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. Soils come up in Prelims as soil-to-region and soil-to-crop matching, and in Mains through resources, land degradation and conservation.

Contemporary hook: The Soil Health Card Scheme completed ten years on 19 February 2025. By then 24.74 crore cards had been generated (PIB, 4 Feb 2025), and the count reached 26.09 crore by July 2026 (Lok Sabha answer, 21 Jul 2026). 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.

Three ideas carry the chapter: soil forms from parent rock under climate and time, so each soil group belongs to a region; fertility is partly natural and partly made by people; and the same irrigation that raised yields can ruin the soil.


PART 1 — Quick Reference

Table 1: Factors of soil formation (NCERT)

FactorWhat it controlsExample from the chapter
ReliefDrainage, depth, and how fast soil is removedGully erosion is common on steep slopes
Parent materialMineral make-up and textureRed soil develops on crystalline igneous rocks
ClimateWeathering, leaching and evaporationLaterite forms under high temperature and heavy rain
Vegetation and other life-formsHumus and binding of soil by rootsPeaty soils form where dense vegetation leaves much dead organic matter
TimeHow mature the soil isKhadar is new alluvium and bhangar is older alluvium
Human activity (NCERT: "also influence it to a large extent")Erosion, salinity and loss of fertilityOver-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)

HorizonPositionContents
Horizon ATopmostOrganic matter mixed with mineral matter, nutrients and water. This is the zone plants use.
Horizon BTransition zoneMaterial from above and below, some organic matter, and noticeably weathered minerals
Horizon CLowest soil layerLoose parent material, the first stage of soil formation
BedrockBelow the three horizonsUnweathered 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.

The soil profile: horizons A, B and C above the bedrockA schematic vertical column of the soil profile, drawn top to bottom in four layers. Horizon A is the topmost layer: organic matter mixed with mineral matter, nutrients and water; this is the zone plants use. Horizon B is the transition zone: material from above and below, some organic matter, and noticeably weathered minerals. Horizon C is the lowest soil layer: loose parent material, the first stage of soil formation. Below the three horizons is the bedrock: unweathered parent rock. A note says NCERT describes three horizons above the bedrock and that the O (litter) and R (bedrock) labels of soil-science textbooks are not part of the NCERT scheme.TopHorizon ATopmostOrganic matter mixed with mineral matter, nutrients and water. This is thezone plants use.Horizon BTransition zoneMaterial from above and below, some organic matter, and noticeably weatheredminerals.Horizon CLowest soil layerLoose parent material, the first stage of soil formation.BedrockBelow the three horizonsUnweathered parent rock.BottomNCERT describes three horizons abovethe bedrock. O (litter) and R (bedrock)labels are not part of its scheme.
Schematic, not to scale; layer thicknesses are not NCERT's. Source: NCERT Class XI, India: Physical Environment, old ch. 6 (2021-22 edition; dropped in the rationalised edition), Table 2 of this page. The O and R labels are not part of NCERT's scheme.

Table 3: ICAR classification of Indian soils by USDA Soil Taxonomy order

OrderArea (thousand ha)Share of total (%)
Inceptisols1,30,372.9039.74
Entisols92,131.7128.08
Alfisols44,448.6813.55
Vertisols27,960.008.52
Aridisols14,069.004.28
Ultisols8,250.002.51
Mollisols1,320.000.40
Others9,503.102.92

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")

SoilWhere (NCERT)Character (NCERT)Crops named in NCERT
AlluvialNorthern plains and river valleys; through a narrow corridor in Rajasthan into the Gujarat plains; east-coast deltasCovers "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 yellowEastern and southern Deccan on crystalline igneous rocks in low-rainfall areas; piedmont of the Western Ghats (red loamy); Odisha, Chhattisgarh, southern middle Ganga plainRed 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
LateriteHigher areas of the Peninsular plateau: Karnataka, Kerala, Tamil Nadu, MP, hilly Odisha and AssamFormed 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)
AridWestern RajasthanRed 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 HaryanaExcess sodium, potassium and magnesium, so infertile. Lacks nitrogen and calcium. Sandy to loamy.Remedy: add gypsum (NCERT advice for Punjab and Haryana)
PeatyNorth Bihar, southern Uttarakhand, coastal West Bengal, Odisha and Tamil NaduHeavy rainfall and humidity, dense vegetation. Organic matter up to 40-50%. Heavy and black, "at many places" alkaline.Not specified
ForestForest areas with enough rainfall; mountain slopesLoamy 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.

NCERT's eight soil groups: where each is found and its characterA grid of eight cards, two columns by four rows, one for each soil group NCERT classifies on the basis of genesis, colour, composition and location. Each card is numbered and gives the soil's name, where it is found and its character as NCERT prints them. 1 Alluvial: northern plains and river valleys, about 40 per cent of the country's area, depositional, light grey to ash grey. 2 Black (regur, black cotton): most of the Deccan Plateau, clayey and deep, swells when wet and cracks when dry. 3 Red and yellow: eastern and southern Deccan, red from iron diffused through crystalline and metamorphic rocks, yellow when hydrated. 4 Laterite: higher areas of the Peninsular plateau, formed by intense leaching, acidic. 5 Arid: western Rajasthan, red to brown, sandy, saline. 6 Saline (usara): western Gujarat, east-coast deltas, Sundarbans, Rann of Kachchh, irrigated Green Revolution areas such as Punjab and Haryana. 7 Peaty: north Bihar, southern Uttarakhand, coastal West Bengal, Odisha and Tamil Nadu, organic matter up to 40 to 50 per cent. 8 Forest: forest areas with enough rainfall and mountain slopes. The ICAR and USDA soil orders of Table 3 are not mixed in.1 AlluvialWhereNorthern plains and river valleys; through a narrowcorridor in Rajasthan into the Gujarat plains; east-coastdeltas.Character•Covers "about 40 per cent of the total area of thecountry".•Depositional (transported by rivers).•Sandy loam to clay.•Generally rich in potash, poor in phosphorus.•Light grey to ash grey.2 Black (regur, black cotton)WhereMost of the Deccan Plateau: Maharashtra, MP, Gujarat,Andhra Pradesh, parts of Tamil Nadu.Character•Clayey, deep, impermeable.•Swells when wet and cracks when dry ("self-ploughing").•Holds moisture for long.•Rich in lime, iron, magnesia and alumina, and containspotash.•Lacks phosphorus, nitrogen and organic matter.3 Red and yellowWhereEastern and southern Deccan on crystalline igneous rocksin low-rainfall areas; piedmont of the Western Ghats;Odisha, Chhattisgarh, southern middle Ganga plain.Character•Red from iron diffused through crystalline andmetamorphic rocks, yellow when hydrated.•Generally poor in nitrogen, phosphorus and humus.4 LateriteWhereHigher areas of the Peninsular plateau: Karnataka,Kerala, Tamil Nadu, MP, hilly Odisha and Assam.Character•Formed by intense leaching: lime and silica removed,iron oxide and aluminium left.•Poor in organic matter, N, P and Ca; iron oxide andpotash in excess.•Acidic (pH < 6.0, Class 10).5 AridWhereWestern Rajasthan.Character•Red to brown, sandy, saline.•Lacks moisture and humus.•Nitrogen insufficient, phosphate normal.•Kankar layers in lower horizons.6 Saline (usara)WhereWestern Gujarat, east-coast deltas, Sundarbans; Rann ofKachchh (salt crust); irrigated Green Revolution areassuch as Punjab and Haryana.Character•Excess sodium, potassium and magnesium, so infertile.•Lacks nitrogen and calcium.•Sandy to loamy.7 PeatyWhereNorth Bihar, southern Uttarakhand, coastal West Bengal,Odisha and Tamil Nadu.Character•Heavy rainfall and humidity, dense vegetation.•Organic matter up to 40-50%. Heavy and black, "at manyplaces" alkaline.8 ForestWhereForest areas with enough rainfall; mountain slopes.Character•Loamy and silty on valley sides, coarse on upperslopes.•Acidic with low humus in snow-bound Himalaya.•Fertile in lower valleys.
Not a map and not to scale. Sources: NCERT Class XI, India: Physical Environment, old ch. 6 (2021-22 edition; dropped in the rationalised edition), Table 4 of this page; NCERT Class 10 Contemporary India II, ch. 1 (Reprint 2026-27) for the pH and Class 10 remarks. The ICAR/USDA orders of Table 3 are a different classification and are not drawn.

Table 5: How much of India's land is degraded? Two official figures

EstimateAreaBasisSource
NBSS&LUP (2004, revised)146.82 Mha (~147 Mha)Soil-degradation mapping by type: water erosion 94, acidification 16, flooding 14, wind erosion 9, salinity 6, combination 7 MhaBhattacharyya et al., "Soil Degradation in India: Challenges and Potential Solutions", Sustainability 7(4):3528-3570, 2015, citing NBSS&LUP (2004); figure also in ICAR-NAAS (2010), Table 1, whose own total is 120.72 Mha
ISRO-SAC Desertification and Land Degradation Atlas (released 17 Jun 2021)97.84 Mha in 2018-19Satellite mapping of land degradation and desertification processesPIB, 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 givenNCERT 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.

Key Term

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.

Explainer

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.
Explainer

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 (Dhruva Narayana and Ram Babu, "Estimation of Soil Erosion in India", Journal of Irrigation and Drainage Engineering 109(4): 419-434), as 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.

