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 is under pressure 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 28 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 | 67.0% | 145 million m³ | 216 million m³ | Safe | First assessment in this series. |
| 2013 | 74.0% | 162 million m³ | 218 million m³ | Semi-critical | Pumping up 12% (145 → 162 million m³). Safe limit up 1% (216 → 218 million m³). Main reason: more water was pumped out, mostly for irrigation (133 → 150 million m³). |
| 2017 | 99.8% | 187 million m³ | 188 million m³ | Critical | Pumping up 16% (162 → 187 million m³). Safe limit down 14% (218 → 188 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 | 80.8% | 142 million m³ | 176 million m³ | Semi-critical | Pumping down 24% (187 → 142 million m³). Safe limit down 6% (188 → 176 million m³). Main reason: less water was pumped out, mostly for irrigation (176 → 125 million m³). |
| 2022 | 80.1% | 139 million m³ | 174 million m³ | Semi-critical | Pumping down 2% (142 → 139 million m³). Safe limit down 1% (176 → 174 million m³). |
| 2023 | 80.2% | 128 million m³ | 160 million m³ | Semi-critical | Pumping down 8% (139 → 128 million m³). Safe limit down 8% (174 → 160 million m³). |
| 2024 | 76.0% | 126 million m³ | 165 million m³ | Semi-critical | Pumping down 2% (128 → 126 million m³). Safe limit up 3% (160 → 165 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
| 2025 | 72.3% | 126 million m³ | 174 million m³ | Semi-critical | Pumping up 0% (126 → 126 million m³). Safe limit up 5% (165 → 174 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…
238 of 337 water bodies (71%) 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 Nuh…
Source: 1st Census of Water Bodies, Ministry of Jal Shakti (counted in 2018-19, published 2023).
Haryana mapped its ponds from satellite images in 2023, so its count differs from the census, which recorded water bodies on the ground in 2018-19. It also counts the tube wells that pump groundwater for irrigation.
Source: Haryana Water Resources Atlas 2025, Haryana Water Resources Authority. Ponds and water bodies mapped from satellite data in 2023 (Pond Authority Haryana, HARSAC); irrigation tube wells counted in 2022-23 (Ground Water Cell, Haryana).
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.
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, Nuh (Haryana) pumped out 72% of the groundwater that can be safely taken out each year, which puts it in the "semi-critical" category. That is 28 points lower than in 2017.
No. At 72% of the safe yield, Nuh is semi-critical, 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 Haryana Water Resources Atlas 2025 counts 16,108 tube wells used for irrigation in Nuh district (2022-23).
The first Census of Water Bodies counted 337 water bodies in Nuh, including 337 ponds. 238 of them were not in use.
Yearly rain at Nuh, 2006–2025, from NASA satellite data. Lighter bars are dry years (20% or more below average), when wells are drawn hardest.