underground, under threat The state of groundwater in England and Wales We are the Environment Agency. It’s our job to look after your environment and make it a better place – for you, and for future generations. Your environment is the air you breathe, the water you drink and the ground you walk on. Working with business, Government and society as a whole, we are making your environment cleaner and healthier. The Environment Agency. Out there, making your environment a better place. Published by: Environment Agency Rio House Waterside Drive, Aztec West Almondsbury, Bristol BS32 4UD Tel: 0870 8506506 Email: [email protected] www.environment-agency.gov.uk © Environment Agency All rights reserved. This document may be reproduced with prior permission of the Environment Agency. Foreword The role of groundwater in providing us with good clean water has long been out of the public eye. But it is a vitally important resource, providing one third of the water we drink and feeding many rivers and wetlands. This summer’s drought has shown just how much we depend on groundwater, and the pressures that it is under. At the Environment Agency we aim to raise the profile of groundwater and give priority to its protection and management. In this report, our first on the state of groundwater, we outline the uses of groundwater as a water resource and then go on to look at the risks to this resource from pollution and over exploitation. At the end of the report we discuss how we manage groundwater and the challenges that we face. It is essential to plan now to secure the long-term health of groundwater for both the environment and public water supply. We will continue to look at groundwater as part of the bigger picture of water management, and we look forward to working in partnership with others to protect this asset for future generations. Paul Leinster Acting Chief Executive, Environment Agency Environment Agency The state of groundwater in England and Wales 3 underground The groundwater issue Most of our water resources are hidden beneath our feet as groundwater. Out of sight, and out of mind. To many of us that use it as a water supply, groundwater remains an unknown and under valued natural asset. There are two main threats to our groundwater resource: Demand • If people take too much groundwater and levels become too low, they might not be able to rely so much on groundwater for their public water supply. Many rivers and wildlife that depend on groundwater might also be harmed or lost. Pollution • Groundwater is vulnerable to contamination and difficult to clean if contamination occurs. It is intimately linked to both surface water and soils, so substances can get into groundwater from either. Groundwater provides clean, fresh water for our homes, industry, agriculture and environment. It is an integral part of the water cycle, linking rainfall to rivers, lakes and seas. But this resource is limited, so groundwater must be managed and protected so that future generations can benefit from this renewable resource. 4 Environment Agency The state of groundwater in England and Wales The amount of groundwater we can use depends on its accessibility and quality. It is especially valuable because it is normally pure and so needs little treatment. If groundwater is polluted, it may need treatment before it is used. This could be too expensive or too difficult to do and the resource may be lost. This report is published with our policy document, Groundwater protection: policy and practice, which explains how we will manage and protect groundwater. In this report we look at the current condition of groundwater. We give advance warning of the challenges that we will face and the changes that the Water Framework Directive will make necessary. Most of the information that we have about groundwater is based on the main aquifers used for drinking water and most of these are in England (See How does groundwater work? on page 7). This is where we have concentrated our monitoring. This means that we do not know as much about the condition of groundwater in minor aquifers, many of which are in Wales. Because of the limitations of the data, we do not know yet what the major issues are in Wales. We have been increasing our monitoring to find out if there are more widespread problems. under threat Summary of the main issues affecting groundwater Issue Now Future Demand Demand is high in some English regions. Everybody must use water carefully to ensure demand does not continue to grow. Potentially increasing Climate change Winter recharge might be reduced if, as predicted, rain falls in shorter heavier showers, but it could increase if winters are wetter. Demand would also increase during more frequent droughts. Uncertain Diffuse pollution comes from many small widespread sources. This makes it difficult to control and even more difficult to correct once it has happened. Nitrate is a particular problem. Pesticides are being used more effectively, which means less needs to be applied. Some pesticides have been banned; but they must not be replaced by others that are even worse. ☺ Same Urbanisation and large building developments can cause a variety of problems – increased demand, reduced recharge and further potential for pollution. Worse Diffuse pollution Pesticides Land use Same Environment Agency The state of groundwater in England and Wales 5 underground Why do we care about groundwater? Groundwater provides us with a range of benefits. To human health • People need a reliable supply of clean water to live. Water companies abstract, treat and distribute groundwater to the public. • In England about one third of the public water supply comes from groundwater, in Wales this proportion is far lower, at around three per cent.1 • Groundwater feeds a large number of small private supplies from springs, wells and boreholes. These provide water supplies in rural areas not connected to the public water system. These supplies are particularly important in Wales and upland England. To the economy • Industries and farms use groundwater, either from the public supply or from private sources. • Groundwater reserves are hugely important to the economy. They are estimated to be worth about £8 billion. • The UK market for bottled water is growing fast and is worth £1.7 billion a year. Each person in the UK drinks an average of more than 30 litres of bottled water every year.2 There are about 100 recognised natural mineral drinking waters in the UK,3 nearly all of which come from groundwater. 