Why this chapter matters for UPSC: Soils was Chapter 6 of India: Physical Environment until NCERT's rationalisation. It is not in the current reprint (2026-27), whose six chapters end with Natural Hazards and Disasters. This page follows the pre-rationalised text (2021-22 reprint) and adds the soil section of the current Class 10 book (Contemporary India II, Chapter 1), which still covers Indian soils. "Indian soils" is still listed in the UPSC Prelims geography syllabus. Mains asks about soils in GS1 resource questions and GS3 land-degradation questions.
Contemporary hook: The Soil Health Card Scheme completed ten years on 19 February 2025. By that month 24.74 crore cards had been generated, and since 2022-23 the scheme has run as the "Soil Health & Fertility" component of the Rashtriya Krishi Vikas Yojana (PIB, 19 Feb 2025).
🧠 First Principles — Read This First
Soil is the loose layer on the land surface. It is a mixture of rock particles, decayed plant and animal matter (humus), water and air. Plants take water and nutrients from it, and most of our food grows in it.
Soil forms when weathering breaks down a parent rock and living things add organic matter. NCERT names five controlling factors: relief, parent material, climate, vegetation and other life-forms, and time. Human activity is a sixth influence. The process is slow. The Class 11 text says soil has "evolved over thousands of years", and the Class 10 text says it takes "millions of years" to build a few centimetres. Either way, soil lost to erosion is not replaced within a human lifetime.
Two ideas explain most of the chapter. The first is that the parent material sets the starting chemistry. Basalt lava weathers into clay-rich black soil, old crystalline rocks give red soil, and river sediment gives alluvium. The second is that climate decides what happens to that material. Heavy tropical rain washes away lime and silica and leaves iron and aluminium behind, which produces laterite. In a dry climate, evaporation pulls salts to the surface and leaves sandy, saline arid soil.
Picture two pots of the same garden soil, one left in a dry corner and one watered every day for years. Their soils end up different, and the same thing happens across India's regions.
UPSC tests this chapter through soil-to-region and soil-to-crop matching in Prelims, and through land degradation and conservation in GS1 and GS3.
PART 1 — Quick Reference
Table 1: Factors of soil formation (NCERT)
| Factor | What it controls | Example from the chapter |
|---|---|---|
| Relief | Drainage, depth, and how fast soil is removed | Gully erosion is common on steep slopes |
| Parent material | Mineral make-up and texture | Red soil develops on crystalline igneous rocks |
| Climate | Weathering, leaching and evaporation | Laterite forms under high temperature and heavy rain |
| Vegetation and other life-forms | Humus and binding of soil by roots | Peaty soils form where dense vegetation leaves much dead organic matter |
| Time | How mature the soil is | Khadar is new alluvium and bhangar is older alluvium |
| Human activity (NCERT: "also influence it to a large extent") | Erosion, salinity and loss of fertility | Over-irrigation makes alluvium saline in Green Revolution areas |
Source: NCERT, India: Physical Environment, Class 11, Ch. 6 "Soils" (2021-22 reprint).
Table 2: The soil profile (NCERT)
| Horizon | Position | Contents |
|---|---|---|
| Horizon A | Topmost | Organic matter mixed with mineral matter, nutrients and water. This is the zone plants use. |
| Horizon B | Transition zone | Material from above and below, some organic matter, and noticeably weathered minerals |
| Horizon C | Lowest soil layer | Loose parent material, the first stage of soil formation |
| Bedrock | Below the three horizons | Unweathered parent rock |
Source: NCERT Class 11 IPE, Ch. 6 (2021-22). NCERT describes three horizons above the bedrock. The O (litter) and R (bedrock) labels used in soil-science textbooks are not part of the NCERT scheme.
