Soils of India: Alluvial Khadar, Black Regur & Laterite

Pedological classification in India is standardized by the Indian Council of Agricultural Research (ICAR), which categorizes the country's pedosphere into eight major soil orders aligned with the United States Department of Agriculture (USDA) Soil Taxonomy. India's territory exhibits wide edaphic diversity driven by parent rock lithology, paleoclimate, and relief. Alluvial soils (classified primarily as Inceptisols and Entisols) form the largest group, occupying approximately forty percent of the total land area across the Indo-Gangetic-Brahmaputra plains and coastal deltas. Black soils (classified as Vertisols or Regur) cover roughly fifteen percent of the country, predominating across the volcanic Deccan lava plateau. These two orders constitute the agricultural foundation of India, sustaining primary cereal, fiber, and commercial cropping belts.

Alluvial soils develop through azonal fluvial deposition of silt transported by perennial Himalayan and peninsular river systems. Geomorphologically, alluvium is divided into Bhangar, the older calcified alluvium situated above historic floodplains containing nodular calcareous concretions termed kankar, and Khadar, the newer, fine-textured alluvium continuously replenished by seasonal inundations. Alluvial profiles contain abundant potash and lime but remain consistently deficient in nitrogen and humus. In contrast, Black or Regur soil forms in situ through the subaerial weathering of Cretaceous basaltic lava rocks. Dominated by montmorillonite clay minerals, Vertisols exhibit high plasticity and moisture retention. During dry periods, severe volumetric shrinkage produces deep vertical fissures that promote soil aeration—a phenomenon known as self-ploughing—which transform into impermeable sticky muds upon hydration. Black soils are well supplied with lime, iron, magnesium, and alumina, yet lack phosphorus, nitrogen, and organic content.

These contrasting soil regimes govern regional cropping patterns: alluvial plains support intensive irrigated cultivation of wheat, rice, and sugarcane, whereas black soils are suited for rainfed cotton, oilseeds, and pulses. However, intensive cultivation has accelerated land degradation, including canal-induced waterlogging and secondary salinization (Reh or Kallar) in northwestern plains, alongside sheet erosion across vertic slopes. Remedial interventions include gypsum treatment, balanced fertilization under the Soil Health Card scheme, and conservation tillage. In UPSC CSE, SSC CGL, and State PSC examinations, Indian pedology is an essential topic. Questions consistently examine the ICAR eight-fold classification, the edaphic contrast between Khadar and Bhangar, the mineral chemistry of montmorillonite, the basaltic origin of Deccan traps, and regional soil conservation measures.

Reviewed by the Master10 Editorial Board for accuracy, clarity and competitive-exam relevance.Editorial Policy

Key Concepts & Self-Assessment15 Key Facts

Review key Soils of India: Alluvial, Black (Regur), Red & Laterite Soils exam facts and rate your mastery to track revision.

Progress: 0/15 Rated 0 Mastered 0 Review Later

#1
ICAR identifies 8 major soil groups in India: Alluvial, Black, Red, Laterite, Arid/Desert, Saline/Alkaline, Peaty/Organic, and Forest soils.
#2
Alluvial soils cover ~40% of total land area, divided into fertile, fine-grained Khadar (new alluvium) and calcified Bhangar (old alluvium).
#3
Black soils (Regur/Vertisols) are rich in montmorillonite clay, exhibit shrinkage-swelling ("self-ploughing"), and excel in cotton cultivation.
#4
Red soils derive their reddish coloration from ferric oxide diffusion in crystalline rocks, turning yellow upon hydration.
#5
Laterite soils develop under alternating wet-dry tropical climates via intense leaching (desilication), leaving iron and aluminum residual crusts.
#6
The Indian Council of Agricultural Research (ICAR) classifies Indian soils according to the USDA Soil Taxonomy, identifying Inceptisols and Entisols as the most widespread soil orders.
#7
Khadar soils occupy river floodplains, renewed annually by seasonal silt deposits, making them highly fertile without requiring heavy chemical fertilizers.
#8
Bhangar soils are older alluvium found above the flood plains, containing calcareous concretions known as 'Kankar' and displaying darker, clayey textures.
#9
Black soils are chemically deficient in nitrogen, phosphorus, and organic matter, but naturally rich in potash, calcium carbonate, magnesium, and alumina.
#10
Red and Yellow soils occupy approximately 18% of India's geographical area, predominant across the Deccan plateau, Eastern Ghats, and parts of Odisha and Chhattisgarh.
#11
Laterite soils are strongly acidic with low silica-sesquioxide ratios, making them deficient in nitrogen, phosphate, and calcium, but suitable for cashew and tea with fertilizer support.
#12
Arid and Desert soils (Aridisols) cover western Rajasthan and northern Gujarat, containing high soluble salt concentrations and low humus due to rapid evaporation.
#13
Saline and Alkaline soils (known locally as Reh, Usar, Kallar, or Chopan) contain high amounts of sodium, magnesium, and calcium salts, reclaimable through gypsum application and subsurface drainage.
#14
Peaty and Organic soils (Kari) occur in high-rainfall coastal regions like Kottayam and Alappuzha in Kerala, characterized by high organic matter (40–50%) and heavy black texture.
#15
The Soil Health Card Scheme was launched by the Union Government on 19 February 2015 at Suratgarh, Rajasthan, testing twelve macro- and micro-nutrient soil parameters.

Subject Specialist Commentary

Analytical perspective & practical exam advice from the Master10 academic board

Educator's Insight

India's soils are classified into eight major groups by the Indian Council of Agricultural Research. Alluvial soils cover about 40 percent of the country, split into fertile new Khadar and older calcified Bhangar. Formed from Deccan basalt, Black soils (Regur) feature high clay content and moisture retention, ideal for cotton farming. Red soils gain their reddish color from iron diffusion, while Laterite soils develop in tropical regions through intense rainwater leaching.

Soil traits appear frequently in UPSC and State PSC prelims papers. Note the "self-ploughing" nature of Black soil: it shrinks and cracks deeply when dry, swelling when wet. A common question trap confuses Khadar and Bhangar: remember Khadar is fresh flood alluvium, while Bhangar contains older kankar nodules. Also remember that Laterite soils lose silica through leaching, leaving iron and aluminum crusts suited for cashew and coffee.

Soils of India: Alluvial Khadar, Black Regur & Laterite

Key Concepts & Self-Assessment15 Key Facts

Subject Specialist Commentary

Related Knowledge Topics to Discover

Looking for more GK practice?