UNIT 21. Environmental Geography and Sustainable Development in India

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UNIT 24. Regional Geography of Northern, Western and Central India

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UNIT 25. Regional Geography of Southern, Eastern and North-Eastern India

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Land Reclamation

Land reclamation is the scientific process of restoring degraded, physically restricted, or ecologically compromised lands into productive, economically viable states suitable for agriculture, forestry, or urban infrastructure. Under the Soils and Land Resources unit of Indian Geography, land reclamation acts as a vital structural mechanism to expand India’s effective land resource base against intensifying demographic pressures and shrinking per capita land availability.

Distinction Between Land Reclamation and Land Restoration
  • Land Reclamation: Involves intensive physical, chemical, or engineering interventions to fundamentally alter a severely degraded or unusable landscape into an entirely new productive use (e.g., converting deep ravines into arable fields or hyper-saline basins into crop tracts).
  • Land Restoration: Focuses on returning an ecosystem to its original or natural historic condition, prioritizing ecological functions and biodiversity over pure economic or agricultural yield.
Mechanical, Chemical, and Biological Interventions

The choice of reclamation strategy depends strictly on the physical and chemical state of the degraded terrain:

  • Mechanical Measures: Utilizing heavy earthmovers for terrain leveling, constructing concrete or masonry chute spillways, and engineering peripheral drainage networks to divert destructive surface runoff.
  • Chemical Remediation: Applying targeted chemical amendments to modify soil chemical structures, replace toxic ions, and correct extreme pH imbalances.
  • Biological Engineering: Planting hyper-accumulators, salt-tolerant halophytes, and deep-rooted pioneer plant species to stabilize mechanical structures and build soil organic matter.

Technical Protocols for Specific Degradation Types

Saline and Alkaline Soils (Usar, Reh, Kallar Lands)

Saline and alkaline soils suffer from high concentrations of soluble salts and exchangeable sodium, which destroy soil structure and induce high osmotic pressure, preventing root water absorption.

  • Leaching and Drainage: Flooding fields with high-quality freshwater to dissolve soluble salts and wash them deep into subsoil layers through specialized subsurface drainage tile systems.
  • Chemical Amendments: Applying Gypsum (CaSO4 · 2H2O) or Agricultural Pyrites (FeS2). The calcium ions displace toxic exchangeable sodium ions from the soil clay complex, converting them into highly soluble sodium sulfate, which is subsequently leached out.
  • Green Manuring: Cultivating and plowing in acidifying green manure crops like Dhaincha (Sesbania aculeata) or Sunnhemp to release organic acids that naturally lower high alkaline pH levels.
Ravines and Gullied Lands (Behads)

Ravines expand through rapid headward fluvial erosion, destroying flat tablelands and expanding uncultivable badlands.

  • Peripheral Runoff Control: Constructing continuous earthen bunds along the ravine perimeter to stop surface runoff from cascading over vertical head-cuts.
  • Gully Plugging: Building a series of mechanical check dams using loose boulders, sandbags, or wire-mesh gabions across the gully bed to trap sediment, reduce water velocity, and flatten the channel gradient.
  • Chute Spillways: Installing paved stone or concrete flumes to guide water safely down from tablelands to the ravine floor without undercutting the vertical walls.
Waterlogged and Marshy Tracts

Waterlogging seals soil pores, cutting off the oxygen supply and creating highly toxic, anaerobic conditions that halt standard crop development.

  • Surface and Subsurface Drainage: Constructing parallel open ditches or installing perforated underground PVC pipes to continuously draw out excess gravitational water and lower the local water table.
  • Bio-Drainage: Planting dense rows of deep-rooted, high-transpiration trees like Eucalyptus tereticornis along waterlogged perimeters to act as natural biological pumps that evaporate subsoil water into the atmosphere.
Acid Soils

Acid soils develop in high-rainfall regions where soluble bases like calcium and magnesium are leached out, causing toxic accumulations of iron, aluminum, and manganese.

  • Liming: Applying heavy quantities of agricultural limestone (Calcium Carbonate, CaCO3) or Dolomite (CaMg(CO3)2) to neutralize humic and mineral acids, raise soil pH to optimal zones, and precipitate toxic aluminum out of solution.

Geographical Matrix of Land Reclamation Hotspots in India

The structural variations in climate, topography, and agricultural practices determine the dominant land reclamation techniques deployed across India’s distinct physiographic zones.