Table 3: ICAR classification of Indian soils by USDA Soil Taxonomy order
| Order | Area (thousand ha) | Share of total (%) |
|---|---|---|
| Inceptisols | 1,30,372.90 | 39.74 |
| Entisols | 92,131.71 | 28.08 |
| Alfisols | 44,448.68 | 13.55 |
| Vertisols | 27,960.00 | 8.52 |
| Aridisols | 14,069.00 | 4.28 |
| Ultisols | 8,250.00 | 2.51 |
| Mollisols | 1,320.00 | 0.40 |
| Others | 9,503.10 | 2.92 |
Source: Soils of India, National Bureau of Soil Survey and Land Use Planning (NBSS&LUP, ICAR), Publication No. 94, as printed in NCERT Class 11 IPE, Ch. 6 (2021-22 reprint, archived copy). The table lists seven orders plus "Others". Inceptisols are the largest order, not Vertisols (the black-soil order).
Table 4: The eight soil groups (NCERT: classified "on the basis of genesis, colour, composition and location")
| Soil | Where (NCERT) | Character (NCERT) | Crops named in NCERT |
|---|---|---|---|
| Alluvial | Northern plains and river valleys; through a narrow corridor in Rajasthan into the Gujarat plains; east-coast deltas | Covers "about 40 per cent of the total area of the country". Depositional (transported by rivers). Sandy loam to clay. Generally rich in potash, poor in phosphorus. Light grey to ash grey. | Sugarcane, paddy, wheat, other cereals and pulses (Class 10) |
| Black (regur, black cotton) | Most of the Deccan Plateau: Maharashtra, MP, Gujarat, Andhra Pradesh, parts of Tamil Nadu. Very deep in the upper Godavari and Krishna and the north-western Deccan. | Clayey, deep, impermeable. Swells when wet and cracks when dry ("self-ploughing"). Holds moisture for long. Rich in lime, iron, magnesia and alumina, and contains potash. Lacks phosphorus, nitrogen and organic matter. | Cotton ("ideal for growing cotton", Class 10) |
| Red and yellow | Eastern and southern Deccan on crystalline igneous rocks in low-rainfall areas; piedmont of the Western Ghats (red loamy); Odisha, Chhattisgarh, southern middle Ganga plain | Red from iron diffused through crystalline and metamorphic rocks, yellow when hydrated. Fine-grained types are normally fertile; coarse-grained upland types are poor. Generally poor in nitrogen, phosphorus and humus. | Not specified |
| Laterite | Higher areas of the Peninsular plateau: Karnataka, Kerala, Tamil Nadu, MP, hilly Odisha and Assam | Formed by intense leaching: lime and silica removed, iron oxide and aluminium left. Poor in organic matter, N, P and Ca; iron oxide and potash in excess. Acidic (pH < 6.0, Class 10). Cut as bricks. | Cashew on red laterite (TN, AP, Kerala); tea and coffee after soil conservation in the hills of Karnataka, Kerala and TN (Class 10) |
| Arid | Western Rajasthan | Red to brown, sandy, saline. Lacks moisture and humus. Nitrogen insufficient, phosphate normal. Kankar layers in lower horizons. | Becomes cultivable with irrigation (western Rajasthan) |
| Saline (usara) | Western Gujarat, east-coast deltas, Sundarbans; Rann of Kachchh (salt crust); irrigated Green Revolution areas such as Punjab and Haryana | Excess sodium, potassium and magnesium, so infertile. Lacks nitrogen and calcium. Sandy to loamy. | Remedy: add gypsum (NCERT advice for Punjab and Haryana) |
| Peaty | North Bihar, southern Uttarakhand, coastal West Bengal, Odisha and Tamil Nadu | Heavy rainfall and humidity, dense vegetation. Organic matter up to 40-50%. Heavy and black, "at many places" alkaline. | Not specified |
| Forest | Forest areas with enough rainfall; mountain slopes | Loamy and silty on valley sides, coarse on upper slopes. Acidic with low humus in snow-bound Himalaya. Fertile in lower valleys. | Not specified |
Sources: NCERT Class 11 IPE, Ch. 6 (2021-22); NCERT Class 10 Contemporary India II, Ch. 1 "Resources and Development" (Reprint 2026-27). Areas in hectares for these eight groups are not given here: NCERT gives only the alluvial share (about 40%), and no single official table of group-wise areas was found to cite.