6 Environment Agency The state of groundwater in England and Wales To the environment • Rivers are partly fed by groundwater and some are almost totally dependent on it. The groundwater part (or base flow) varies less throughout the year than water running off the land surface, so in the summer most rivers and their ecosystems rely on groundwater to keep them flowing. Because of this some public supply abstractions from rivers actually come from groundwater. • Springs and groundwater seepages can form wetlands that support a unique ecology with specially adapted plant and animal species. Wetlands have other benefits too. They can help control flooding by retaining and slowly releasing surface water. They can also filter out sediments, nutrients and toxic substances, which prevents pollution of downstream rivers, but makes wetlands particularly vulnerable to contamination. under threat How does groundwater work? Groundwater comes from rainfall that has filtered down through the ground and is stored in permeable rocks, known as aquifers (Figure 1). The amount of water aquifers receive (known as recharge) varies throughout the year. Recharge rates and water levels are lowest in the summer and early autumn, when there is less rain and higher temperatures. In these conditions more water is evaporated at the surface and plants take more water from the ground, so less is available for recharge. Recharge rates are highest in the winter and groundwater levels reach a peak in early spring. Changes in groundwater levels lag behind rainfall, and this allows springs and rivers to continue to be fed by groundwater over the summer, which in turn causes the groundwater level to fall (Figure 2). Failure of winter rainfall over one or more years can lead to shortages in groundwater. Figure 1 The main aquifers in England and Wales are the Chalk in the south and east of England, sandstone in the west of England and Wales, and limestone (Figure 3). Most water circulates slowly in the upper 100 or 200 metres of an aquifer. In some places it can penetrate several kilometres below the surface, although at this depth the water becomes too salty to drink. Although at least 40 billion m3 of water is contained in the top 20 metres of the two main aquifers alone, over 16 times more than the total capacity of all surface reservoirs in the UK, only some of this is available to use.4 Groundwater flows through aquifers and out into rivers, lakes and the sea. The water table usually follows the shape of the ground surface above it, and gravity causes water to flow from high to low areas. Figure 2 Groundwater levels and rainfall, 1995 to 2005 The water cycle Groundwater level: Above average Below average Rainfall cloud High Rainfall outflow to spring infiltration evaporation groundwater (saturated rock) out flow river uptake by plants to r ive r outfl impermeable rock ow to sea Low sea saline groundwater 1995 1997 1999 2001 2003 2005 Environment Agency Environment Agency The state of groundwater in England and Wales 7 underground Water flows through cracks and pores in the rock and the flow speed varies with geology and depth. Groundwater samples can contain a mixture of water of different ages. Water that stays near the top of an aquifer might only be underground for a month, but some of the deepest water is thought to be millions of years old. Water in the Chalk in the south east of England can be 20,000 years old, originally falling as rain towards the end of the last Ice Age.4 The unsaturated soils and rock above groundwater can protect it from pollution. They often act as a filter, sieving out harmful chemicals and bacteria. But in some places groundwater is closer to the surface, so some contaminants do get through. Natural processes that help clean up groundwater, which take days or weeks in rivers and lakes, can take decades or centuries in groundwater. This is partly because water and pollutant flow is so slow, but also because microbial decay processes are slowed down by a lack of oxygen and nutrients, and low temperatures.5 Figure 3 Main aquifers in England and Wales Chalk Sandstone Limestone UK Groundwater Forum 8 Environment Agency The state of groundwater in England and Wales under threat Balancing supply and demand Many people rely heavily on groundwater whether they know it or not but groundwater systems also support other animals, plants and habitats. The amount of water taken (or abstracted) from an aquifer needs to be in balance with the rate of recharge and the amount of water that plants and animals in rivers and wetlands need to survive. Critically low water levels could cause irreparable harm to vulnerable and often rare habitats. Replacement sources of clean water would also have to be found for public supply, which would be extremely costly. In the future, water demand is set to increase, particularly with the projected growth in the number of homes being built.6 Changes in weather patterns, as a result of long-term climate change, could cause additional supply problems. Supply and demand In some parts of the country people take and use a lot of groundwater. In the future groundwater is likely to be under even more pressure from more homes being built in the driest and most groundwater dependent areas. It is tempting to think that the answer to water shortages caused by new housing is to build more reservoirs, but this is not always the right option in the long term. The best alternative is to manage demand by introducing water efficiency measures, controlling leakage or installing water meters. But there are also