Aquifers could be part of solving crisis

The discovery of aquifers — underground earth formations that hold water — often creates excitement because of their ability to ease water scarcity in a region.

For instance, about 10 years ago a large aquifer was discovered in Kenya’s Turkana region.

This is one of the hottest, driest parts of Kenya and frequently suffers from drought.

The government said the aquifer could supply the entire country with water for 70 years.

More recently, the US announced the discovery of five aquifers in Niger, one of Africa’s most water scarce countries, containing over 600billion cubic metres of water.

To put it into perspective, Egypt’s current water demand is 114-billion cubic metres of water a year.

These are welcome announcements. Due to a changing climate and the increasing demands of a growing population, many of Africa’s surface water resources — such as dams and rivers — are under strain.

They are overused and are being slowly depleted.

Alternative water sources, like aquifers, need to be explored.

Based on Africa’s geology we know aquifers are highly prevalent across the continent.

But, as a groundwater and aquifer expert, I want to highlight that they’re not always going to help address water scarcity.

For instance, early research findings deemed Kenya’s Turkana aquifer water unfit for use due to high salinity.

It’s important to bear these challenges in mind so that expectations can be managed.

It is also useful for planners and governments, as they need to think of other ways around the water scarcity problem.

The volume of groundwater that’s held in African aquifers is estimated to be 0.66m km³.

This is more than 100 times the annual renewable freshwater resources stored in dams and rivers, and 20 times the freshwater stored in Africa’s lakes.

The size and shape of an aquifer is based on the body of rock beneath the Earth’s surface.

Some can be in the form of caves and hold water on a large scale.

Some can range from a few metres thick to hundreds of metres with multiple layers.

Aquifers can also extend for many kilometres or be localised in certain areas.

Water gets into these aquifers in different ways.

Some are filled by new rainfall, others hold old, or ancient, rainfall.

In Africa, most are found less than 50m below the ground’s surface.

Many of Africa’s aquifers are spread across country borders, meaning countries have to share the water resource.

The largest volumes of groundwater in Africa are found in large aquifers in Libya, Algeria, Egypt and Sudan.

There are various ways to tap into aquifers, including hand-dug wells, drilled wells and boreholes, and natural springs.

Some countries have already taken steps to tap into aquifers.

SA has two huge aquifers. The largest stretches from Cape Town to Gqeberha, a city 750km away.

This geological formation covers a surface area of 37,000km² and ranges in thickness from 900m to 4,000m. The other big one is the Cape Flats aquifer.

It is estimated that by 2036, almost R5bn will have been invested to tap these aquifers.

They will yield about half of the amount of water in the Berg River dam, which provides almost 20% of the City of Cape Town’s supply.

Another large aquifer on the continent, containing only ancient trapped water, is the Nubian Sandstone in North Africa.

It covers about 2-million km², and spans Libya, Egypt, Sudan and Chad.

It contains more than 150,000km³ of groundwater — more water than the Nile River discharges in 500 years.

The countries it spans are tapping into the aquifer and have agreed on its fair use.

Libya has undertaken the Great Man-Made River project to pipe water hundreds of kilometres from the Nubian sandstone to the coast by means of gravity flow.

But aquifers aren’t a silver bullet. There are many factors to consider when using them as a water source.

The distance between the aquifer and where the water is needed can be an obstacle.

In some places in Africa, this distance is covered by women carrying buckets and walking for many kilometres.

The construction of pipelines and infrastructure can be costly.

A related challenge is the depth required to drill for groundwater. This can incur great costs.

A type of X-ray of the surface is done to confirm whether there are groundwater resources worth exploiting, and then there’s the expense of a drilling rig.

Water quality in an aquifer isn’t always good. Sometimes it’s polluted by human activity.

An example is outside Gqeberha, which has one of the largest drilled wells in the southern hemisphere. It yields about 100 litres per second.

Unfortunately the iron content of the water is above the required standards. It has to be treated before it is drinkable.

Industrial activity, agriculture and chemical leaks can also affect groundwater quality.

Overpumping can also cause seawater to get into groundwater.

The more dense seawater migrates to replace the freshwater removed from an aquifer.

This has devastating implications for the storage capacity of aquifers as well as the overall groundwater quality.

It has been seen in certain coastal aquifers. Saline intrusions are difficult to address.

Despite these concerns, aquifers have the capacity to provide some water in almost all parts of Africa.

Groundwater is part of the solution to water scarcity, but not the entire solution.

It should be used in a way that keeps it available long into the future.