Why this chapter matters for UPSC: India's soil types (alluvial, black cotton, red laterite, arid, mountain) — their location, properties, and suitability for crops — are a core GS1 Physical Geography topic and connect to agriculture in GS3. Soil erosion and conservation are GS3 environmental topics.
PART 1 — Quick Reference Tables
India's Major Soil Types
| Soil Type | Region | Properties | Best Crops |
|---|---|---|---|
| Alluvial | Indo-Gangetic plains, river valleys, deltas | Fertile; loamy to clayey; replenished by floods; new (khadar) and old (bhangar); most widespread in India | Wheat, rice, sugarcane, jute, cotton |
| Black (Regur) | Deccan Plateau (Maharashtra, MP, Gujarat, AP) | Formed from basalt (Deccan Traps); self-ploughing (cracks when dry); high moisture retention; poor in nitrogen | Cotton (best), soybean, wheat, jowar |
| Red Laterite | Peninsular India (Tamil Nadu, Karnataka, Kerala, WB, NE) | Formed by leaching in high rainfall; red from iron oxides; low fertility; acidic | Tea, coffee, cashew, rubber (acid-tolerant); rice where irrigated |
| Desert/Arid | Rajasthan, Gujarat (semi-arid) | Sandy; low moisture retention; poor in humus; alkaline | Drought-resistant crops with irrigation; bajra, pulses |
| Mountain | Himalayas, NE hills | Thin; immature; organic-rich in upper slopes; acidic in forest areas | Tea (Darjeeling, Assam on hill slopes), potatoes, apples |
| Saline/Alkaline | Rann of Kutch, some river deltas, waterlogged areas | Excess salt/alkali; infertile without reclamation | Only salt-tolerant species; reclamation with gypsum, drainage |
Soil Profile Horizons
| Horizon | Name | Description |
|---|---|---|
| O | Organic layer | Leaf litter, decomposing organic matter; on surface |
| A | Topsoil | Darkest; most fertile; humus + minerals; most organisms; most root activity |
| B | Subsoil | Less organic; minerals leached down from A; clay accumulation |
| C | Parent material | Partially weathered rock; few organisms |
| R | Bedrock | Unweathered parent rock |
PART 2 — Detailed Notes
Soil Formation
How soil forms (pedogenesis):
Weathering of parent rock:
- Physical: Temperature changes crack rocks; water in cracks freezes and expands; roots break rocks
- Chemical: Rain (weakly acidic) dissolves minerals; oxidation; hydration
- Biological: Lichens secrete acids that etch rock surfaces; roots exert pressure
Accumulation of organic matter:
- Dead plant and animal material accumulates
- Decomposers (bacteria, fungi) break it down → humus (dark, stable organic matter)
- Humus improves water retention, aeration, nutrient content
Soil takes hundreds to thousands of years to form:
- 1 cm of topsoil = ~100–200 years (depends on climate, parent rock)
- Therefore soil is considered a non-renewable resource on human timescales
- Loss of topsoil = permanent loss of agricultural productivity for generations
Soil components:
- Minerals (~45%): From parent rock; provide structure
- Water (~25%): In pore spaces; available to plants
- Air (~25%): In pore spaces; essential for root respiration and aerobic soil organisms
- Organic matter (~5%): Humus; crucial for fertility despite small percentage
Soil Erosion and Degradation
UPSC GS3 — Soil erosion:
Soil erosion: Removal of topsoil by water, wind, or other agents faster than it is formed.