other ways to store and distribute large volumes of water. Water could be transferred between water companies, or aquifers that are not full to capacity can be used as ready made underground reservoirs. This takes advantage of a process known as aquifer storage and recovery.7 • The average annual recharge to the main aquifers is seven billion m3, and about 30 per cent of this is abstracted at a rate of nearly 7 million m3 per day8 (Figure 4). Most of this is abstracted in the south east of England. Only one per cent of the total is abstracted in Wales9 (Figure 5). This does not mean that there is spare groundwater. Any water abstracted from the ground is water that will not reach rivers. The Thames Gateway development Almost 120,000 new homes are planned on land either side of the Thames Estuary to the east of London.15 • Building water efficient new houses will help delay the need for extra water, but will not solve the problem. The issues: • More households will produce more sewage and waste. The risk of urban groundwater pollution will increase. Existing sewerage networks and waste water treatment works might not be able to cope. • Water in the area is already scarce and groundwater supplies are under pressure. More water will be needed to support the new homes, but it’s not clear where this water will come from and finding it will be costly. Developing the area will reduce infiltration to groundwater, possibly reducing aquifer recharge. Wetlands will also be lost. Environment Agency The state of groundwater in England and Wales 9 underground The Shropshire groundwater scheme In dry periods groundwater can be pumped out of aquifers into rivers to increase flow. There are over 50 of these augmentation schemes in England and Wales, usually used to protect the river environment or to support abstraction from the river downstream. We need to protect rivers during periods of low flow, but it is important that groundwater resources are not sacrificed to preserve the more visible surface water reserves. Figure 4 Groundwater replenishment and abstraction Replenishment Abstraction Million cubic metres/year 5,000 4,500 1,500 1,000 500 Chalk PermoTriassic sandstone Jurassic limestone Lower Greensand UK Groundwater Forum The £20 million groundwater scheme began in 1982 and is being completed in eight stages as water demands increase. When all phases are complete an extra 225,000 m3 per day will be able to be taken from the river for public supply, enough water for more than 600,000 homes.17 Figure 5 Groundwater abstracted in 2003 Percentage of total abstracted Wales 1% Anglian 16% Thames 25% Total = 2,388 Mm3 Midlands 17% South West 9% North East 7% Southern 20% North West 5% Environment Agency 10 The River Severn is a vital source of water for the West Midlands. During dry spells water is released into the river from two reservoirs, Lake Vyrnwy and Llyn Clywedog, to increase the flow. In exceptionally dry years this still may not be enough water. Groundwater is then pumped into the river from the sandstone aquifer that underlies much of North Shropshire. Environment Agency The state of groundwater in England and Wales Based on weather patterns over the last 50 years the groundwater scheme is likely be operated in two out of every five years. In other years water from the reservoirs will be enough to meet demand. under threat Groundwater provides a significant proportion of the public water supply in some areas. • In 2004/5 an average of about 150 litres per day of water was supplied to each person in England and Wales.10 Demand for water will continue to grow unless we improve water efficiency. Water companies need to make sure that leakage from the public water system is kept as low as possible, so the problem isn’t made worse. Figure 6 Public water supplied by groundwater 11% • The south east of England is an area of particular concern. It is a highly populated area with relatively low annual rainfall. As a result, the supply of water in the south east of England is limited. Some parts have less usable water per person than countries such as Syria.11 Many more homes are due to be built in the area, putting even more pressure on the water supply. • Groundwater provides a significant proportion of the public water supply in some areas. This varies around England and Wales according to where the aquifers are (Figure 6). In the Environment Agency Southern region more than 70 per cent of public water supply comes from groundwater.8 14% North West North East 40% 37% Midlands 3% Anglian Wales 35% Thames 74% Southern 30% South West Environment Agency • Seventy eight per cent of abstracted groundwater is supplied to households and businesses by water companies. Industry (12 per cent), aquaculture (five per cent) and agriculture (four per cent) also directly abstract large volumes12 (Figure 7). Figure 7 Estimated abstractions from groundwater by purpose Other Electricity supply Private water supply Agriculture Fish farming etc Spray irrigation Mineral washing Public water supply Other industry • In most Welsh aquifers, recharge is thought to greatly exceed abstraction, but we have found some areas (such as the sandstone in the Vale of Clwyd) where groundwater appears to be at or near its abstraction limit.13 Million litres/day • Our assessment for the Water Framework Directive showed that over a quarter of the groundwater bodies in England and four per cent in Wales are at risk of failing environmental objectives because of abstraction pressures.14 8,000 6,000 4,000 2,000 1995 1997 1999 2001 2003 Environment Agency Environment Agency The state of groundwater in England and Wales 11 underground Climate change Rainfall variation means that groundwater levels go up and down naturally, but changes in long-term weather patterns might mean that groundwater levels change permanently. In the future we need to make sure that we recognise these changes and find ways to manage them. • The volume of rainfall is predicted to increase, but shorter winters will mean that it will fall more intensely over a shorter period. Aquifers are recharged most effectively by prolonged steady rainfall, falling outside the plant growing season. Rainfall delivered over a shorter period might lead to a long-term reduction in recharge of some aquifers. Droughts are expected to be more common. • The changing weather patterns could also be felt in the environment. Lower groundwater levels can disrupt vulnerable and rare habitats. • Rising sea levels could also lead to a loss of groundwater resources and ecological damage, as seawater can mix with groundwater in low-level coastal aquifers. What happens when groundwater levels are too high? 12 Groundwater flooding Rising groundwater During periods of prolonged high rainfall, groundwater (which naturally flows towards lowlying areas) can rise to the surface and flood lowlying land and sub-surface structures. Groundwater flooding is rarer than river or coastal flooding and usually occurs in chalk areas.16 It can sometimes be more disruptive and damaging than surface water flooding, because it takes far longer for the water to recede. Groundwater flooding is a natural occurrence, but the problem is complicated when areas that have artificially low water tables due to past industrial abstraction are developed. When this abstraction stops, due to the decline of some industries, groundwater rises to the previous natural level. For instance, in London groundwater levels had fallen to 90 metres below the surface by the 1960s.4 Since then the rate of abstraction has declined and groundwater levels have recovered. The rising groundwater threatened to flood some parts of the underground infrastructure. The only way to stop this happening has been to increase abstraction again, to keep the water table below foundations and tunnels. Environment Agency The state of groundwater in England and Wales under threat Groundwater pollution Groundwater has deteriorated in quality over the last 50 years and we all need to take action now to stop things getting worse. Pollution from diffuse sources (rather than from point sources, which are easier to identify and manage) has been a problem for groundwater for some time. Anything soluble which is put on the land has the potential to get into an underlying aquifer, so everybody needs to be careful about what they put on gardens, roads and fields (Figure 8). There is direct interaction between groundwater and surface water. If groundwater is polluted, it can threaten surface water supplies, river ecosystems and wetlands. Contaminated public water supplies might have to be closed and replaced, or undergo more extensive treatment. Towns and cities Industry Rural communities leaking sewers petrol stations wat er tabl e public water supply • Almost half of the groundwater supply is now blended with cleaner water, treated or has been replaced (Figure 9).18 • One hundred and forty six groundwater sources have been closed since 1975 because of groundwater quality problems. At least 425,000 m3 per day have been lost in licensed output from the closures, about seven per cent of current abstraction levels (Figure 10).18 • The capital investment required to maintain drinking water quality is expected to be at least £15 to £36 million every year. Problems with groundwater quality cost the UK water industry £754 million between 1975 and 2004.18 Figure 9 Public groundwater supply in the UK affected by pollution Figure 8 Threats from pollution runoff road salt What does it cost? People drink lots of groundwater, but also pollute it. Water companies pay for it to be cleaned and these costs are passed on to water bills. Sometimes it gets so polluted that the aquifer can’t be used any more, and other sources have to be found. contaminated land oil storage manure, pesticides and fertilizer ploughing septic tank Nitrate Blending Treatment Closure Pesticides Blending Treatment Closure Other Blending and treatment Closure Volume (Ml/d) (cumulative) 4,000 3,000 landfill 2,000 groundwater flow private well saturated rock public water supply impermeable rock 1,000 1975 1980 1985 1990 1995 2000 2005 2010 UKWIR Environment Agency The state of groundwater in England and Wales 13 underground Polluting substances Diffuse pollution Pollution that comes from many small sources (diffuse pollution) is the main problem for groundwater. Substances that are spread on land, or leak from underground pipes or storage can contaminate aquifers. The problem is widespread, and diffuse pollution is hard to trace and prevent. • Around 81 per cent of groundwater bodies in England and 35 per cent in Wales are at risk of failing Water Framework Directives objectives because of diffuse pollution.14 Nitrate is the most widespread pollutant in England, others include pesticides, oil, solvents and potentially phosphate. Nitrate Nitrate is one of the most common groundwater pollutants. It can come from widespread sources, like fertiliser spread on farmland or leaking sewers. It is a particular problem in the south, east and midlands of England. Other micro Cryptosporidium Pesticides Nitrate Number of sources 60 50 40 • Sixty per cent of groundwater bodies in England and 11 per cent in Wales are at risk of failing Water Framework Directive objectives because of high nitrate concentrations.14 30 20 10 1975 1980 1985 1990 1995 2000 2005 UKWIR 14 • More than two thirds of the nitrate in groundwater comes from past and present agriculture, mostly from chemical fertilisers and organic materials. Organic materials, such as manure or treated sewage sludge, can be a valuable source of nutrients and organic matter to soils. If too much is applied, or is applied in the wrong place or at the wrong time, it can get into and harm groundwater. It is estimated that over 10 million tonnes per year of organic material is spread on the land in the UK. More than 90 per cent of this is animal manure, the rest is treated sewage sludge, green waste compost, paper sludge and organic industrial wastes. • Other major sources of nitrate are leaking sewers, septic tanks, water mains and atmospheric