06 · GS-III: Environment, Himalayan Cryosphere & Biodiversity
Ecological Fragility of Himalayan Spring-Sheds: Groundwater Depletion, Land-Use Change and National Spring Mission
NEWS PEG
- Hydrogeological surveys in the Central and Eastern Himalayas revealed that over 50% of perennial mountain springs (Dharas) have dried up or become seasonal, impacting drinking water security for over 5 crore mountain inhabitants.
- Researchers identified road widening, hill cutting without muck disposal safeguards, and deforestation in upper recharge zones as critical factors fracturing subterranean aquifers.
- NITI Aayog called for nationwide implementation of the 8-step hydrogeological spring-shed revival framework under the National Spring Mission, integrating isotope hydrology and community groundwater management.
STATIC FOUNDATION
- Spring-Shed Concept: Hydrogeological unit that feeds a mountain spring; distinct from a surface watershed as spring recharge areas can span across topographic ridgelines depending on underlying rock fractures.
- Isotope Hydrology: Technique using stable environmental isotopes (Oxygen-18, Deuterium) to accurately map the elevation and extent of subterranean aquifer recharge zones.
- NITI Aayog Report on Inventory and Revival of Springs in the Indian Himalayan Region: Highlighted that springs provide 90% of drinking water in mountain villages.
PRELIMS TRAP & PYQ BRIDGE
MAINS ENHANCEMENT
- Scientific Hydrogeology: Mapping Subsurface Recharge Zones — Using isotope techniques to delineate and protect spring recharge catchments before construction.
- Participatory Groundwater Governance: Para-Hydrogeologists & Village Water Committees — Training local mountain youth to monitor spring discharge and rainfall telemetry.
- Nature-Based Infrastructure: Contour Trenches & Broadleaf Afforestation — Enhancing infiltration capacity in upper slopes to sustain lean-season perennial base flows.