Groundwater is the name used to describe water which is stored underground in permeable rocks.
The period of storage may be a few weeks or several years depending on the geology. Most groundwater flows and emerges at the ground surface as a spring or within a river.
Groundwater and surface water are intimately connected such that pollution which enters groundwater can emerge in surface water.
Equally, groundwater can be affected by polluted surface water. Groundwater is used for drinking water supply and by industry. Pumping too much groundwater can cause rivers to dry up and the level of lakes to fall unacceptably low.
Near the coast, over abstraction can cause salt water to move into the aquifer rocks reducing the quality of the freshwater.
What is Groundwater?
Groundwater is water that has drained through surface layers of soil and rock until it reaches a layer of rock material through which it cannot pass, or can pass only very slowly. This results in the accumulation of water in the rock layers above this impermeable layer. The water is stored in gaps in the rock, or between the particles of which the rock is composed. Rock which retains water in this way is called an aquifer.
Rock types which can hold water include chalk, limestone and sandstone. Rock types which do not hold water but can prevent water moving out of a permeable rock type include granite, basalt and mudstone. Groundwater supplies springs and wells and, when there has been a period with little rain, it is often groundwater that maintains flow in rivers rather than surface drainage from land.
About 35% of all public water supply in England and Wales comes from groundwater which has undergone treatment (Source: Environment Agency Facts and Figures). In more remote areas, where there is no public water supply, a household may take its water supply direct from groundwater via a borehole and use it with little or no treatment if the aquifer is of good quality. Industry and agriculture also abstract water directly from aquifers either because they cannot, or it is not convenient, to take water from the mains supply or because they do not need to use water of potable quality.
Photographed in the winter of 2000/01 during the period when rainfall and subsequent recharge to many aquifers in England exceeded previously recorded quantities.
As a result, groundwater levels rose to their highest recorded levels leading to extensive groundwater flooding mainly in the upper, normally dry valleys on the dip slope of the Chalk escarpment.
At Tancred Pit borehole, water levels are between 7 and 10 metres below ground under normal conditions. In the background groundwater flooding of the dry valley (see crop pattern), as a result of the exceptionally high groundwater levels, can be seen.
Photo and details courtesy of Rob Ward and Chris Train
Pressures and Impacts
An aquifer may be as little as 30m from the surface, or as much as 300m. It costs more to pump water from the deeper aquifer but the water quality in the deeper one may be better than the shallower since contaminants which the water may be carrying are removed as the water moves through the rock.
Historically, groundwater has been naturally very clean because of this filtering effect. However, increased use of chemicals in everyday life means that groundwater is now vulnerable to the same pressures as water at the surface. Since water continuously flows from one to the other (See figure 1), groundwater can become polluted with nutrients or chemicals when surface water carrying these substances drains into the groundwater environment.
Diffuse sources of groundwater contamination include pesticide and fertiliser use. Point-specific sources include industrial spills, leaking oil and chemical storage tanks and landfill sites. Normally it is easier to remedy a point-specific source since its point of origin can be relatively easily identified.
Since water continuously flows from one to the other, groundwater can become polluted with nutrients or chemicals when surface water carrying these substances drains into the groundwater environment.
Diagram courtesy of the Groundwater Forum
When groundwater is used at rates which are greater than the rate at which it is replaced by natural processes, its level within an aquifer drops. This will happen naturally during the summer and may be protracted in drought years. However, prolonged abstraction for water supply purposes above the rate that an aquifer can support can impact rivers, wells and wetlands connected to the aquifer. Wildlife habitat and recreational fisheries and boating will be negatively affected where excessive groundwater use impinges on river water supply. Where there is less water entering a river, the chemical quality of the river can suffer since the dilution of any chemicals present will be reduced and this can lead to fish death.
Over-abstraction is being more widely identified as a problem and water companies and environmental protection bodies are increasingly working together to remedy the situation.
Freshwater in an aquifer near the coast will exist in balance with the salt water which is contained in the aquifer beneath the sea. Salt water is heavier than fresh water so at the margin between fresh and salt waters it will lie underneath the fresh water. The boundary between the two moves through the year, moving further out to sea when winter rainfall increases the pressure and volume of freshwater in the landward side of the aquifer.