deposition. Atmospheric deposition of nitrogen makes a significant contribution to nitrate inputs to groundwater. A study in the Midlands concluded that around 15 per cent of the nitrogen leached from soils came from the atmosphere.19 Sources of atmospheric deposition of nitrate include transport, power generation and farm animals. Figure 10 Groundwater sources closed due to pollution Salinity Misc point source Hydrocarbons and solvents Iron/manganese • In 2004 almost 15 per cent of monitoring sites in England (none in Wales) had an average nitrate concentration that exceeded 50 mg/l, the upper limit for nitrate in drinking water.8 To put the problem in context, groundwater naturally contains only a few mg/l of nitrate. Water with high nitrate levels has to be treated or diluted with cleaner water to reduce concentrations. Environment Agency The state of groundwater in England and Wales under threat Pollution that comes from many small sources (diffuse pollution) is the main problem for groundwater. Pesticides Pesticides are used to control weeds and pests, and can cause diffuse pollution. They can get into groundwater if they are able to leach through the soil. Some pesticides break down slowly, so will stay in groundwater for a long time. Others break down quickly, but some produce more toxic chemicals in the process. Some pesticides have been banned from use but we need to make sure that the replacements are better for the environment. • In 2004 we found pesticides in over a quarter of groundwater monitoring sites, and in some cases they exceeded the drinking water limit (Figure 11). There is some evidence that pesticide concentrations in groundwater are declining in some areas.20 This improvement is likely to be the result of a shift to pesticides that are used at lower application rates, and more controlled use and disposal in response to tighter legislation. • Atrazine is a weed killer used mainly to protect maize crops and in the past to maintain roads and Figure 11 Pesticides in groundwater 2004 Pesticides > 1µg/l Pesticides > level of detection Atrazine Simazine Atrazine desethyl* Propazine Atrazine desisopropyl* Trietazine HCH delta Bentazone Metazachlor Dieldrin Pirimicarb Terbutryn 0 10 20 Percentage of sites 30 railways. It has been a major problem, but since the non-agricultural uses were banned in 1993, concentrations in groundwater have gradually declined. A complete ban on all use of atrazine (and simazine, another pesticide) will be phased in between 2005 and 2007. Banned pesticides can remain a problem for many years after they were last used. Solvents, hydrocarbons, and fuel additives Fuel, fuel additives and solvents can contaminate groundwater under cities and industrial areas. Some of these chemicals are quite new, so we do not know how much of a problem they will be. • Chlorinated solvents are widely used as degreasers in the metal, engineering, electronics and leather industries. They are denser than water, they degrade slowly and are toxic at very low levels so small amounts can pollute large volumes of groundwater. There is widespread contamination in the aquifers below our industrial cities. • Groundwater can be contaminated by hydrocarbons (such as oils and fuels) from installations such as petrol stations that are not properly installed or maintained. Hydrocarbons can disperse in water and be transported over long distances. MTBE (Methyl Tertiary Butyl Ether) is often added to petrol to enhance engine performance. MTBE is highly soluble and can move through groundwater much more easily than other components of petroleum. Fuel containing MTBE can enter groundwater through accidental spillage or from leaking underground storage, and it can create odour and taste problems in drinking water. Related substances like ETBE (Ethyl Tertiary Butyl Ether) could start to have wide spread use in petroleum replacement biofuels, with similar risks to MTBE. *Degradation products of atrazine Environment Agency Environment Agency The state of groundwater in England and Wales 15 underground Sometimes harmful microbes can get into groundwater from sewage sludge spread on farmland and leaking sewers or septic tanks. Microbes Microbes like bacteria and viruses are often filtered out of water before they reach groundwater by the overlying soils and rocks. Sometimes harmful microbes can get into groundwater from sewage sludge spread on farmland and leaking sewers or septic tanks. • Over the last five years 42 groundwater sources have been identified to be at high risk from the micro-organism Cryptosporidium, and shut down. Nineteen Cryptosporidium treatment schemes were installed over this period and there are plans for 54 more.18 Water companies routinely sample sites where a significant risk of Cryptosporidium has been identified. This costs around £20,000 per site per year. • Problems in groundwater are likely to be localised and we do not routinely monitor for microbes. Studies have found microbes from man-made sources in aquifers below Birmingham and Nottingham at depths of up to 90 metres.21 Salinity There is a natural boundary where fresh and saline groundwater meet in coastal aquifers. When fresh water is pumped out, this boundary moves and seawater is sucked into the aquifer. This can also happen inland, with groundwater abstraction causing saltwater to be drawn up from deep water aquifers. If too much water is taken from a coastal aquifer, it can eventually become too salty to drink. • Since the mid 1970s 11 groundwater sources belonging to water companies have been shut down due to saline intrusion problems and 50 sites belonging to industry and private abstractors.18 • Salt can get into groundwater from other sources, such as salt spread on roads in winter washing into the ground. This has increased over the past decade and shows the impact that human activities are having on groundwater (Figure 12). 