding capacity decreases in the order: Clay > Silt > Sand.
  • Clay soil has the highest water retention capacity due to very small pore spaces.
  • Sandy soil has the minimum water retention capacity due to large pore spaces.
  • False Statement: “Clay has pore spaces of large size.”

Soil Composition

  • Loamy soil is a mixture of sand, clay, and silt (typically around 40% sand, 40% clay, and 20% silt).

5. Other Soils and Regional Distribution

Major Soil Types by Predominant State

  • Alluvial Soil: Predominantly found in Uttar Pradesh.
  • Black Soil: Predominantly found in Maharashtra.
  • Red Soil: Predominantly found in Andhra Pradesh.
  • Desert Soil: Predominantly found in Rajasthan.
  • Karewas Soil: Found in the Kashmir Valley, Himalaya. Useful for cultivating Zafran (a local saffron).

Specific Soil Characteristics

  • Red Soil:
    • Red colour is due to ferric oxides.
    • Deficient in nitrogen, lime, magnesium, phosphates, and humus, but rich in potash.
  • Desert Soil (Western Rajasthan):
    • Has a high content of calcium.
    • Generally alkaline and saline.
  • Himalayan Soil: Not rich in humus.

Soil Particles

  • Clay: Diameter of less than 0.002 mm.
  • Silt: Diameter ranges from 0.002 mm to 0.06 mm.

6. Soil Fertility and Nutrients

Micronutrient Deficiency

  • Zinc is the most deficient micronutrient in Indian soils.

Crops that Improve Fertility

  • Leguminous crops like Pea and Black Gram (Urd) fix atmospheric nitrogen, improving soil fertility.

7. Soil Acidity and Alkalinity

General Properties & Fertility

  • A pH value between 6 and 7 is ideal for nutrient availability and is considered fertile for common crops.
  • Extreme acidity or alkalinity is harmful.

Problem Soils: Usar (Alkali) Soil

  • Usar soil is an alkali soil with a pH greater than 7.
  • Characteristics: Deficient in bacteria, nitrogen, and zinc.
  • Reclamation Methods: Treated with gypsum, pyrites, and green manure. (Lime is not used).
  • Crop Suitability: Tolerant paddy varieties like Narendra Shankar Usar Paddy-1 and Usar Paddy-2.

Saline & Alkali Soil Reclamation

  • Salinization: A Process where irrigation water evaporates, leaving behind salts that make soil impermeable.
  • Reclamation: Gypsum is the primary amendment used for long-term reclamation, followed by leaching with water.

Geographic Distribution of Problem Soils

  • Largest Alkali Soil Area: Uttar Pradesh (35.75% of India’s total). Other states: Gujarat, Maharashtra, Tamil Nadu, Haryana, Punjab.
  • Largest Saline Soil Area: Gujarat (has the largest total area under salt-affected soils).

Crop-Specific Soil Requirements

  • Tea plantation requires acidic soil (low pH).

8. Soil Erosion and Conservation

Types and Process of Erosion

  • The sequential process of water erosion is:
    1. Splash Erosion: Caused by raindrop impact.
    2. Sheet Erosion: Uniform removal of a thin layer of topsoil.
    3. Rill Erosion: Formation of small, removable channels.
    4. Gully Erosion: Formation of deep, permanent channels.
  • Gully erosion is responsible for the formation of the Chambal Ravines.

Critical Erosion Areas in India

  • Barren lands of the Chambal and Yamuna valleys.
  • Foothill areas of the Shiwalik ranges.
  • Chotanagpur Plateau, Malwa Plateau, and the black soil region of Maharashtra.
  • In Madhya Pradesh, the Chambal Valley (districts like Morena, Bhind) is severely affected.

Factors Causing Soil Erosion

  • Major Cause: Deforestation.
  • Not a Cause: Terrace cultivation is a conservation method.
  • Crop Type: Farmland erodes most rapidly with Sorghum and least with Clover.

Soil Conservation Methods

  • Agricultural Practices:
    • Crop Rotation
    • Mixed/Multiple Cropping
    • Allowing crop residue to remain in the field.
    • Reduced/Zero tillage to conserve soil moisture.
  • Physical Structures:
    • Terracing
    • Windbreaks
    • Afforestation
  • Not a conservation method: Seed modification (increases yield but does not enhance soil fertility).

Know More About Soils Resources of India: