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Soil Resources — Notes

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1. Alluvial soil

  • Formation: deposited by rivers (Indus, Ganga, Brahmaputra systems; east-coast deltas).
  • Distribution: largest soil group (roughly two-fifths of India) — Punjab, Haryana, Uttar Pradesh, Bihar, West Bengal, Assam valley; deltas of the Mahanadi, Godavari, Krishna, Kaveri; coastal plains.
  • Composition: sand, silt, clay; generally rich in potash and lime, poor in nitrogen and humus; coarse near the foothills, finer downstream.
  • Khadar: new alluvium on low floodplains, renewed by floods, light-coloured, very fertile.
  • Bhangar: old alluvium on higher terraces above flood level, more clayey, less fertile, contains kankar.
  • Crops: wheat, rice, sugarcane, jute (deltas), pulses, oilseeds.
Table comparing khadar and bhangar
HeadKhadarBhangar
AgeNewOld
PositionLow floodplainHigher terrace
FloodsRenewed oftenAbove flood level
FertilityHighLower
KankarAbsentPresent

Key terms

Khadar

New alluvium on the low floodplains of rivers, renewed by floods almost every year.

Bhangar

Old alluvium on higher river terraces, above normal flood level, often containing kankar.

Kankar

Nodules (lumps) of lime found in bhangar soil.

2. Black soil (regur)

  • Formation: weathering of basalt (Deccan trap lava).
  • Distribution: Maharashtra, Malwa plateau (Madhya Pradesh), Saurashtra (Gujarat), parts of Karnataka, Telangana, Andhra Pradesh.
  • Characteristics: fine, clayey; retains moisture; sticky when wet; deep cracks when dry (self-ploughing); rich in lime, iron, magnesia, potash; poor in nitrogen, phosphorus, humus.
  • Crops: cotton (black cotton soil), sugarcane, jowar, wheat, groundnut, tobacco.
Table of black-soil properties and their effects
PropertyEffect for the farmer
ClayeyHolds water; sticky when wet
Cracks when dryAeration, self-ploughing
Rich in lime and potashGood for cotton

Key terms

Regur

Another name for the black soil of the Deccan plateau.

Self-ploughing

The turning over of black soil as loose soil falls into the deep cracks that open in the dry season.

3. Red soil

  • Formation: weathering of old crystalline and metamorphic rocks (granite, gneiss) in low to moderate rainfall.
  • Colour: red from iron oxide spread through the soil; yellow where the oxide is hydrated.
  • Distribution: Tamil Nadu, Karnataka, Telangana, Andhra Pradesh, Odisha, Chhattisgarh, Chota Nagpur (Jharkhand).
  • Characteristics: sandy to loamy, porous, light; low water retention; poor in nitrogen, phosphorus, humus.
  • Crops (with fertilisers, irrigation): ragi, jowar, groundnut, pulses, tobacco; rice in lowlands.
Table summarising red soil
FeatureRed soil
Parent rockGranite, gneiss
TextureSandy to loamy
CropsMillets, groundnut

Key terms

Iron oxide

The compound that gives red soil its colour; it looks yellow when hydrated.

4. Laterite soil

  • Formation: high temperature and heavy rain with alternate wet and dry seasons; leaching removes lime and silica, leaving oxides of iron and aluminium. (Latin later = brick.)
  • Distribution: summits of the Western and Eastern Ghats, Kerala, Karnataka, Goa, Odisha hills, Meghalaya.
  • Characteristics: coarse, acidic, infertile; poor in nitrogen, lime, humus; hardens in air (used as building bricks).
  • Crops (with manure): cashew, tea, coffee, rubber, coconut.
HeadRedLaterite
RainfallLow to moderateHeavy
ProcessWeatheringLeaching
FertilityLowVery low, acidic
CropsMillets, groundnutCashew, tea, coffee
Table of the steps in laterite formation
StepWhat happens
Heavy rainWater percolates through soil
LeachingLime and silica removed
ResidueIron and aluminium oxides remain

Key terms

Leaching

The washing down of soluble minerals such as lime and silica by water percolating through soil.

5. Soil erosion

  • Soil erosion: removal of topsoil by natural agents faster than new soil forms.
  • Agents: running water, wind, waves, glaciers.
  • Sheet erosion: thin, even layer removed from a wide area by running water.
  • Gully erosion: deep channels cut by running water; badly gullied land becomes ravines (Chambal valley).
  • Wind erosion: dry, loose, bare soil blown away (western Rajasthan).
  • Human causes: deforestation, overgrazing, ploughing up and down slopes, shifting cultivation, mining and construction.
Table of types of erosion with agent and example area
TypeAgentExample area
SheetRunning waterGentle slopes
GullyRunning waterChambal valley
WindWindWestern Rajasthan

Key terms

Soil erosion

The removal of the top layer of soil by water, wind or other agents faster than it can form.

Ravines

Land cut up by deep, joined gullies, unfit for farming.

6. Soil conservation

  • Meaning: protecting soil from erosion and maintaining its fertility.
  • Importance: soil forms slowly; agriculture depends on it; eroded silt fills reservoirs and worsens floods; loss of land hurts livelihoods.
  • Terrace farming: flat steps on steep slopes (Himalayas, north-east).
  • Contour ploughing: furrows across the slope on gentle slopes.
  • Strip cropping: alternate strips of crops and grass.
  • Shelter belts: rows of trees across the wind in dry, windy plains (western Rajasthan).
  • Afforestation: trees on bare slopes and wasteland.
  • Plugging gullies: check dams and planting in gullied land (Chambal).
  • Controlled grazing: pasture rotation.
Table of conservation methods and the land they suit
MethodSuits
TerracesSteep slopes
Contour ploughingGentle slopes
Shelter beltsWindy dry plains
Check damsGullies

Key terms

Shelter belt

Rows of trees planted across the path of the wind to slow it and protect fields from wind erosion.

Contour ploughing

Ploughing across a slope along lines of equal height so that furrows hold back running water.

Exam tips

Common mistakes

  • Calling bhangar new alluvium, or saying khadar contains kankar.
  • Saying black soil forms from river silt (it forms from basalt lava).
  • Describing laterite as fertile.
  • Writing that contour ploughing runs up and down the slope.

How marks are usually awarded

  • Soil questions: formation, distribution, characteristics and crops (1 mark each point with a named area).
  • "Give a geographical reason": the property and how it causes the effect.
  • Conservation: method plus the type of land and a named region.