Soil Profile Of Uttar PradeshSoil Profile Of Uttar Pradesh

The soil profile of Uttar Pradesh is primarily shaped by the Indo-Gangetic river system, varying from alluvial soils in the plains to red and mixed soils in the southern plateau. Understanding these agro-climatic zones, soil composition, and regional distribution is essential ...The soil profile of Uttar Pradesh is primarily shaped by the Indo-Gangetic river system, varying from alluvial soils in the plains to red and mixed soils in the southern plateau. Understanding these agro-climatic zones, soil composition, and regional distribution is essential ...

Mediumमध्यम 60 min totalकुल 60 मिनट

Chronological Evolution of Soil Profile Of Up

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Soil Profile Of Uttar Pradesh Core Study Notes

The soil profile of Uttar Pradesh is primarily shaped by the Indo-Gangetic river system, varying from alluvial soils in the plains to red and mixed soils in the southern plateau. Understanding these agro-climatic zones, soil composition, and regional distribution is essential for clearing the Allahabad High Court RO/ARO and UPPSC examinations.

Major Soil Types and Classification in UP

Uttar Pradesh can be broadly divided into three major soil zones: Alluvial soils of the Gangetic plain, Southern Red and Mixed soils, and Vindhyan/Bundelkhand tract soils.

  • Alluvial Soil (Jallodh Mitti): Covers about 80% of UP's total land area, brought down by Himalayan rivers. Highly fertile, rich in potash and lime, but deficient in nitrogen and organic matter. Subdivided into Khadar (new alluvium) and Bhangar (old alluvium).
  • Khadar (New Alluvium): Found in floodplains of rivers like Ganga and Yamuna. It is sandy-clayey to loam in texture, replenished annually by floods, highly suitable for paddy, wheat, and sugarcane cultivation.
  • Bhangar (Old Alluvium): Found away from river floodplains at higher elevations. Contains kankar (calcareous nodules), less fertile than Khadar, requires intensive irrigation and fertilization.
  • Red and Mixed Soils (Lal Evam Mishra Mitti): Found in southern districts bordering Madhya Pradesh (Jhansi, Mirzapur, Sonbhadra, Banda, Chandauli). Formed due to weathering of ancient crystalline rocks. Rich in iron oxide (giving red color), poor in nitrogen, phosphorus, and humus.
  • Bundelkhand Tract Soils (Parwa, Mar, Kabar, Rakar): Specialized local soil classifications in the Bundelkhand region: 'Mar' is black cotton soil (clayey, sticky), 'Kabar' is heavy clay soil, 'Parwa' is sandy-loam (light soil), and 'Rakar' is sloping, eroded red soil found near hills.
Soil Type Key Districts / Region Nutrient Status Major Crops Grown
Khadar (New Alluvial) River basins across Western & Central UP Rich in Potash/Lime; Deficient in Nitrogen Sugarcane, Paddy, Wheat, Vegetables
Bhangar (Old Alluvial) Doab regions, Eastern UP uplands Moderate fertility, needs nitrogen/phosphorus Wheat, Maize, Bajra, Pulses
Mar & Kabar (Black Soils) Mahoba, Hamirpur, Jhansi, Banda High moisture retention, rich in iron/lime Wheat, Gram, Jowar, Oilseeds
Parwa & Rakar (Red/Mixed) Bundelkhand & Vindhyan tract Low organic matter, acidic to neutral Millets, Pulses, Sesame, Mustard

Soil Degradation, Salinity, and Reclamation in UP

Intensive farming, canal irrigation, and deforestation have led to severe issues like Usar (saline-alkaline) soils, ravine formation along Chambal, and soil erosion in the sub-Himalayan tract.

  • Usar / Alkaline Soils (Reh / Kallar): Extensively found in Aligarh, Mainpuri, Etawah, Unnao, Rae Bareli, and Kanpur districts. Characterized by high sodium carbonate/bicarbonate accumulation making soils impermeable and infertile.
  • Reclamation of Usar Soils: Gypsum (Calcium Sulfate) application is the primary chemical method used to replace sodium ions with calcium ions, followed by leaching and cultivation of salt-tolerant paddy varieties.
  • Ravine (Bihad) Formation: Caused by severe gully erosion by Yamuna and Chambal rivers in districts like Etawah, Jalaun, and Agra, turning fertile lands into rugged, undulating ravines.
  • Bhabhar and Terai Soil Erosion: Northern strip along the Nepal border faces heavy rainfall and rapid water runoff, causing sheet and rill erosion along with waterlogging in low-lying Terai pockets.
Problem Type Affected Districts Root Cause Remedial / Reclamation Method
Salinity & Alkalinity (Usar) Mainpuri, Aligarh, Etah, Kanpur Over-irrigation, poor drainage, high evaporation Gypsum application & tolerant paddy crops
Ravine Erosion (Bihad) Etawah, Agra, Jalaun, Auraiya Running water action of Yamuna/Chambal, deforestation Afforestation, check dams, contour bunding
Waterlogging (Jal-Magnata) Terai belt (Pilibhit, Lakhimpur, Gorakhpur) Heavy monsoon rainfall, flat topography Drainage channels, raised bed planting

Practice Zone: 50 Questions

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