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India Soils Pedology — Black Regur soil shrinking clay cracks with a cotton plant silhouette, Laterite weathering leached steps under red iron oxide washing rain, and Alluvial Indo-Gangetic delta channels depositing fertile grey sand silts BLACK REGUR CLAY Self-ploughing Deccan basalt LEACHED LATERITE Silica washed, iron baked hard ALLUVIAL SILT Indo-Gangetic Khadar & Bhangar PEDOLOGY: BASALT LAVA DECCAN, GRANITE PENINSULAR CRYSTALS, AND SILT DELTAS

Soils of India: Classifications, Properties, and Agriculture — Complete Guide

Geography GK • Pedology 17 min read Updated: July 21, 2026

🌱 Key Takeaways

45% share
Alluvial soil: largest group in India
15% share
Black Regur: Deccan cotton giant
18.5% share
Red & Yellow: peninsular iron block
0.75% Target
Ideal soil organic carbon (SOC) level

Table of Contents

  1. The 5 Soil Architects: Weathering and Genesis
  2. Alluvial Soil: Fertile Indo-Gangetic Plains
  3. Black Soil (Regur): Tectonic Deccan Basalt
  4. Red and Yellow Soil: Peninsular Crystalline Gneiss
  5. Laterite Soil: Leached Slopes and plantation
  6. Arid, Mountain, Saline, and Peaty Soils
  7. The Modern Crisis: Degradation and Reclamation
  8. Soils of India Specifications Matrix
  9. Exam-Oriented Quick Revision Points
  10. Frequently Asked Questions

The 5 Soil Architects: Weathering and Genesis

In earth sciences, pedology is the study of soils in their natural environment, detailing how parent rock minerals, atmospheric climate, topography slope drainage, biological humus, and geological time interact.

For competitive exams like the UPSC Civil Services, state PSCs, and SSC CGL, understanding soil groups, chemical profiles, and agricultural distributions is essential. Let's study these systems.

Alluvial Soil: Fertile Indo-Gangetic Plains

Sourced from the Indus, Ganga, and Brahmaputra river networks, alluvial soils cover 43-45% of India:

Black Soil (Regur): Tectonic Deccan Basalt

Covering 15-16.6% of India (Maharashtra, MP, Gujarat):

Red and Yellow Soil: Peninsular Crystalline Gneiss

Found across 18.5% of the peninsular block:

Laterite Soil: Leached Slopes and plantation

Covers 4.3% of the land (Western Ghats summits, Kerala, Assam hills):

Arid, Mountain, Saline, and Peaty Soils

These soils represent specialized climatic and geographic developments:

The Modern Crisis: Degradation and Reclamation

Modern intensive cultivation places stress on subcontinental soils:

Soils of India Specifications Matrix

Soil GroupLand Share (%)Parent Rock / OriginChemical HighlightsStar Crop Varieties
Alluvial~43–45%Himalayan river silts (Ganga, Indus)Rich in Potash & Lime; Low in NitrogenRice, Wheat, Sugarcane, Jute
Red & Yellow~18.5%Peninsular crystalline graniteRich in Iron Oxide; Low in HumusRagi, Millets, Groundnut, Pulses
Black (Regur)~15–16%Deccan Traps cooled basaltic lavaRich in Calcium & Magnesia; High clayCotton, Soybean, Wheat, Jowar
Laterite~4.3%Leached tropical escarpmentsRich in Iron & Alum; Poor in SilicaCashew, Coffee, Tea, Rubber
Arid / Desert~4.3–4.4%Wind-blown desert sands (Thar)High soluble salts; Kankar calcium layersBajra, Jowar, Guar, Mustard
Forest / Mountain~3.7%High elevation forest litterHigh humus; acidic on exposed slopesApples, Tea, Saffron, Spices
Saline (Usar)~2.1%Waterlogged capillary crustsHigh Sodium & Magnesium saltsSalt-tolerant barley (after gypsum)
Peaty (Kari)~1.1%Anaerobic organic delta marshesExtremely high humus (up to 50%)Paddy, Mangrove ecosystems

Exam-Oriented Quick Revision Points

Frequently Asked Questions

What is the difference between Khadar and Bhangar alluvial soils?

Khadar is the young, light-colored, highly fertile alluvial soil deposited annually by rivers in floodplains. Bhangar is the older, darker, more clayey alluvial soil found on elevated terraces above flood levels, containing calcium carbonate nodules (Kankar).

Why is black soil called 'self-ploughing'?

Black soil contains swelling clays. When dry, it shrinks and forms deep, wide cracks that allow organic debris to fall in. When wet, it swells and closes up, naturalizing and mixing the soil layers without manual turning.

How is laterite soil formed and what are its properties?

Laterite soil forms under high temperatures and heavy monsoon cycles through intense leaching. Soluble silica, lime, and potash are washed down, leaving behind iron and aluminum oxides. It is soft when wet and bakes rock-hard when dry.

What makes red soil red, and why does it sometimes appear yellow?

The reddish color comes from ferric oxide coatings on soil grains, weathered from granite. In low-lying, poorly drained valley areas, hydration transforms it into yellow-shaded hydrated iron oxide.

What is the Kankar layer in desert soil?

The Kankar layer is a hard sub-surface accumulation of calcium carbonate nodules. Found in arid soils, it blocks deep root penetration and limits water infiltration, requiring management for agriculture.

What is Usar or Reh soil, and how is it reclaimed?

Usar or Reh is saline/alkaline soil with a white salt crust formed by capillary action from over-irrigation. It is reclaimed by adding Gypsum (calcium sulphate) to displace sodium, flushing with water, and planting salt-tolerant crops.

What are the Bhabar and Terai zones?

Bhabar is a porous, pebble-strewn strip at the base of the Shivaliks where mountain streams sink underground. Terai is the marshy, jungle-rich zone just south of Bhabar where streams re-emerge, providing fertile soils for rice and sugarcane.

What are the primary chemical deficiencies in most Indian soils?

Due to intense cultivation and tropical climates, most Indian soils are deficient in Nitrogen, Phosphorus, and Organic Humus, though they are generally rich in Potash.

What are Laurasia and Gondwanaland?

When the supercontinent Pangea split during the Mesozoic era, it divided into two smaller supercontinents: Laurasia in the Northern Hemisphere (consisting of North America, Europe, and Asia) and Gondwanaland in the Southern Hemisphere (consisting of South America, Africa, India, Australia, and Antarctica).

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