South Africa’s driest regions rely on groundwater, which dries up as the climate warms. Replenishing aquifers with excess rainfall may be a solution.
South Africa is the 30th driest country in the world. Over 400 towns, especially in the western and central parts of the country, rely on water from aquifers that they pump out of the ground (groundwater).
A rural dam of brown, muddy water, about the size of half a soccer field and not very deep looking. In 2018 an intense drought occurred in the Northern Cape province. Both dams and groundwater sources were depleted. Some towns, like Sutherland, passed “Day Zero” (the day water runs out) in 2021. To manage the crisis, the local authorities began water-shedding (shutting the water off except for a few scheduled hours daily). But this is not a lasting solution as climate observations show that rain is falling later than expected every year, and is not replenishing groundwater enough. In these dry areas, there is the possibility of another solution: managed aquifer recharge. This works by channelling surplus surface water into specially constructed basins, ponds or ditches. This water slowly seeps through the soil to recharge the aquifer. Water can also be pumped in. We are groundwater scientists who study aquifers. In a recent paper, we discussed how managed aquifer recharge had refilled groundwater in the rural Karoo towns of Carnarvon, Vanwyksvlei, Williston, Sutherland and Calvinia. These towns rely on borehole water, but rain was not replenishing the aquifers enough for the towns to keep drawing water from them. Our research sets out the specific approaches and successes of small-scale, low-cost schemes that used surplus rainwater to enhance the recharge of the aquifers. We found that managed aquifer recharge delivered a number of benefits. These included improving water supply in the towns and improving the quality of the water. There were also environmental benefits – some vegetation improved around some of the recharge sites. The vegetation stabilised the soil, allowing greater amounts of rain to filter back down into the aquifer instead of flowing away. Our research shows that groundwater can efficiently make up for a water supply shortfall in small towns. Most managed aquifer recharge schemes elsewhere in the world are large and relatively high cost. We’ve shown that it’s possible to use the method effectively at small scale and at low cost.How the small towns got their water supply back
An aquifer is like a underground dam. The bottom of an aquifer is like the bottom of the dam: if there is no more water in an aquifer it dries up, just like a dam. In all five projects, after being recharged, the aquifers water levels rose – in some cases, dramatically.Carnarvon: population 7,400
In 2015, we drilled six boreholes to a depth of 12 metres through clay layers in the river bed. This was so that when it rained and the river filled up, the water would seep into the ground faster. After continuous good rains since 2022, the aquifer water level rose from 24 metres below ground level (the bottom of the borehole) to 19 metres below ground level.Williston: population 3,400
This small town’s current managed aquifer recharge scheme, set up in 1983 by the municipality and the Department of Water and Sanitation, is made up of check dams – barriers placed across rivers or channels to slow the movement of water. These check dams are in a river tributary and, together with the town dam, serve as basins from which water infiltrates into the ground. A heavy rainfall event of 40mm in 2022 caused a 10 metre rise in the groundwater level. This amount of water sustained the town for two years.