Soil Resources of the Indian Subcontinent

“Soils in the Indian Subcontinent are diverse, reflecting the varied climate, relief, and vegetation.”

Factors Influencing Soil Formation

  • Parent Rock Material: Determines the mineral composition of soil.
  • Climate: Temperature and rainfall affect soil weathering and organic matter.
  • Relief: Slope and altitude influence soil drainage and erosion.
  • Vegetation: Provides organic matter and affects soil acidity/alkalinity.
  • Time: Older soils are usually more developed and leached.
  • Human Activities: Agriculture, deforestation, and irrigation modify soil characteristics.

Major Soil Types in the Indian Subcontinent

  • Alluvial Soil: Found in northern plains and river valleys, highly fertile and suitable for agriculture.
  • Black Soil (Regur): Predominantly in Deccan Plateau; retains moisture, ideal for cotton cultivation.
  • Red Soil: Found in southern and eastern India, rich in iron, low in nitrogen and organic matter.
  • Laterite Soil: Occurs in high rainfall areas like Western Ghats and northeastern states; poor fertility.
  • Desert Soil: Present in Rajasthan and arid regions; sandy and saline with low organic content.
  • Mountain Soil: Found in Himalayan region, thin, acidic, and rich in humus.
  • Saline and Alkaline Soils: Found in arid and semi-arid regions; adversely affect crop growth.

Characteristics and Uses

  • Alluvial Soil: Fertile, supports rice, wheat, sugarcane, and other crops.
  • Black Soil: Moisture-retentive, good for cotton, cereals, and pulses.
  • Red Soil: Suitable for groundnut, millet, and pulses but requires fertilizers.
  • Laterite Soil: Used for plantation crops like tea, coffee, and cashew.
  • Desert Soil: Supports drought-resistant plants and limited agriculture.
  • Mountain Soil: Supports horticulture and forestry.
  • Saline & Alkaline Soil: Requires reclamation for agriculture.

Soil Erosion and Conservation

  • Causes of Soil Erosion: Deforestation, overgrazing, excessive plowing, and heavy rainfall.
  • Types of Erosion: Wind erosion (common in arid zones) and water erosion (common in hilly and plains areas).
  • Soil Conservation Methods: Afforestation, contour plowing, terrace farming, crop rotation, and use of windbreaks.

Previous Year Questions

  • SSC CGL 2018: Which soil type is known as black cotton soil and why?
  • Black soil retains moisture well and is suitable for cotton cultivation.
  • RRB JE 2017: What are the main characteristics of alluvial soil?
  • Highly fertile, rich in potash, lime, and phosphoric acid, found in northern plains.
  • HSSC CET 2019: How can soil erosion be controlled in hilly areas?
  • By terrace farming, afforestation, and contour plowing.
  • SSC MTS 2016: Name two regions where laterite soil is commonly found.
  • Western Ghats and northeastern states.
  • RRB Group D 2018: What is the impact of human activities on soil resources?
  • Deforestation and over-cultivation cause soil degradation and erosion.
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