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.
Groundwater level in Dausa
233%Over-exploited
This area pumps out 2.3 times the water that 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. Up 56 points since 2017.
586 million m³pumped out each year (2025)
252 million m³can be taken out safely each year
334 million m³yearly shortfall drawn from stored water
80%goes to irrigation; the rest to homes and industry
Extraction since 2009
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.
Safe · up to 70%Semi-critical · 70–90%Critical · 90–100%Over-exploited · above 100%
Show the numbers
| Year | Stage | Pumped out | Safe limit | Category | What changed |
|---|---|---|---|---|---|
| 2009 | 158.0% | 399 million m³ | 252 million m³ | Over-exploited | First assessment in this series. |
| 2013 | 163.0% | 416 million m³ | 254 million m³ | Over-exploited | Pumping up 4% (399 → 416 million m³). Safe limit up 1% (252 → 254 million m³). Main reason: more water was pumped out, mostly for irrigation (370 → 390 million m³). |
| 2017 | 176.5% | 408 million m³ | 231 million m³ | Over-exploited | Pumping down 2% (416 → 408 million m³). Safe limit down 9% (254 → 231 million m³). Main reason: less water soaked back in, from weaker rain, less canal seepage or more paved ground. CGWB changed its method in 2017 (GEC-97 to GEC-2015), so part of this change comes from the new method. |
| 2020 | 216.3% | 534 million m³ | 247 million m³ | Over-exploited | Pumping up 31% (408 → 534 million m³). Safe limit up 7% (231 → 247 million m³). Main reason: more water was pumped out, mostly for irrigation (384 → 495 million m³). 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 | 208.3% | 508 million m³ | 244 million m³ | Over-exploited | Pumping down 5% (534 → 508 million m³). Safe limit down 1% (247 → 244 million m³). Main reason: less water was pumped out, mostly for irrigation (495 → 402 million m³). |
| 2023 | 233.2% | 586 million m³ | 251 million m³ | Over-exploited | Pumping up 15% (508 → 586 million m³). Safe limit up 3% (244 → 251 million m³). Main reason: more water was pumped out, mostly for irrigation (402 → 475 million m³). |
| 2024 | 243.7% | 591 million m³ | 242 million m³ | Over-exploited | Pumping up 1% (586 → 591 million m³). Safe limit down 4% (251 → 242 million m³). Main reason: less water soaked back in, from weaker rain, less canal seepage or more paved ground. |
| 2025 | 232.6% | 586 million m³ | 252 million m³ | Over-exploited | Pumping down 1% (591 → 586 million m³). Safe limit up 4% (242 → 252 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
Million m³: 1 million m³ = 100 crore litres. 2009 and 2013 used the older GEC-97 method.
Loading 20 years of rainfall…
Ponds and lakes in Dausa
5 of 9 water bodies (56%) are not in use: dried up, silted, built over or polluted. Bringing them back is one of the cheapest ways to recharge groundwater.
Loading the map of water bodies in Dausa…
- Tanks7
- Reservoirs2
Source: 1st Census of Water Bodies, Ministry of Jal Shakti (counted in 2018-19, published 2023).
What will fix it here
Most of the water here goes to farming, so using less on fields matters as much as recharge.
Recharge pits and shafts in open land
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.
Revive village ponds and johads
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.
Rooftop rainwater recharge
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.
Check dams and contour trenches
On sloping or rocky land, small dams on seasonal streams and trenches along contours slow water down long enough for it to sink in.
Treat and reuse wastewater
Treated water from a sewage treatment plant can run flushing, gardens, cooling towers and construction, which today often draw on borewells.
Frequently asked questions
What is the groundwater level in Dausa?
In the 2025 Central Ground Water Board assessment, Dausa (Rajasthan) pumped out 233% of the groundwater that can be safely taken out each year, which puts it in the "over-exploited" category. That is 56 points higher than in 2017.
Is groundwater in Dausa over-exploited?
Yes. Dausa takes out more groundwater than rain and other sources put back, so the water table keeps falling.
How can groundwater be recharged in Dausa?
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.
How many ponds and lakes are there in Dausa?
The first Census of Water Bodies counted 9 water bodies in Dausa, including 0 ponds. 5 of them were not in use.
Other districts in Rajasthan
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