How much land is degraded: official estimates, then causes and conservationTop: a horizontal bar chart of three official estimates of degraded land in million hectares, drawn to scale on one axis from 0 to 160. NBSS&LUP, 2004 revised: 146.82 million hectares, from soil-degradation mapping by type (water erosion 94, acidification 16, flooding 14, wind erosion 9, salinity 6, combination 7). ICAR-NAAS, 2010: 120.72 million hectares, the grand total of its Table 1, which also prints the NBSS&LUP figure. ISRO-SAC Desertification and Land Degradation Atlas: 97.84 million hectares in 2018-19, from satellite mapping. The bars measure different things and are not a trend. NCERT itself says only about half of the total land of India, with no source. Bottom: a left-to-right flow. Causes NCERT names: erosion; over-irrigation, which brings salt up from lower layers; chemical fertilisers without organic manure, which harden the soil; over-grazing and shifting cultivation, which remove the natural vegetation cover. These lead to soil degradation, the decline in soil fertility. Conservation measures: land with a slope gradient of 15 to 25 per cent should not be cultivated and, if farmed, terraced; contour bunding, terracing and ploughing; check dams and gully plugging; strip cropping, shelter belts and agro-forestry; and integrated land-use planning.Degraded land, million hectares (Mha): official estimates by different methodsNBSS&LUP (2004, revised)Soil-degradation mapping by type146.82ICAR-NAAS (2010)Grand total of its Table 1120.72ISRO-SAC Atlas, 2018-19Satellite mapping of degradation anddesertification97.84NBSS&LUP by type: water erosion 94, acidification 16, flooding 14, wind erosion 9, salinity 6, combination 7 Mha.NCERT's own text: "about half of the total land of India", no source given.CAUSES (NCERT)CONSERVATION MEASURES (NCERT)ErosionOver-irrigationBrings salt up from lower layers to thesurface.Chemical fertilisers withoutorganic manureHarden the soil and lower its fertilityin the long run.Over-grazing and shiftingcultivationRemove the natural vegetation cover.Slope gradient of 15-25%Not to be cultivated; if farmed,terraced.Contour bunding, terracing,ploughingSlow the run-off down slopes.Check dams, gully pluggingReduce water speed; stop gulliesextending headward.Strip cropping, shelter belts,agro-forestryBreak the force of wind; protect landfrom encroaching sand dunes.Integrated land-use planningNCERT's recommendation: classify land bycapability, map it, use it rightly.Soil degradationThe decline in soilfertility: nutritionalstatus and depth ofsoil go down due toerosion and misuse.
Bars drawn to scale. Sources: NBSS&LUP (2004, revised), 146.82 Mha, and ICAR-NAAS (2010), grand total 120.72 Mha, both from ICAR and NAAS, Degraded and Wastelands of India (June 2010), Table 1; the NBSS&LUP breakdown from Bhattacharyya et al., Sustainability 7(4), 2015; ISRO-SAC Atlas, 97.84 Mha in 2018-19 (PIB, 17 Jun 2021 and 7 Aug 2023). Causes and measures: NCERT Class XI, India: Physical Environment, old ch. 6 (2021-22 edition; dropped in the rationalised edition), and NCERT Class 10 ch. 1. The methods differ, so the bars are not a trend.

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:

MeasurePurpose (NCERT)
Contour bunding, contour terracing, contour ploughingSlow the run-off down slopes
TerracingRemoves finger gullies and restricts erosion on slopes. Well developed in the western and central Himalaya (Class 10).
Check damsReduce the erosive speed of water in larger gullies
Gully plugging, terracing, cover vegetationStop gullies from extending headward
Regulated forestry, controlled grazing, cover cropping, mixed farming, crop rotationGeneral remedies
Strip cropping (strips of grass between crops)Break the force of the wind (Class 10)
Shelter belts and agro-forestryProtect cultivable land from encroaching sand dunes
Converting land unfit for cropping into pastureKeeps it under cover
Sand-dune stabilisationTrials 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.

Beyond the Book

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 set up in 17 states (PIB, 4 Feb 2025). By 21 July 2026 the count was 26.09 crore cards, with 8,313 soil testing labs of all kinds (Lok Sabha Unstarred Q. 360). Since 2022-23 the scheme has been the "Soil Health & Fertility" component of RKVY (PIB backgrounder, 19 Feb 2025).


PART 3 — UPSC Integration

UPSC Connect

Cross-paper relevance

  • GS1 (geography): distribution of soils as a natural resource; the resource potential of a region such as the Deccan Trap; desertification; regional disparity in agriculture.
  • GS3 (agriculture, environment): land degradation, salinity from irrigation, watershed management and soil-health policy.