Types:
- Sheet erosion: Thin layer of topsoil removed uniformly by surface runoff — most insidious (invisible)
- Rill erosion: Small channels (rills) carved by concentrated runoff
- Gully erosion: Deep channels carved; creates ravines; "Chambal ravines" in MP/Rajasthan
- Wind erosion: Dry, barren areas; powdery soil blown away; common in Rajasthan, coastlines
- Coastal erosion: Sea waves eroding coastline
Causes of soil erosion:
- Deforestation (roots hold soil; canopy reduces raindrop impact)
- Overgrazing (livestock remove vegetation, expose soil)
- Faulty agricultural practices (ploughing up/down slopes instead of across)
- Flood and heavy rain
- Wind in dry areas
India's soil degradation — authoritative data:
- ISRO Desertification and Land Degradation Atlas (2018-19 data): 97.85 million hectares (29.7% of India's total 328.72 Mha) underwent land degradation — the official satellite-based figure
- Of this, 83.69 million hectares specifically underwent desertification (up from 81.48 Mha in 2003–05 — a worsening 20-year trend)
- Desertification increased in 28 of 31 states/UTs monitored
- Rajasthan tops with 21.23 Mha desertified; Maharashtra second at 14.3 Mha
- 5.3 billion tonnes of soil lost annually through water erosion — ICAR
- Waterlogging + salinisation in canal-irrigated areas (Punjab-Haryana: Green Revolution's negative legacy)
[Additional] Soil Organic Carbon (SOC) and climate change:
- Soil is the world's largest terrestrial carbon store — soils hold ~2,500 gigatonnes of carbon, roughly 3× the amount in the atmosphere and 4× the amount in all living vegetation
- When topsoil erodes or organic matter declines, stored carbon is released as CO₂ → contributes to climate change
- "4 per 1000" Initiative (launched by France at COP21, Paris 2015): If global soil organic carbon content increased by 0.4% (4 per 1,000) per year, it would offset all annual global CO₂ emissions from fossil fuels — illustrating soil's potential as a climate mitigation tool
- India has not formally joined the 4 per 1000 initiative, but improving SOC through organic farming, cover crops, and reducing tillage is increasingly emphasised in India's agricultural policy (PM Pranam, Natural Farming Mission)
Conservation measures:
- Contour ploughing: Plough across slope (along contour lines) rather than up/down → reduces runoff
- Terracing: Cut steps into hillside → reduces slope; allows cultivation without erosion
- Shelter belts: Rows of trees planted around fields → reduce wind erosion (Rajasthan, Punjab)
- Afforestation: Planting trees → roots hold soil; canopy reduces rain impact
- Cover crops: Plant vegetation even in fallow season to keep soil covered
- Check dams: Small dams in ravines slow water → reduces gully erosion; stores water
- Bunding: Earthen embankments around fields to retain rainwater + reduce runoff
[Additional] Key Government Schemes for Soil Health:
- Soil Health Card (SHC) Scheme (2015): Every farmer receives a card with soil nutrient status and recommended fertilizer doses — reduces over-application of chemical fertilizers and soil acidification. Over 23 crore SHCs distributed across two cycles.
- PM Pranam Scheme (2023): PM Programme for Restoration, Awareness, Nourishment, and Amelioration of Mother Earth — incentivizes states to reduce chemical fertilizer use; 50% of savings in fertilizer subsidy given back to the state for soil restoration.
- National Mission for Sustainable Agriculture (NMSA): Part of NAPCC; focuses on soil health management, organic farming, watershed development.
- [Additional] Land Degradation Neutrality (LDN): India's commitment under UNCCD (UN Convention to Combat Desertification) — target to restore 26 million hectares of degraded land by 2030 and neutralise further degradation. NITI Aayog coordinates restoration.
Exam Strategy
Prelims traps:
- Black soil = Regur = Deccan Plateau (from basalt); BEST for cotton (NOT alluvial soil for cotton)
- Alluvial soil = most widespread in India (Indo-Gangetic Plains + deltas + river valleys)
- Laterite soil = acidic, poor in nitrogen (leaching by heavy rain); good for tea, coffee, cashew
- Contour ploughing = across slope (NOT up/down); reduces runoff and erosion
- Topsoil = Horizon A (most fertile, most humus); NOT Horizon B or C
- Soil is non-renewable on human timescales — 100–200 years per cm; critical for sustainable agriculture
- Chambal ravines = severe gully erosion (MP/Rajasthan/UP); worst ravine formation in India
Practice Questions
Prelims:
"Black cotton soil" (Regur) is primarily found in which region of India and is formed from which type of rock?
(a) Deccan Plateau; formed from basalt (Deccan Trap lava flows)
(b) Indo-Gangetic Plain; formed from river alluvium
(c) Rajasthan; formed from sandstone
(d) Western Ghats; formed from granite"Contour ploughing" as a soil conservation measure involves:
(a) Ploughing in the direction of slope to allow water drainage
(b) Ploughing across the slope along contour lines to reduce water runoff and soil erosion
(c) Deep ploughing to break the hardpan layer below the topsoil
(d) Alternating ploughed strips with unploughed strips across a fieldWhich of the following soil types is best suited for tea cultivation due to its well-drained, slightly acidic nature?
(a) Alluvial
(b) Black
(c) Laterite
(d) Desert
BharatNotes