16 Environment Agency The state of groundwater in England and Wales • High levels of abstraction for public water supply have caused saltwater intrusion in the chalk aquifer near Brighton. The problem is being successfully managed by using boreholes in different places at different times of year. In winter, more fresh groundwater is flowing towards the sea, so boreholes near the coast can be used and inland boreholes are rested. In summer, saline intrusion is more likely so the inland boreholes are used instead. • Boreholes around the Mersey Estuary have also suffered from saline intrusion. In the past industry close to the estuary abstracted large volumes of water from the sandstone aquifer underlying the Mersey basin, causing saltwater intrusion. It has become less of an issue since the 1970s, when the problem was recognised and strategies were put in place to control the problem, but it still needs careful management. Natural contaminants Natural contaminants can also occur in groundwater. As water flows through the ground the chemistry changes as elements are released from the rocks. In certain aquifers, iron, manganese, arsenic, fluoride and radon are found at relatively high concentrations. Dissolved radon can be released as a gas and accumulate in confined spaces such as houses. Things we are looking out for There are hundreds of chemicals that could get into groundwater. We look for substances that are not a problem now, but that we think might be in the future. • Pharmaceuticals have been found in groundwater in other countries, usually near landfills that have been used to dispose of hospital or pharmaceutical industry waste.22 under threat • Caffeine is a natural stimulant found in coffee and tea. It has been detected at low concentrations in groundwater across England and Wales. It is thought to have reached groundwater via septic tanks and leaking sewers. Although the caffeine in groundwater does not present any risk it does highlight how vulnerable groundwater is from human activities. • Triclosan is an antibacterial agent that is added to a large range of consumer products. Sixty to 90 tonnes are used every year in the UK. Its widespread use may be a risk to the environment and human health.23 It is present in small quantities in sewage effluent and sewage sludge, and it has been found at a small number of groundwater monitoring sites. There is a risk that triclosan could affect bacteria that help break down some pollutants. Percentage of sites above concentration threshold 56 52 48 1995 1997 1999 2001 Urbanisation Nearly everybody lives, works and travels in towns and cities. Inadequate or faulty drainage systems mean that groundwater can be polluted by dirty water running off roads and other surfaces, badly connected drains, leaking sewers and spilled chemicals, oil and fuel. • Poor water and sewerage systems often make groundwater quality worse in urban areas. For example, in Nottingham around half of the nitrate loading in groundwater comes from the leaking water mains and sewerage system.24 Groundwater can also infiltrate sewers and overwhelm sewage treatment works. • About 24 per cent of groundwater bodies in England and 7 per cent in Wales are at risk of failing Water Framework Directive objectives because of diffuse urban pollution.14 Mining Metal and coal mines can have a huge impact on groundwater systems. While mining is happening groundwater is usually pumped out in large quantities. When mining and pumping stops the rising groundwater can become contaminated. The mine structures can also change groundwater flow permanently. Figure 12 Chloride in groundwater 1993 to 2004 1993 Polluted places 2003 • The main pollutants from mining are iron, zinc, lead, cadmium and acidic water. These substances can leach down into groundwater from spoil heaps, or can contaminate the upper part of the aquifer as groundwater levels (previously artificially lowered by pumping) begin to rise. The impacts can remain for hundreds of years. Environment Agency Environment Agency The state of groundwater in England and Wales 17 underground • In 1994, it was estimated that abandoned coal mines had polluted more than 400 km of rivers.25 This was primarily due to the rise in contaminated groundwater after pumping stopped, known as rebound. Treatment schemes operated by the Coal Authority clean up more than 170 thousand m3 per day of polluted groundwater. This has cost more than £30 million since 1997. • Mines and quarries can physically disrupt the flow of groundwater. Removal of the overlying protective layers of rock and soil, or bypassing them with tunnels or engineering works, can provide rapid pathways for pollutants to groundwater. Or the aquifer itself can be removed. For example, in the Mendip Hills the important limestone aquifer has been extensively quarried. • Metal mining has caused high concentrations of heavy metal pollutants in groundwater across Wales, the south west and northern England. When the polluted groundwater reaches rivers it can severely impact on fish and other aquatic life. For example, 20 per cent (108 km) of all river quality objective failures in Wales have been attributed to mining pollution. In Cornwall, we treat more than 17,000 m3 per day of polluted groundwater every day at the abandoned Wheal Jane tin mine. This minewater would otherwise pollute the River Fal with heavy metals. • Minewater rebound threatens several drinking water supply aquifers. In County Durham, the Coal Authority has to pump out over 5,000 m3 of groundwater each day to prevent minewater rising up and polluting the source of Sunderland’s drinking water. In some areas recovering groundwater levels can cause surface flooding. • Fifteen per cent of groundwater bodies in Wales and six per cent in England are at risk of failing to meet Water Framework Directive objectives because of pollution from mining.14 Industry can leave behind land contaminated by chemicals or radiological material that can leach through soils and rock and pollute groundwater. 