Switch thirsty crops, water by drip
Where most water goes to fields, moving from paddy and sugarcane to millets, pulses or maize, and from flood to drip or sprinkler irrigation, saves more than any recharge can add.
This area pumps out more water than rain puts back. That is the 2025 stage of groundwater extraction: water pumped out in a year as a share of what rain and other sources safely put back. Down 30 points since 2017.
Each point is one CGWB assessment. Over-exploited means more water leaves the ground than comes back, so the water table keeps falling. Hover over or tap a point to see why it moved.
| Year | Stage | Pumped out | Safe limit | Category | What changed |
|---|---|---|---|---|---|
| 2009 | 132.0% | 315 million m³ | 238 million m³ | Over-exploited | First assessment in this series. |
| 2013 | 148.0% | 359 million m³ | 242 million m³ | Over-exploited | Pumping up 14% (315 → 359 million m³). Safe limit up 2% (238 → 242 million m³). Main reason: more water was pumped out, mostly for irrigation (240 → 269 million m³). |
| 2017 | 170.3% | 410 million m³ | 241 million m³ | Over-exploited | Pumping up 14% (359 → 410 million m³). Safe limit down 0% (242 → 241 million m³). Main reason: more water was pumped out, mostly for irrigation (269 → 333 million m³). CGWB changed its method in 2017 (GEC-97 to GEC-2015), so part of this change comes from the new method. |
| 2020 | 141.1% | 486 million m³ | 345 million m³ | Over-exploited | Pumping up 19% (410 → 486 million m³). Safe limit up 43% (241 → 345 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. A swing this large usually comes partly from revised estimates (a new well count or changed district boundaries), not only from changes on the ground. |
| 2022 | 138.6% | 365 million m³ | 263 million m³ | Over-exploited | Pumping down 25% (486 → 365 million m³). Safe limit down 24% (345 → 263 million m³). |
| 2023 | 137.2% | 382 million m³ | 279 million m³ | Over-exploited | Pumping up 5% (365 → 382 million m³). Safe limit up 6% (263 → 279 million m³). |
| 2024 | 139.2% | 391 million m³ | 281 million m³ | Over-exploited | Pumping up 2% (382 → 391 million m³). Safe limit up 1% (279 → 281 million m³). |
| 2025 | 140.6% | 396 million m³ | 282 million m³ | Over-exploited | Pumping up 1% (391 → 396 million m³). Safe limit up 0% (281 → 282 million m³). |
Million m³: 1 million m³ = 100 crore litres. 2009 and 2013 used the older GEC-97 method.
Loading 20 years of rainfall…
Most of the water here goes to farming, so using less on fields matters as much as recharge.
Where most water goes to fields, moving from paddy and sugarcane to millets, pulses or maize, and from flood to drip or sprinkler irrigation, saves more than any recharge can add.
Parks, campuses, warehouse yards and road sides can take recharge shafts that reach past the clay layer, so runoff that floods streets goes down to the aquifer instead.
Desilting old ponds and opening their feeder channels restores natural recharge. A one-hectare pond that soaks in a metre of water over the monsoon puts back about a crore litres.
Pipe roof water through a silt trap and filter into a recharge pit or an old borewell. Every 100 m² of roof puts back tens of thousands of litres a year, right where the pumping happens.
On sloping or rocky land, small dams on seasonal streams and trenches along contours slow water down long enough for it to sink in.
Treated water from a sewage treatment plant can run flushing, gardens, cooling towers and construction, which today often draw on borewells.
In the 2025 Central Ground Water Board assessment, Bikaner (Rajasthan) pumped out 141% of the groundwater that can be safely taken out each year, which puts it in the "over-exploited" category. That is 30 points lower than in 2017.
Yes. Bikaner takes out more groundwater than rain and other sources put back, so the water table keeps falling.
Rooftop rainwater harvesting into recharge pits or old borewells, recharge shafts in open land, reviving ponds, check dams, treating and reusing wastewater, and moving farms to drip irrigation and less thirsty crops.
Yearly rain at Bikaner, 2006–2025, from NASA satellite data. Lighter bars are dry years (20% or more below average), when wells are drawn hardest.
To stop the water table falling, Bikaner has to put back or save 114 million m³ a year. At 335 mm of rain, here is what that looks like:
In practice it is a mix: recharge in towns, ponds and check dams in villages, and saving water on farms and in factories.
1 mm of rain on 1 m² is 1 litre. The surface factor allows for water lost to splash, evaporation and first-flush.