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Dr Eelco Lukas, a geohydrologist, is the Director of the Institute for Groundwater Studies at the University of the Free State (UFS).

Nearly two-thirds of South Africa depends solely or partially on groundwater for domestic needs, and in a water-stressed country this source is becoming increasingly important. But we need to use it wisely.

Dr Eelco Lukas, a geohydrologist, is the Director of the Institute for Groundwater Studies at the University of the Free State (UFS). He explains that all the natural water found in the earth’s subsurface is called groundwater. “When we look hard enough, we can find groundwater almost everywhere.  But that does not mean that we can start pumping groundwater at any location.  In many places, the amount of groundwater available (yield) is so little, or the water so deep that it is not financially viable to pump it.  Another problem might be the quality of the water.”

Numerous towns and communities depend solely on groundwater and many towns use a combined supply of surface and groundwater. When the town or settlement is far from any surface water and groundwater is available, boreholes are drilled. Depending on the size of the settlement, the boreholes are equipped with electrical or hand pumps.

Most of the big cities use surface water in their water pipes. Almost all big cities worldwide are located close to a supply of freshwater.  Cape Town has drilled many boreholes in the past two years to augment the city’s water supply.  However, problems can arise when a borehole is drilled for a community with a certain number of people, and soon there are more people than the borehole can supply for. It is not so much a case of the ‘borehole drying up’ but that the capacity has been exceeded.

Misconceptions about groundwater

With increasing drought and water restrictions being imposed, many people opted for their own borehole. When so many people draw water from the same source, the water table will drop. It can be compared to drinking a milkshake, but when five other people also drink with straws from the same milkshake, all will be left thirsty. 

Dr Lukas says because groundwater is something that cannot be seen with the naked eye, the general public has many misconceptions about groundwater. Some people think that you can drill a hole just anywhere and that you will find water, while others believe that water flows in underground rivers. It generally moves very slowly, only a few metres per year. And if it rains in a specific place, it does not mean that water will reach a particular borehole.

“Sustainable groundwater usage is the certainty that enough groundwater is available in years to come.  Sustainability is dependent on two external factors, namely demand and supply.  Unfortunately, both these factors are beyond the control of the geohydrologist.  When enough water is available for a community, the chances are that the community starts to grow, thereby enlarging the demand.  If the higher demand cannot be met, sustainability is no longer possible. When a change in rainfall pattern results in a decline of the precipitation, the groundwater recharge will become less, resulting in a lower supply of water.”


How does water move?

Groundwater moves through openings in the subsurface. These openings can be large (a millimetre to a few centimetres), but most of the time they are small, only a fraction of a millimetre. These are called pore spaces.  Water can only move through the pores if the pores are connected to other pores. The ease with which water can move through the rock is called hydraulic conductivity and is expressed in volume per area per time.  

Dr Lukas explains that different types of rock have different sizes of pore openings. The speed at which water can move through unconsolidated materials ranges from 1 000 m/d (gravel) to 10-8 m/d (clay). Consolidated materials range from 1 000 m/d (highly fractured rock) to 10-7 m/d (shale).  Sandstone, a rock that occurs in abundance in South Africa, has a typical hydraulic conductivity of 10-2 m/d, meaning that the speed at which the water flows is around 1 cm/d, which is less than 4 metres per year.  

In a way, you can compare groundwater flow to a pipe filled with marbles.  If you remove one marble at the one side, a marble may enter the pipe on the other side.  Although it may take the marble a long time to reach the other side of the pipe, the movement of the marbles is noticed almost immediately, says Dr Lukas.

Before groundwater is used, experts must make sure that it is suitable, Dr Lukas says. This is one of the areas that the Institute of Groundwater Studies at the UFS excels in. The institute also provides a complete service to industries through field investigations, the development of specialised field equipment, a well-equipped commercial and water research laboratory, and a number of computer models for the management of the aquifers, protecting them from pollution.

There are different standards for different purposes.  The best-known standard is the drinking 
water standard (SANS 241).  The water is tested for microbiology, as well as for the physical, aesthetic, operational and chemical determinants, and for the taste and colour.

There are several geophysical methods to locate groundwater.  “It must be stressed that the geophysical methods do not actually indicate places with water, but rather places where the geology and geological features support the presence of groundwater,” he says.