Table 5: How much of India's land is degraded? Two official figures
| Estimate | Area | Basis | Source |
|---|---|---|---|
| NBSS&LUP (2004) | ~146.8 Mha (~147 Mha) | Soil-degradation mapping by type: water erosion 94, acidification 16, flooding 14, wind erosion 9, salinity 6, combination 7 Mha | Bhattacharyya et al., "Soil Degradation in India: Challenges and Potential Solutions", Sustainability 7(4):3528-3570, 2015, citing NBSS&LUP (2004) |
| ISRO-SAC Desertification and Land Degradation Atlas (released 17 Jun 2021) | 97.84 Mha in 2018-19 | Satellite mapping of land degradation and desertification processes | PIB, MoEFCC Lok Sabha reply, 7 Aug 2023; PIB release of the Atlas, 17 Jun 2021 |
| NCERT (2021-22) | "about half of the total land of India" | Text estimate, no source given | NCERT Class 11 IPE, Ch. 6 |
The two official figures measure different things and should not be compared as a trend. NBSS&LUP mapped soil degradation by type, while ISRO-SAC mapped land degradation and desertification processes from satellite data. Against India's total geographical area of 328.7 Mha (Bhattacharyya et al. 2015), 97.84 Mha works out to about 29.8%. That percentage is arithmetic on the two cited figures, not a published number.
PART 2 — Concepts & Narrative
How Indian soils came to be classified
People have long grouped soils by how they look and how well they grow crops. NCERT traces the history in three steps:
- Ancient period. Soils were classified as urvara (fertile) and usara (sterile).
- 16th century. Classification used inherent characteristics and external features: texture (sandy, clayey, silty, loam), colour (red, yellow, black), slope and moisture.
- After Independence. The Soil Survey of India (established 1956) surveyed selected areas such as the Damodar Valley. The National Bureau of Soil Survey and Land Use Planning, an ICAR institute, then classified Indian soils according to the USDA Soil Taxonomy so that they could be compared internationally (Table 3).
The eight-group list in Table 4 is a separate scheme based on genesis, colour, composition and location. Prelims questions can use either vocabulary. "Vertisols" are the black soils, and "Aridisols" broadly correspond to the arid soils.
Khadar and bhangar. These are the two kinds of alluvium in the upper and middle Ganga plain. Khadar is new alluvium, deposited every year by floods, which leave fine silt that enriches it. Bhangar is older alluvium lying away from the floodplain. NCERT Class 11 says that both contain calcareous concretions (kankar). NCERT Class 10 adds that bhangar has a higher concentration of kankar nodules, and that khadar has more fine particles and is more fertile. Kankar is therefore not unique to bhangar: it is present in both and more concentrated in bhangar.
Alluvial soils
Rivers carry and deposit alluvial soil rather than forming it from the rock underneath. NCERT puts its extent at about 40% of the country. That makes it the most widespread group by NCERT's genesis classification, and Class 10 calls it "the most widely spread and important soil". Its character changes in three ways:
- Texture changes downstream. It is coarse near the break of slope in piedmont plains (Class 10 names the Duars, Chos and Terai), becomes more loamy and clayey in the lower and middle Ganga plain and the Brahmaputra valley, and its sand content falls from west to east.
- Colour depends on depth, texture and age. It ranges from light grey to ash grey.
- Chemistry. Class 11 calls it generally rich in potash and poor in phosphorus. Class 10 says it contains "adequate proportion of potash, phosphoric acid and lime". The two books disagree on phosphorus. For a Class 11-based answer, use "rich in potash, poor in phosphorus".
The Class 10 book adds that in drier areas alluvial soils are more alkaline and can be made productive with treatment and irrigation. Alluvial regions are intensively cultivated and densely populated.
Why black soil holds water, and why that matters for cotton. Black soil is made of very fine clay. Clay absorbs water slowly and also gives it up slowly. That is why NCERT says black soil "retains the moisture for a very long time, which helps the crops, especially, the rain fed ones, to sustain even during the dry season." When the clay dries, it shrinks and develops wide cracks. Topsoil falls into the cracks and the soil gets aerated, which NCERT calls "self-ploughing". The same clay makes the soil sticky when wet, so Class 10 notes that it is hard to work unless tilled right after the first shower or before the monsoon.