18 Environment Agency The state of groundwater in England and Wales under threat Landfills Many different types of waste go to landfill, so there are lots of potential pollutants. They are only a problem if the landfill they are in has not been lined properly, or is badly maintained. • Most modern landfills are highly regulated and operated to high standards, posing little risk of pollution to groundwater. Older and closed landfills might cause localised contamination issues. • All landfill sites are likely to have been sent exempt radioactive waste, for example smoke detectors and exit signs.27 As a result low levels of radioactivity are commonly found in landfill leachates, but it doesn’t often get into groundwater and any problems are minor and local. Contaminated land Industry can leave behind land contaminated by chemicals or radiological material that can leach through soils and rock and pollute groundwater. • The best estimates are that over 300,000 sites have been used for activities that could cause contamination.27 Examples of these sites are former gas works and petrol filling stations. • Of these around 33,000 sites require action, and about 21,000 sites have received some action to remove contamination or prevent harm from contamination. Many of these sites could cause groundwater pollution so work is being carried out to prevent this.27 Sustainable Urban Drainage Systems (SUDS) Sustainable Urban Drainage Systems are an approach to drainage management in towns and cities that try to mimic natural drainage patterns as much as possible. These drainage systems can intercept pollutants and reduce flood risk, and we think that they should become a common feature of urban design. Surfaces in urban areas are usually impermeable to water, so rates of infiltration (and therefore recharge of underlying aquifers) are limited. SUDS can help return water to groundwater by slowing down rainfall runoff in soakaways, permeable surfaces, ponds and wetlands. This could make groundwater more vulnerable to pollution if the scheme is not designed and maintained properly. Environment Agency The state of groundwater in England and Wales 19 underground How we look after groundwater We set out our position on groundwater in our publication Groundwater protection: policy and practice. The document presents the legal and technical framework in which we work, and provides detailed and informed advice on many groundwater policy issues. There is a lot we already do to protect groundwater resources. The EU Water Framework Directive is a new piece of legislation. Its aim is for all waterbodies (river, lakes, estuaries, coastal waters and groundwater) to achieve ‘good status’ by 2015. The directive is likely to be particularly beneficial to groundwater, as rivers, lakes and groundwater are considered in an integrated way, rather than in isolation. This is particularly useful when trying to address the issue of diffuse pollution, which is a significant pressure on groundwater that has proved difficult to deal with. We routinely monitor groundwater quality and level to help us understand the condition of groundwater, and ideally identify any problems before they become too difficult to deal with. There are 7,300 groundwater level monitoring sites (180 of these are in Wales), and the number of quality monitoring sites has doubled to 3,500 since 1999 (280 of these are in Wales). We also work with and advise others, such as development planners and industrial groups, to identify groundwater issues. 20 Environment Agency The state of groundwater in England and Wales It takes a long time to clean up groundwater, so people who manage groundwater need to assess the cost and difficulty of tackling pollution over equally long timescales. There are no quick fixes for groundwater, but preventing harm in the short term will protect the resource for years to come. Groundwater regulation As part of our regulatory role, we issue permits for abstractions and for discharges to water and land and have enforcement powers. Where possible, our decisions and actions are risk based. We concentrate on activities and operators that are most likely to harm groundwater. We can refuse licences if, for example, we believe they will cause erosion of someone else’s existing abstraction rights or harm an aquifer or a protected wetland. The Water Framework Directive extends our role. We will be able to refuse to license activities that are likely to harm river, lake, estuary, coastal or wetland environments, or are likely to cause saline intrusion or other contamination of clean groundwater. Land use If people want to keep using groundwater in the future, it is vital that the sources are protected. The risk of pollution generally increases when a polluting activity or release is close to the groundwater source, so sources used for public drinking water supply need protection zones. We have published detailed maps of nearly 2000 protection zones. Nitrate Vulnerable Zones (NVZs) have been created to reduce nitrates entering groundwater by limiting the amount of nitrogen applied to farmland. The rules that govern the application of manure and fertilisers to land in these areas have been in place since the mid-1990s and are due to be revised soon. under threat As yet, there is no evidence that nitrate levels in groundwater are declining, but we expect the changes to take time. There are a number of recent measures that will help to deal with diffuse pollution from agriculture. These include the Catchment Sensitive Farming scheme, the Voluntary Initiative for controlling pesticides, and reform of the European Union’s Common Agricultural Policy. To deal successfully with nitrate from agriculture, more fundamental land use changes might be needed. Radical measures like converting some arable land to forestry have been shown to work in Denmark and Germany. Economics In the future economic instruments may need to be used more. These are financial incentives and sanctions that operate using market forces, to encourage beneficial behaviour. We are carrying out research to try to place an economic value on groundwater. As water resources become scarcer, either from climate change or increased use by society, then the value of