Different techniques are used to ‘look’ at different depths.   Water found close to the surface (upper 20 m) is often young water, meaning that it has been recharged not too long ago.  Because it is so close to the surface, it is vulnerable to contamination.   Deeper water is probably a bit older and because it is farther below the surface, it is more protected against surface contamination and the quality of this water is generally good.  Really deep groundwater (> 200 metres deep) will be even older and may have elevated salt content due to the long residence time of the water.

How much groundwater do we have?

Groundwater is a significant source of water, and in some parts of the country the only source of potable water.  According to the Department of Water Affairs and Sanitation, the most recent estimate of sustainable potential yield of groundwater resources at high assurance is 7 500 million m³/a, while current groundwater use is estimated at around 2 000 million m³/a. Allowing for an underestimation on groundwater use, about 3 500 million m³/a could be available for further development.  Unfortunately, if there is a shortage of water on one side of the country, it cannot be supplemented with water from the other side.
 
With a drought, the amount of water falling from the sky is below average, which means that the available water to recharge is also less. With less recharge water, the groundwater levels will decline.  To make things worse during a drought, groundwater users will pump more water to make up the deficit in rainfall, thereby accelerating the drop in water levels.

“Groundwater can be used to help humanity. The pore space in aquifers can be used to store water during a wet period, to be used later during a drought. This is called water banking, where water is injected into the aquifers (artificial recharge) during a period when there is enough water and pumped from the same aquifer during a period of water shortage,” says Dr Lukas. 

News Archive

Year-long programme to celebrate the story of life and survival
2009-02-13

 
At the launch of the UFS's year-long programme to celebrate the story of life and survival were, from the left: Prof. Schalk Louw, Department of Zoology and Entomology, Prof. Jo van As, Department of Zoology and Entomology, Prof. Maitland Seaman, Centre for Environmental Management, and Prof. Matie Hoffman, Department of Physics. All four are associated with the UFS.
Photo: Hannes Pieterse

A year-long programme to celebrate the 200th anniversary of the birth of Charles Darwin and the 150th anniversary of the publication of his scientifically important book “The Origin of Species” was launched yesterday (the birth date of Darwin) by the University of the Free State (UFS) on its Main Campus in Bloemfontein.

The UFS is the only university in the country that is presenting such an extensive programme on life and survival. Yesterday’s launch programme entailed a portrayal of the life of Darwin and a presentation on what nature tells us about cosmic history. It was the start of a year-long lecture programme in which various departments at the UFS will take part.

“The lecture programme, called “The story of life and survival”, forms a cycle of the progress of man and does not only focus on Darwin. The programme aims to portray the influence of Darwin’s theory of evolution on a wide range of disciplines. We see this as a good opportunity to promote science in its broadest context,” says Prof. Jo Van As, head of the Department of Zoology and Entomology at the UFS.

The lecture programme will include topics such as the geological evolution of our planet, extinction, Darwinian agriculture, the road to civilisation, the proliferation of technology and communication, human demography and the human impact on the environment. It will be concluded in February 2010 with a lecture on the future of evolution.

The programme is spearheaded by the Department of Zoology and Entomology at the UFS, in conjunction with the National Museum and the Central University of Technology.

“Today evolution is no longer considered to be a theory and is widely accepted by most serious scientists as the process responsible for the diversity of life on our planet,” says Prof. Van As.

Complete programme:

26 February 2009: The geological evolution of our planet
13 March 2009: Origin of life, prokaryotes and eukaryotes
24 March 2009: Extinction
16 April 2009: Evolution and biodiversity of plants
30 April 2009: Evolution and biodiversity of animals
14 May 2009: The mechanisms of evolution: Heredity and Natural Selection
28 May 2009: Origin of humankind
4 June 2009: Darwinian agriculture
30 July 2009: Road to civilisation
6 August 2009: Human demography
20 August 2009: Proliferation of technology and communication
10 September 2009: Human impact: On the environment
8 October 2009: Human impact: Resistance, ectoparasites, HIV/Aids, antibiotics
22 October 2009: How to care for the world
12 February 2009: The future of evolution

Media Release
Issued by: Lacea Loader
Assistant Director: Media Liaison
Tel: 051 401 2584
Cell: 083 645 2454
E-mail: loaderl.stg@ufs.ac.za
13 February 2009

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