Chemically, black soil is rich in lime, iron, magnesia and alumina and contains potash. It is poor in phosphorus, nitrogen and organic matter. Its colour ranges from deep black to grey. Its parent material is the basalt of the Deccan Traps, and Class 10 adds that climate together with this parent rock decides how it forms. NCERT does not say what causes the dark colour. Some older textbooks attribute it to titaniferous magnetite, but the NCERT text does not, and this page no longer states that as fact.
Red, yellow and laterite soils: the colour of iron
Red and laterite soils both owe their colour to iron, but they form in different ways.
- Red soil. Iron is spread through crystalline and metamorphic rocks. When those rocks weather, mostly in low-rainfall parts of the eastern and southern Deccan, the iron gives a red colour. Where the iron is hydrated, the soil turns yellow. Fertility depends on texture: fine-grained red soil is normally fertile, while coarse upland red soil is poor.
- Laterite. Laterite forms through leaching. Under high temperature and heavy rain, water removes lime and silica and leaves iron oxide and aluminium compounds. Bacteria that thrive in the heat also break down humus quickly. The result is poor in organic matter, nitrogen, phosphate and calcium, with excess iron oxide and potash. Class 11 says laterites are "not suitable for cultivation" without manures and fertilisers. Class 10 says laterite develops under an alternation of wet and dry seasons and is acidic (pH below 6.0). Where it supports forests it can be rich in humus. With soil conservation on the hills of Karnataka, Kerala and Tamil Nadu it grows tea and coffee, and red laterite in Tamil Nadu, Andhra Pradesh and Kerala suits cashew.
The name comes from the Latin later (brick), because the soil hardens and is cut into bricks for houses (NCERT).
Arid, saline, peaty and forest soils
- Arid soils (western Rajasthan). These are red to brown, sandy and saline. In places the salt content is high enough that common salt is obtained by evaporating the water. Calcium increases with depth and forms kankar layers in the lower horizons. NCERT notes that this layer restricts infiltration, so irrigation water stays available to plants. The soils are poor in humus and nitrogen, but phosphate is normal.
- Saline soils (usara). These contain more sodium, potassium and magnesium, which makes them infertile. NCERT gives three origins: a dry climate with poor drainage, seawater intrusion in deltas, and over-irrigation in the Green Revolution areas, where capillary action lifts salt to the surface. NCERT recommends gypsum for Punjab and Haryana. ICAR-CSSRI puts the salt-affected area at about 6.73 million ha, 2.1% of the geographical area, with sodic soils concentrated in the alluvial soils of the Indo-Gangetic plains (ICAR, citing ICAR-CSSRI Karnal; page accessed 1 Oct 2026). In soil science, saline soils (excess soluble salts) are distinguished from sodic (alkali) soils (excess exchangeable sodium, high pH). The ICAR-CSSRI reclamation example on that page reports sodic soils with pH 8.5-10.1, reclaimed with gypsum and pressmud.
- Peaty soils. These form where heavy rain, high humidity and dense vegetation leave large amounts of dead organic matter, up to 40-50%. They are heavy, black and in many places alkaline. NCERT's regions are north Bihar, southern Uttarakhand, and coastal West Bengal, Odisha and Tamil Nadu.
- Forest soils. These vary with the mountain environment: loamy and silty on valley sides, coarse on upper slopes, acidic and low in humus in the snow-bound Himalaya, and fertile on lower valley terraces and alluvial fans.
Soil erosion: sheet, gully and wind. Soil formation and erosion go on together, and NCERT describes them as normally in balance. Erosion becomes a problem when deforestation, overgrazing, construction or poor farming upsets that balance.
- Sheet erosion takes place on level land after heavy rain. It is hard to notice but removes the finest, most fertile topsoil.
- Gully erosion is common on steep slopes. Gullies deepen with each rain and cut farmland into small, unusable fragments. Land with many deep gullies is badland topography, and in the Chambal basin these are called ravines. NCERT also names Tamil Nadu and West Bengal and says India loses "about 8,000 hectares of land to ravines every year". NCERT gives no date or source for this figure.
- Wind erosion matters most in arid and semi-arid regions.