groundwater could increase. This could encourage trading in groundwater and people could manage groundwater better, knowing that the costs involved to save water, or improve quality, could be offset by selling it at a higher price. Groundwater would become another asset to be traded, bringing a greater awareness of its value. There are no quick fixes for groundwater, but preventing harm in the short term will protect the resource for years to come. Environment Agency The state of groundwater in England and Wales 21 underground Groundwater in the future Most people don’t think about groundwater very much. But if we look after it carefully then it will keep supplying clean water for many generations to come. Some contamination is inevitable and we must learn to deal with it. Solutions need to be a realistic mix that meet the demands of society and the economy as well as the environment. We think We must We support 22 that with the possibility of less water available in the future demand must be brought under control and eventually reduced. If groundwater pollution continues then there will be even less water available and water resources will be put under even more stress. protect vulnerable aquifers from potential sources of pollution. Prevention is better than cure; and that requires continued investment. We need to ensure that we have the right regulatory tools to protect groundwater in the future. the development of Defra and Welsh Assembly Government’s water, soil and land contamination strategies. We are encouraged by the initiatives to protect groundwater developed by some water companies, farmers and others. Environment Agency The state of groundwater in England and Wales under threat 1 Defra, 2005. e-digest statistics about: Inland Water Quality and Use (2003 data). Available at www.defra.gov.uk/environment/statistics/inlwater/iwab straction.htm 2 Food Standards Agency, 2006. Natural Mineral Water, Spring Water and Bottled Drinking Water (England) Regulations 2006. Annex E: Partial Regulatory Impact Assessment. Available at www.food.gov.uk/multimedia/pdfs/mineralwater2006pr ias.pdf. Per capita consumption figure calculated using estimate of UK population from the Office of National Statistics available at www.statistics.gov.uk 16 Defra and Jacobs, 2004. Strategy for Flood and Coastal Erosion risk management: Groundwater Flooding Scoping Study (LDS 23) Final Report, vol 1 of 2. 17 Based on average water use of 358 litres per household per day. www.ofwat.gov.uk/aptrix/ofwat/publish.nsf/Content/wa terandyoumarch2001 18 United Kingdom Water Industry Research, 2004. Implications of changing groundwater quality for water resources and the UK water industry, Phase III: Financial and water resources impact. UKWIR, London, 70pp. 19 3 Food Standards Agency, 2005. Mineral Waters. Available at www.food.gov.uk/foodindustry/mineralwaters Environment Agency, 2003. Investigation of the atmospheric deposition of nitrogen into groundwater. Environment Agency, Technical Report P2-079/TR. Available at www.environment-agency.gov.uk 4 Downing R.A., 1998. Groundwater our hidden asset. UK Groundwater Forum, Wallingford, 60pp. 5 Environment Agency, 2006. Groundwater protection: policy and practice. 6 Environment Agency, 2006. Water demand and availability. Environmental indicator available at www.environment-agency.gov.uk/yourenv 7 Environment Agency, 2001. Water Resources for the Future: a strategy for England and Wales. Environment Agency, Bristol, 96pp. 8 Environment Agency data (2003) 20 Worrall, F., Besien, T., and Garthwaite, D., 2006 (in prep). Pesticides in the groundwater of Southern England 1992–2000. J. Hydrol. 21 Environment Agency, 2001. Distribution of microbiological contaminants in Triassic Sandstone urban aquifers. Environment Agency, Technical Report SP2-255/TR. Available at www.environmentagency.gov.uk 22 Environment Agency, 2000. Review of human pharmaceuticals in the environment. Environment Agency, STRP390. Available at www.environmentagency.gov.uk 9 Environment Agency data (2003), ‘Wales’ refers to political Wales. 23 Environment Agency, Triclosan briefing note. Available at www.environment-agency.gov.uk 10 Ofwat, 2005. Security of supply, leakage and efficient use of water 2004–05 report. Ofwat, Birmingham. Available at www.ofwat.gov.uk 24 Wakida, F. T. and Lerner, D. N., 2005. Nonagricultural sources of groundwater nitrate: a review and case study. Water Research, 39, 3–16. 11 National Audit Office, 2005. Environment Agency; Efficiency in Water management. NAO, report HC73, 2005–2006. Available at www.nao.org.uk 12 Environment Agency data (2003) 13 Environment Agency, 2001. Water Resources for the future, a strategy for Wales. Environment Agency Wales, Cardiff, 184pp. 14 From Water Framework Directive river basin characterisation. The figure refers to the number of groundwater bodies at risk or probably at risk of failing to achieve their environmental objectives by 2015. 25 National Rivers Authority, 1994. Abandoned mines and the water environment. NRA Water Quality Series No. 14. HMSO, London. 26 Environment Agency, 2002. Metal Mines Strategy for Wales. Available at www.environment-agency.gov.uk 27 Environment Agency, 2005. Indicators for land contamination. Environment Agency, Science Report SC030039/SR. Available at www.environmentagency.gov.uk 15 ODPM, 2005. Creating sustainable communities – Delivering the Thames Gateway. Available at www.communities.gov.uk Environment Agency The state of groundwater in England and Wales 23 Would you like to find out more about us, or about your environment? Then call us on 08708 506 506 (Mon–Fri 8–6) email [email protected] or visit our website www.environment-agency.gov.uk incident hotline 0800 80 70 60 (24hrs) floodline 0845 988 1188 Environment first: This publication is printed on paper made from 100 per cent previously used waste. By-products from making the pulp and paper are used for composting and fertiliser, for making cement and for generating energy. GEHO0906BLDB-E-P
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