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 use is within safe limits here. 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 25 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 |
|---|---|---|---|---|---|
| 2017 | 93.8% | – | – | Critical | First assessment in this series. |
| 2020 | 78.4% | 379 million m³ | 483 million m³ | Semi-critical | Down 15 points since 2017. |
| 2022 | 69.2% | 393 million m³ | 568 million m³ | Safe | Pumping up 4% (379 → 393 million m³). Safe limit up 18% (483 → 568 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
| 2023 | 62.7% | 383 million m³ | 610 million m³ | Safe | Pumping down 3% (393 → 383 million m³). Safe limit up 8% (568 → 610 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
| 2024 | 67.3% | 408 million m³ | 606 million m³ | Safe | Pumping up 7% (383 → 408 million m³). Safe limit down 1% (610 → 606 million m³). Main reason: more water was pumped out, mostly for irrigation (371 → 395 million m³). |
| 2025 | 68.8% | 342 million m³ | 497 million m³ | Safe | Pumping down 16% (408 → 342 million m³). Safe limit down 18% (606 → 497 million m³). |
Million m³: 1 million m³ = 100 crore litres. 2009 and 2013 used the older GEC-97 method.
Loading 20 years of rainfall…
481 of 3,316 water bodies (15%) 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 Siddipet…
Source: 1st Census of Water Bodies, Ministry of Jal Shakti (counted in 2018-19, published 2023).
Groundwater here is in balance. Keeping it that way means recharging as the area builds up and paves over.
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.
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.
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.
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, Siddipet (Telangana) pumped out 69% of the groundwater that can be safely taken out each year, which puts it in the "safe" category. That is 25 points lower than in 2017.
No. At 69% of the safe yield, Siddipet is safe, though recharge is still needed as demand grows.
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.
The first Census of Water Bodies counted 3,316 water bodies in Siddipet, including 1,386 ponds. 481 of them were not in use.
Yearly rain at Siddipet, 2006–2025, from NASA satellite data. Lighter bars are dry years (20% or more below average), when wells are drawn hardest.