The Class 11 exercise identifies water erosion as the main cause of topsoil loss in India. Eroded material silts up rivers, reduces their carrying capacity and makes floods more frequent. A national estimate often quoted is about 5.3 billion tonnes of soil lost per year, at about 16.4 t/ha/yr. This is a 1983 estimate (Dhruvanarayana and Ram, Journal of Irrigation and Drainage Engineering 109:419-434), cited in Bhattacharyya et al. (2015). It is not a current measurement.
Soil degradation: what NCERT says and what the official figures add
NCERT defines soil degradation as "the decline in soil fertility, when the nutritional status declines and depth of the soil goes down due to erosion and misuse". Besides erosion, it names three causes:
- Over-irrigation brings salt up from lower soil layers to the surface.
- Chemical fertilisers used without organic manure harden the soil and lower its fertility in the long run. NCERT says this problem is common in the command areas of river-valley projects, which were the first beneficiaries of the Green Revolution.
- Over-grazing and shifting cultivation remove the natural vegetation cover.
NCERT gives the extent only as "about half of the total land of India". The two official national estimates in Table 5 are lower and use different methods. Class 10 adds a regional pattern for land degradation: mining in Jharkhand, Chhattisgarh, MP and Odisha; overgrazing in Gujarat, Rajasthan, MP and Maharashtra; and over-irrigation with waterlogging, salinity and alkalinity in Punjab, Haryana and western UP.
Soil conservation
NCERT's starting rule is that land with a slope gradient of 15-25% should not be cultivated. If it must be farmed, it should be terraced. The other measures are:
| Measure | Purpose (NCERT) |
|---|---|
| Contour bunding, contour terracing, contour ploughing | Slow the run-off down slopes |
| Terracing | Removes finger gullies and restricts erosion on slopes. Well developed in the western and central Himalaya (Class 10). |
| Check dams | Reduce the erosive speed of water in larger gullies |
| Gully plugging, terracing, cover vegetation | Stop gullies from extending headward |
| Regulated forestry, controlled grazing, cover cropping, mixed farming, crop rotation | General remedies |
| Strip cropping (strips of grass between crops) | Break the force of the wind (Class 10) |
| Shelter belts and agro-forestry | Protect cultivable land from encroaching sand dunes |
| Converting land unfit for cropping into pasture | Keeps it under cover |
| Sand-dune stabilisation | Trials in western Rajasthan by the Central Arid Zone Research Institute (CAZRI) |
Source: NCERT Class 11 IPE, Ch. 6 (2021-22); NCERT Class 10 Contemporary India II, Ch. 1 (2026-27).
NCERT notes that the Central Soil Conservation Board prepared conservation plans for different regions, but calls them "fragmental". It recommends integrated land-use planning instead: classify land by its capability, map it, and put it to the right use.
Soil Health Card Scheme (beyond NCERT). The Prime Minister launched the scheme on 19 February 2015 at Suratgarh, Rajasthan. Each card reports 12 parameters:
- Macronutrients: N, P, K, S
- Micronutrients: Zn, Fe, Cu, Mn, B
- Others: pH, electrical conductivity (EC) and organic carbon (OC)
So the card covers 9 nutrients plus 3 soil properties, not "12 nutrients". It also recommends fertiliser doses and soil amendments. By February 2025, 24.74 crore cards had been generated and 665 village-level soil testing labs had been set up in 17 states. Since 2022-23 the scheme has been the "Soil Health & Fertility" component of RKVY (PIB backgrounder, 19 Feb 2025).
PART 3 — UPSC Integration
Cross-paper relevance
- GS1 (geography): distribution of soils as a natural resource. Real questions: the natural-resource potential of the Deccan Trap (gs1-pyq-2022-09), desertification beyond climatic boundaries (gs1-pyq-2020-06), and the Green Revolution bypassing the east "despite fertile soil" (gs1-pyq-2014-04).
- GS3 (agriculture, environment): land degradation, salinity from irrigation, and soil-health policy. The closest bank question is micro-watershed development in drought-prone regions (gs1-pyq-2016-20, set in GS1).