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. The 40% is for the alluvial group; the 39.74% for Inceptisols is a USDA order, a different scheme, so do not equate them.
  • 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 usually come through other themes: the resources of a region (the 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

Practice (UPSC-pattern, not past papers). Questions 1 to 4 are NCERT's own exercise MCQs.

Prelims:

  1. Which one of the following is the most widespread and most productive category of soil?
    (a) Alluvial soil
    (b) Laterite soil
    (c) Black soil
    (d) Forest soil

  2. "Regur soil" is another name for the:
    (a) Saline soil
    (b) Arid soil
    (c) Black soil
    (d) Laterite soil

  3. Which one of the following is the main reason for the loss of the top soil in India?
    (a) Wind erosion
    (b) Water erosion
    (c) Excessive leaching
    (d) None of these

  4. Arable land in the irrigated zones of India is turning saline due to which of the following reasons?
    (a) Addition of gypsum
    (b) Over grazing
    (c) Over irrigation
    (d) Use of fertilisers

  5. With reference to Indian soils, consider the following statements: 1. Both khadar and bhangar contain calcareous concretions (kankar). 2. Inceptisols occupy the largest area among the 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?
    (a) 1 and 2 only
    (b) 2 and 3 only
    (c) 1 and 3 only
    (d) 1, 2 and 3

Mains (practice):

  1. What are black soils? Describe their formation and characteristics. (NCERT Ex. 3(i), 125 words)
  2. What is soil conservation? Suggest some measures to conserve soil. (NCERT Ex. 3(ii), 125 words)
  3. How do you know that a particular type of soil is fertile or not? Differentiate between naturally determined fertility and culturally induced fertility. (NCERT Ex. 3(iii), 125 words)
  4. India's official land-degradation estimates range from about 98 to about 147 million hectares. Explain why they differ, and suggest how soil conservation should be targeted. (practice, 15 marks)

Short answers (NCERT Ex. 2, about 30 words): soil is the mixture of rock debris and organic material that develops on the earth's surface. Its formation depends on relief, parent material, climate, vegetation and other life forms, and time, and human activities also influence it to a large extent. A soil profile has three horizons: A, the topmost, where organic matter mixes with minerals, nutrients and water; B, a transition zone with matter from above and below; and C, loose parent material. Soil degradation is the decline in soil fertility, when the nutritional status declines and the depth of the soil goes down due to erosion and misuse. Khadar is new alluvium deposited by floods every year; bhangar is older alluvium away from the floodplain.

Worked answer, NCERT Ex. 3(iii) (built from the chapter's own text): whether a soil is fertile depends on its components (mineral particles, humus, water and air) and on its nutrients. A soil short of humus, nitrogen or phosphorus, a salt crust on the surface, or soil that has thinned through erosion are signs of low fertility; NCERT defines degradation as the decline in fertility when "the nutritional status declines and depth of the soil goes down". Naturally determined fertility is what the soil inherits from parent rock, climate and vegetation: alluvial soils are rich in potash, fine-grained red and yellow soils are normally fertile, while laterites lose lime, silica and humus to leaching and are poor in nitrogen, phosphate and calcium. Culturally induced fertility is what human use adds or takes away: manures and fertilisers make laterites fit for cultivation, and gypsum treats salinity in Punjab and Haryana; but over-irrigation raises salt to the surface, and chemical fertilisers without organic manure harden the soil and reduce its fertility in the long run.


📦 Revision Capsule

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 by Feb 2025 (PIB), 26.09 crore by Jul 2026 (Lok Sabha)

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, revised) vs 97.84 Mha (ISRO-SAC, 2018-19). The two use different methods.
  • Soil loss ~5.3 billion t/yr is a 1983 estimate, not a current measurement

PYQ Pattern

  • Mains GS1 brings soils in through regional resources (the Deccan Trap), desertification, regional disparity in agriculture and watershed management.

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
  • ICAR and NAAS, Degraded and Wastelands of India: Status and Spatial Distribution, June 2010 (Table 1: NBSS&LUP 2004 revised, 146.82 Mha; grand total 120.72 Mha). ICAR PDF
  • Dhruva Narayana, V. V. and Ram Babu, "Estimation of Soil Erosion in India", Journal of Irrigation and Drainage Engineering (ASCE) 109(4): 419-434, December 1983. DOI
  • PIB (MoA&FW), "Implementation of the New Soil Health Card Scheme", Lok Sabha written reply, 4 Feb 2025. PIB
  • Lok Sabha Unstarred Question No. 360, "Soil Health Card Scheme", answered 21 Jul 2026. Lok Sabha PDF
  • PIB (MoA&FW), "Celebrating a Decade of Soil Health Cards", 19 Feb 2025. PIB backgrounder PDF