Where freshwater abstraction from the coastal aquifer is not in equilibrium with the flow and ebb of these two bodies of water, salt water can intrude into the zone of freshwater abstraction and reduce the quality of water supply. This is termed saltwater intrusion and it is particularly prevalent in hot climates where fresh water is in short supply.
Where freshwater abstraction from the coastal aquifer is not in equilibrium with the flow and ebb of these two bodies of water, salt water can intrude into the zone of freshwater abstraction and reduce the quality of water supply
Diagram courtesy of the Groundwater Forum
The southern coast of Spain suffers saline intrusion because freshwater abstraction for the tourist and horticultural industries exceeds the ability of the freshwater aquifer to supply. However, saltwater intrusion also occurs in the UK where there is excessive abstraction from coastal aquifers.
There are several ways that groundwater may be protected from contamination. The spillage of substances which may cause pollution should be avoided through the use of good management practice. Fertilisers should be used in a fashion which maximises their use by the crop and minimises leaching losses to rivers and groundwater. This is the objective of creating Nitrate Vulnerable Zones (see below).
Drinking water supplies may be protected by defining source protection zones within which development is limited in order to reduce the chance of spillage of potentially polluting substances. The size of the source protection zone will depend on the geology of the aquifer, including how fissured (cracked) the rock is, and hence how fast the groundwater is travelling through it. The degree of sensitivity is dependant on the proximity, with development being more restricted close to the point of abstraction.
The innermost zone is within 50m of the abstraction point, while Zone I is defined by the distance a particle of water travels through the saturated zone in 50 days, by which time pathogens should be absent. Prohibited development in these zones would include a petrol station or landfill site. Two further zones at a greater distance from the borehole are also defined in which such development would be discouraged.
Nitrate Vulnerable Zones
Nitrogen is a major plant nutrient and nitrate is the form in which nitrogen arising primarily from nitrogen fertilisers leaks into water, particularly groundwater. The loss of nitrate in soil water drainage is termed leaching. Agriculture is the primary source of nitrate in groundwater. Nitrate Vulnerable Zones have been identified in order to reduce the loss of nitrogen from agricultural land.
Nitrate Vulnerable Zones (NVZ) were introduced by the Nitrates Directive and have developed in two phases since 1998. From 1 January 2009, the areas covered by Nitrate Vulnerable Zones (NVZs) were increased to approximately 70% of England. This includes the 55 per cent originally designated in 2002. Within these zones, certain agricultural practices have to be adhered to in order to minimise nitrate leaching.These measures include limiting the total amount of nitrogen that can be applied in animal manures in any one year and defining strict periods when neither commercial fertiliser nor organic manures can be applied, and defining good practice for the use of nitrogen fertilisers on farms. The primary objective is to prevent nitrate entering groundwater in order that potable supplies do not exceed the EU maximum permissible concentration of 50mgl-1 nitrate.
Further reading on NVZs can be found at:
Rising Water Levels Under Cities
The groundwater level under London is rising rapidly – up to 3m per year in places and becoming problematic to many public buildings and private homes. London is located on chalk which has been used for private and industrial water supply for a great many years.
Deterioration in the water quality within the aquifer, due to urban and industrial pollution, has led private operations to become connected to the public water supply system. This, coupled with the closure of heavy industry and ceasing of their water abstraction, means that water in the aquifer is rising and coming to the surface at points where buildings are now located. The resolution to this is costly and needs to be tackled strategically to be effective.
The UK Groundwater Forum is an informal grouping of technical, industrial and research organisations which have an involvement with groundwater.
It was formed in 1995 as a means of consulting stakeholders during a study undertaking a strategic review of Groundwater Issues and Research Needs. The forum now operates a highly informative website, sponsors open meetings on topical groundwater issues and produces educational and technical publications.
Member organisations include the Environment Agency and the British Geological Survey.
The Groundwater Forum website gives an insight into the implications of the WFD and how it is being implemented in the UK - with an emphasis on groundwater. It also explains where the proposed new Directive on groundwater fits in.
A Groundwater Forum meeting dealing with implications of WFD for groundwater protection was held in March 2004.
The presentations are available on-line at the Forum website:
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