How the bank questions use this chapter
| Bank ID | Question (exact) | Material from this chapter |
|---|---|---|
| gs1-pyq-2022-09 (2022, 10 marks) | "Discuss the natural resource potentials of the Deccan Trap." | Black soil from Deccan basalt: moisture retention and suitability for cotton |
| gs1-pyq-2020-06 (2020, 10 marks) | "The process of desertification does not have climatic boundaries. Justify with examples." | Degradation through salinity from over-irrigation and through erosion. The SAC atlas figure (Table 5) separates desertification from land degradation. |
| gs1-pyq-2014-04 (2014, 10 marks) | "Why did the Green Revolution in India virtually bypass the eastern region despite fertile soil and good availability of water?" | Alluvial soils of the eastern plains: the question assumes they are fertile |
| gs1-pyq-2016-20 (2016) | "In what way micro-watershed development projects help in water conservation in drought-prone and semi-arid regions of India?" | Contour bunding, check dams and gully plugging (conservation table) |
PYQ note: No Prelims question on soils is in the bank file that this site resolves (prelims/2026/gs1.json), so prelims_pyq_ids is empty.
Mains frames that need this chapter
- Soil, crop and region. Black soil and rain-fed cotton. Alluvium and the intensively cropped plains. Laterite, which becomes useful for plantations and cashew only with conservation and inputs.
- The irrigation paradox. NCERT's own example: the Green Revolution command areas that first gained from canal irrigation are the ones where over-irrigation, salinity and fertiliser use without manure now degrade the soil.
- Measurement. Two official degradation figures (Table 5) use different methods. A good answer names the source and year of each figure it uses.
Exam Strategy
Prelims fact-traps from this chapter:
- Largest USDA order is Inceptisols (39.74%), followed by Entisols (28.08%). Vertisols (the black-soil order) are 8.52% (NBSS&LUP Pub. 94, via NCERT).
- Alluvial share: NCERT says "about 40 per cent". Figures like 43% that appear in some guides are not from NCERT.
- Kankar is in both khadar and bhangar (Class 11) and more concentrated in bhangar (Class 10). A statement that "only bhangar contains kankar" is false.
- Laterite has iron oxide and potash in excess. It is poor in N, P, Ca and organic matter, and acidic (pH < 6.0).
- Black soil is rich in lime, iron, magnesia and alumina and contains potash. It is poor in phosphorus, nitrogen and organic matter.
- Saline-soil regions in NCERT are western Gujarat, the east-coast deltas, the Sundarbans and the Rann of Kachchh. Punjab and Haryana appear as irrigation-induced cases, with gypsum as the remedy.
- Peaty soils can be alkaline in many places (NCERT), so do not mark them as always acidic. Organic matter is up to 40-50%.
- Slope rule: land with a 15-25% gradient should not be cultivated, and should be terraced if it must be farmed.
- Soil Health Card: 12 parameters, of which 9 are nutrients. Launched at Suratgarh on 19 Feb 2015.
Mains pattern: Questions on soils come through other themes: resources of a region (Deccan Trap), desertification, regional disparity in agriculture, and watershed management. Write the soil facts into those frames instead of describing the soils in a list.
Practice Questions
- UPSC Mains GS1 2022 (bank ID gs1-pyq-2022-09, 10 marks): "Discuss the natural resource potentials of the Deccan Trap."
- UPSC Mains GS1 2020 (bank ID gs1-pyq-2020-06, 10 marks): "The process of desertification does not have climatic boundaries. Justify with examples."
- Practice (UPSC-pattern, not a past paper): With reference to Indian soils, consider the following statements: (1) Both khadar and bhangar contain calcareous concretions. (2) Inceptisols occupy the largest area among USDA soil orders in India. (3) Laterite soils have excess iron oxide and potash but are poor in nitrogen and phosphate. Which of the statements given above are correct? (All three, per NCERT Class 11, 2021-22.)
- Practice (UPSC-pattern, not a past paper): "India's land-degradation estimates range from about 98 to about 147 million hectares." Explain why official estimates differ, and suggest how soil conservation should be targeted. (15 marks)
📦 Revision Capsule
Hard Facts
- Soils is the pre-rationalised IPE Chapter 6 and is not in the current 2026-27 reprint. Indian soils are still covered in Class 10 Contemporary India II, Ch. 1.