Region / ZonePrimary Degradation TypeTarget Districts / HotspotsDominant Reclamation Protocol Deployed
Indo-Gangetic PlainsAlkaline/Saline Usar LandsSangrur (Punjab), Karnal (Haryana), Mainpuri, Etah (Uttar Pradesh)Subsurface drainage systems, mass gypsum distribution, and cultivation of salt-tolerant paddy varieties.
Chambal-Yamuna BasinsDeep Ravine BehadsBhind, Morena (Madhya Pradesh), Dholpur (Rajasthan), Etawah (Uttar Pradesh)Structural land-leveling with heavy earthmovers, peripheral contour bunding, and Acacia afforestation.
Central Gujarat PlainsCoastal & Inland SalinityAnand, Kheda, Bharuch (Gujarat)Construction of coastal tidal embankments (bandharas), flushing with canal waters, and brackish-water aquaculture.
Southwestern CoastHighly Acidic, Waterlogged Kari SoilsKuttanad region (Alappuzha, Kottayam districts of Kerala)Structured polder construction, seasonal liming, and below-sea-level paddy water-gate management.
Chota Nagpur PlateauOpen-cast Mining WastelandsDhanbad, Jharia (Jharkhand), Korba (Chhattisgarh), Angul (Odisha)Structural backfilling of quarries, topsoil stockpiling and re-spreading, and pioneer legume forestry.
Western Arid FrontierMobile Eolian SandsJaisalmer, Barmer, Bikaner (Rajasthan)Checkerboard mechanical brushwood mulching followed by Lasiurus scindicus grass seeding.

Priority Flora for Biological Land Reclamation

Biological reclamation relies on specialized plants capable of thriving in highly toxic, nutrient-deficient environments while mechanically binding the soil matrix.

Vetiver Grass (Chrysopogon zizanioides)
  • Utility: Possesses an exceptionally deep, massive, and fibrous root system that grows vertically down up to 3–4 meters. It creates a living underground root curtain that anchors unstable slopes, controls water erosion, and thrives across a wide pH range (4.5 to 10.5).
Dhaincha (Sesbania aculeata)
  • Utility: A rapid-growing, nitrogen-fixing leguminous crop with high tolerance to waterlogging and salinity. It accumulates massive green biomass that, when plowed back into alkaline soil, produces organic acids that neutralize excess sodium carbonate.
Israeli Babool (Acacia tortilis)
  • Utility: An extremely drought-resistant, deep-rooted pioneer tree used extensively for hyper-arid sand dune stabilization and dry ravine reclamation. Its canopy buffers wind shear while its roots bind loose sand.
Whistling Pine (Casuarina equisetifolia)
  • Utility: A actinorhizal, salt-tolerant tree capable of fixing atmospheric nitrogen in nutrient-poor sand. It is heavily utilized along the coastal plains of Odisha and Andhra Pradesh to reclaim sandy wastes and act as a coastal bio-shield against storm surges.
Kankar/Malabar Neem (Melia dubia)
  • Utility: A fast-growing industrial agroforestry tree species utilized for the rapid biological rehabilitation of degraded mining overburden dumps due to its low nutrient requirements and high biomass production.

Institutional Frameworks and National Reclamation Policies

Integrated Watershed Management Programme (IWMP)

Administered under the Pradhan Mantri Krishi Sinchayee Yojana (PMKSY-WDC Component), the programme uses satellite remote sensing data and ridge-to-valley treatment planning to systematically reclaim degraded sub-catchments through check dams, farm ponds, and community-led afforestation.

Central Soil Salinity Research Institute (CSSRI) Interventions

The CSSRI has pioneered the technological template for reclaiming alkali soils in India. Its multi-tier model—comprising land leveling, bunding, precise gypsum application based on soil testing, leaching, and the sequential cultivation of salt-tolerant rice (e.g., CSR-10, CSR-30) and wheat (e.g., KRL-210)—has successfully brought millions of hectares back under active crop production.

National Afforestation Programme (NAP)

Focuses specifically on the eco-reclamation of degraded, notified forest lands and adjoining village commons through a decentralized structure involving Joint Forest Management Committees (JFMCs) at the grassroots level.

UNCCD Land Degradation Neutrality (LDN) Targets

As part of its international commitments under the United Nations Convention to Combat Desertification, India has raised its target to reclaim 26 million hectares of degraded and wasteland tracts by 2030, leveraging multiple converging central schemes.

UPSC Prelims Facts and Trivia

Gypsum Requirement (GR) Value

The Gypsum Requirement value is a laboratory diagnostic metric indicating the exact amount of pure gypsum (CaSO4 · 2H2O) required per hectare to replace toxic exchangeable sodium ions from the top 15 cm of an alkali soil profile down to a safe threshold level.

Acid Sulfate Soils and Cat Clays

When coastal marshy soils containing high concentrations of iron sulfides are drained for agriculture, the sulfide minerals oxidize to produce sulfuric acid. This drops the soil pH below 3.5, forming highly toxic “acid sulfate soils” (locally called Kari in Kerala). Geographers historically termed these highly uncultivable clays “cat clays.”

Polder Farming System of Kuttanad

Kuttanad is one of the rare places globally where farming is practiced successfully 1 to 2.5 meters below sea level. This land reclamation system utilizes massive earthen embankments (polders) to isolate backwater tracts, which are then de-watered using seasonal pumping systems to allow paddy cultivation.

Subsurface Drainage (SSD) Technology

Unlike surface ditches that remove standing water, SSD uses a network of perforated corrugated PVC pipes wrapped in geotextile filters, buried horizontally at a depth of 1 to 2 meters. This layout leverages gravity to lower high saline groundwater tables below the crop root zone, safely collecting and flushing brackish waters away from the farm terrain.

Last Modified: June 5, 2026

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