How the Restored Pond Works
A pond is a simple piece of infrastructure: a basin that catches monsoon rain, holds it, and lets it soak slowly into the ground. These diagrams show the mechanism. They are schematic and not drawn to scale.
How it works
Where the monsoon rain goes
The same piece of land, before and after restoration. Buried, it sheds water into the streets. Opened up, it stores water and passes it down to the aquifer.
- A buried basin. Years of household waste and construction rubble filled the pond and were compacted flat.
- Rain runs off. With nowhere to collect, monsoon rain runs across hard ground into streets and drains, adding to waterlogging (Dev, 2017; Shuster et al., 2005).
- Little recharge. Very little water soaks through the compacted fill, so the groundwater below is not replenished.
- Catches the rain. The open basin collects rain and runoff from the ground around it. About 77% of the district's annual rain arrives in the monsoon months (Dev, 2017).
- Holds stormwater. Water held in the pond is water kept off the roads and out of the drains at the peak of a downpour (Balasubramanian, 2023).
- Recharges groundwater. Stored water seeps slowly through the bed into the aquifer, the same principle as a percolation tank (Raj et al., 2024).
- Plants clean the water. Vegetation on the banks and in the shallows traps sediment and takes up nutrients and pollutants (Fletcher et al., 2024).
- Cools the air. Evaporation from open water lowers the temperature of the air around it (Jandaghian & Colombo, 2024).
- Makes habitat. Open water and planted margins give insects, amphibians and birds somewhere to live (Hill et al., 2021).
A year in the life of the pond
The pond will not look the same all year. It fills in the monsoon and draws down through the dry months, and that cycle is how it does its work.
Rain and runoff fill the basin. Most of the year's rain arrives in these months (Dev, 2017).
The pond holds its water, and the water seeps slowly into the ground (Raj et al., 2024).
Planted margins take hold, and the standing water becomes habitat for insects, amphibians and birds (Hill et al., 2021).
Evaporation is at its highest and the water draws down. Like many water bodies in Gurugram, the pond may dry out before the next monsoon.
How planting keeps the water clean
The research the project draws on describes three planting zones, each doing a different job, from the top of the bank to the open water.
- AThe bank. Trees, shrubs and grasses form a buffer that slows runoff and filters it before it reaches the water (Mishra et al., 2025).
- BThe shallows. Reeds and other plants rooted at the water's edge trap sediment and take up nutrients (Fletcher et al., 2024).
- COpen water. Planted floating rafts and native aquatic plants treat the water itself (Addo-Bankas et al., 2022).
What the design has to manage
A pond that works on paper can still fail in the ground. These are the processes that decide whether Badshahpur Pond keeps holding, cleaning and recharging water over the years, and what each one asks of the design.
The water budget
Every pond keeps the same account. Water comes in as rain and runoff, and leaves by seeping into the ground, evaporating or overflowing. Only the share that seeps down recharges the aquifer.
- 1Rain. Falls straight onto the pond. About 77% of the district's annual rain arrives in the monsoon months (Dev, 2017).
- 2Runoff. Hard surfaces increase both the volume and the speed of the water running off them (Shuster et al., 2005). The area draining to the pond decides how much arrives.
- 3Percolation. Water seeping through the bed, the useful output. It depends on permeable soil beneath the pond (Bouwer, 2002).
- 4Evaporation. Water lost to the air, at its highest in the hot months before the monsoon.
- 5Overflow. Once the basin is full, the surplus has to leave by a safe route.
Change in stored water = rain + runoff − percolation − evaporation − overflow
The terms in blue add water and the terms in brown remove it. Of the three losses, only percolation reaches the aquifer.
- Percolated into the aquifer: 57 to 63%
- Evaporated: 37 to 43%
A percolation tank in hard-rock terrain in South India, monitored for two years. About 80% of the water that percolated was later pumped out again by neighbouring boreholes (Massuel et al., 2014). Badshahpur's soil and climate are different, so its own figures have to be measured.
- The area that drains to the pond and the volume the basin can hold.
- A record of the water level through the year.
- The rate at which water soaks into the bed, tested on site (Bouwer, 2002).
Silt: why a pond needs upkeep
Runoff carries soil with it, and ponds are very good at trapping that sediment (Verstraeten & Poesen, 2000). Left alone, a pond slowly fills itself in and seals its own bed.
- Sediment arrives. Soil washed off the surrounding ground enters with the runoff and settles in the still water.
- The bed clogs. A layer of fine material builds up on the bed and blocks the pores of the soil beneath, so less water seeps through (Bouwer, 2002).
- The basin shrinks. Each year the pond is shallower and holds less water.
- A silt trap at the inlet. Letting sediment settle out before the water reaches the pond limits clogging (Bouwer, 2002), and a small trap is far easier to dig out than the whole bed.
- Planted banks. A buffer of grasses, shrubs and trees slows runoff and filters it before it reaches the water (Mishra et al., 2025).
- Desilting in the dry season. Drying the bed and scraping off the clogged layer restores the rate at which water soaks in (Bouwer, 2002).
- An inlet where silt can settle and be dug out.
- Stable, planted banks.
- A desilting routine for the dry season, with someone responsible for it.
What lies under the bed
This pond was used as a dump. Water that passes through buried waste dissolves what is in it and becomes leachate, which can carry dissolved organic matter, salts, heavy metals and synthetic chemicals (Kjeldsen et al., 2002). Around the Gazipur landfill in Delhi, leachate was found to have contaminated the groundwater (Mor et al., 2006).
- Water seeps down. The pond does what it was built to do and sends water into the ground.
- It passes through the waste. On the way it dissolves contaminants out of whatever is still buried there.
- The aquifer receives them. Recharge turns into a source of pollution.
- Excavate to natural soil. The dumped material has to come out across the whole bed, not only where the water will stand.
- Water seeps through clean ground. The ground beneath a recharge basin has to be free of polluted material (Bouwer, 2002).
- The aquifer gains clean water. Recharge adds to the groundwater without degrading it.
- Excavation that reaches natural soil across the whole bed.
- A soil test of the finished bed.
- A water quality test once the pond holds water.
Three more things to manage
Standing water in a city brings its own problems and its own opportunities.
Runoff and sewage bring nitrogen and phosphorus. Too much of either feeds algal blooms, which strip oxygen from the water (Smith et al., 1999). Keeping sewage out comes first: about one water body in five in Gurugram is at risk from it (GMDA, 2019).
Still, shallow water choked with plants breeds mosquitoes. Research on constructed wetlands points to design and upkeep: areas of open, deeper water, vegetation that is kept in check, and conditions that favour the natural predators of the larvae (Walton, 2012).
New ponds are colonised quickly. A group of new ponds in England, monitored for seven years, came to hold more plant and invertebrate species than established ponds nearby, helped by clean water and other wetlands close by (Williams et al., 2008).
What still has to be measured
These are the mechanisms the restoration relies on. They are not results yet. How much water the pond holds, how quickly it seeps into the ground and how clean that water is will be assessed once the pond has been through a monsoon. Measurements of this kind are scarce: a review of rainwater harvesting in India found surprisingly little field evidence of how much individual structures recharge (Glendenning et al., 2012).
References on this page19 sources
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Every source used on this website is listed on the References page.