- Soil-forming factors (NCERT): relief, parent material, climate, vegetation and other life-forms, time, plus human activity
- Profile (NCERT): Horizon A (organic + mineral), Horizon B (transition), Horizon C (loose parent material), then bedrock
- USDA orders (NBSS&LUP Pub. 94): Inceptisols 39.74%, Entisols 28.08%, Alfisols 13.55%, Vertisols 8.52%, Aridisols 4.28%, Ultisols 2.51%, Mollisols 0.40%, Others 2.92%
- Eight NCERT groups: alluvial, black, red and yellow, laterite, arid, saline, peaty, forest
- Alluvial covers about 40% of India (NCERT). It is rich in potash and poor in phosphorus.
- Kankar occurs in both khadar and bhangar, with a higher concentration in bhangar (Class 10)
- Black soil: rich in lime, iron, magnesia, alumina and potash; lacks P, N and organic matter; self-ploughing
- Laterite: iron oxide and potash in excess; poor in organic matter, N, P, Ca; pH < 6.0; cashew on red laterite
- Peaty soils: organic matter up to 40-50%; alkaline at many places
- Salt-affected soils: 6.73 Mha, 2.1% of geographical area (ICAR-CSSRI)
- Soil Health Card: launched 19 Feb 2015 at Suratgarh; 12 parameters; 24.74 crore cards generated by Feb 2025 (PIB)
Core Concepts
- Parent material sets the chemistry and climate reworks it: basalt gives black soil, leaching gives laterite, evaporation gives saline arid soil
- Clay holds water, which is why black soil carries rain-fed crops through the dry season
- Heavy rain removes nutrients, so laterite is poor without inputs
- Over-irrigation without drainage turns fertile alluvium saline
Confused Pairs
- Khadar (new, flood-renewed, more fertile) vs bhangar (old, away from floodplain, more kankar)
- Saline soils (excess soluble salts) vs sodic/alkali soils (excess sodium, high pH, reclaimed with gypsum)
- NBSS&LUP ~147 Mha (soil degradation by type) vs ISRO-SAC 97.84 Mha in 2018-19 (land degradation and desertification)
Data Points
- Degraded area: ~146.8 Mha (NBSS&LUP 2004) vs 97.84 Mha (ISRO-SAC, 2018-19). The two use different methods.
- Soil loss ~5.3 billion t/yr is a 1983 estimate (Dhruvanarayana and Ram)
PYQ Pattern
- Mains GS1 brings soils in through regional resources (gs1-pyq-2022-09), desertification (gs1-pyq-2020-06), agricultural disparity (gs1-pyq-2014-04) and watershed management (gs1-pyq-2016-20). The Prelims bank used by this site has no soil question.
Sources
Sources
- NCERT, India: Physical Environment (Class 11), Chapter 6 "Soils", 2021-22 reprint (pre-rationalised). Archived copy, Wayback Machine, 18 Oct 2021. Includes the ICAR table sourced to NBSS&LUP Soils of India, Publication No. 94.
- NCERT, India: Physical Environment (Class 11), contents page, Reprint 2026-27 (kegy1ps.pdf): six chapters, Soils absent.
- NCERT, Contemporary India II (Class 10), Chapter 1 "Resources and Development", Reprint 2026-27. jess101.pdf
- Bhattacharyya, R. et al., "Soil Degradation in India: Challenges and Potential Solutions", Sustainability 7(4):3528-3570 (2015). MDPI
- PIB (MoEFCC), "Government releases Desertification and Land Degradation Atlas of India", 17 Jun 2021. PIB
- PIB (MoEFCC), "Land Degradation and Desertification", Lok Sabha written reply, 7 Aug 2023. PIB
- ICAR, "Farmers' participatory sodic soil reclamation…" (source: ICAR-CSSRI, Karnal), accessed 1 Oct 2026. ICAR
- PIB (MoA&FW), "Celebrating a Decade of Soil Health Cards", 19 Feb 2025. PIB backgrounder PDF
BharatNotes