P7 Flashcards
Introducing the issue - an unequal water world
- Improving access to water and sanitation underpinned many of the UN’s Millennium Development Goals (MDGs).
- The problem is that when a final assessment of progress was made in 2015, some fifteen per cent of the world’s people still did not have reliable access to safe water, and around 25 per cent still lacked clean sanitation.
- Figure 3.1 re-emphasises how, of the volume of water in the global water pot, only 2.5 per cent is available as fresh water for humans to use, and only around one per cent is available as easily accessible surface water.
- In theory, this should not be a problem as, according to the UN, our basic needs can be met by 1000 cubic metres per year.
- In 2010 it was estimated that nearly 60 per cent of this accessible fresh water - contained in rivers, lakes and groundwater aquifers - was being used, leaving some 40 per cent untapped so, in theory, there is more than enough to go round. So, what’s the problem?
- As you will see, the combination of rising demand and the diminishing availability of finite supplies could create a ‘perfect storm’ of resource shortages in combination with food and energy, for which water is a vital part of production.
- The phrase peak water’ is being used increasingly to describe the state of growing constraints on quantity and quality of accessible water.
- The fundamental problem lies with an unequal water world, as opposed to the generally satisfactory global situation.
- There are three facets to this state of affairs: physical distribution, the gap between rising demand and diminishing supplies, and the water availability gap.
Players:
Individuals, groups or organisations with an involvement or interest in a particular issue.
Physical distribution
- In terms of physical distribution there is a mismatch between where the water supplies are and where the demand is.
- Water supplies are spread very unevenly across the world: 60 per cent of the world’s supplies are contained in just ten countries.
- both physical factors, such as location of precipitation belts/temperature, and level of development are important.
- In conclusion, 66 per cent of the world’s population live in areas receiving only 25 per cent of the world’s annual rainfall.
- Clearly, there are areas of supply shortage such as most of the Middle East where there are potential sources of conflict over shared basin usage/dams and pollution.
Gap between rising demand and diminishing supplies
There is a global gap between rising demand (Table 3.2) and diminishing supplies.
Table 3.2 Projections for increasing global water usage
Year
1900
1950
2000
2025
Total annual water withdrawal (km3)
579
1,382
3,973
5,235 (projected)
Rising demand
This is driven by a number of factors:
- Population growth, possibly fuelled by an additional 3 billion people by 2030.
- Rising standards of living as countries such as China adopt meat-rich diets, which lead to higher consumption of water for agricultural purposes.
- increased domestic use - for drinking, bathing and cleaning - as people become more affluent.
- Equally, the demand for consumer goods such as white goods and electronics encourages more use of water in manufacturing (i.e. embedded water).
- The combination of rising numbers and changing lifestyles, often in rapidly urbanising environments with high costs of providing water infrastructure, puts pressure on water supplies.
- Economic growth increases demand for water in all economic sectors (agriculture, industry, energy and services). The mining of unconventional energy sources, for example fracking, puts huge demands on water.
- Irrigated farming places a particular strain on resources. Countries such as Israel or areas such as the Murray-Darling Basin in Australia (page
27) are experiencing increasing droughts as a result. The countries bordering the Aral Sea - Turkmenistan, Kazakhstan and Uzbekistan - have the highest water use per capita in the world, with around 99 per cent being used for irrigated crops.
This overuse led to the environmental degradation of the ecosystems surrounding the Aral Sea (see page 56).
Fracking:
Hydraulic fracking or oil/gas well stimulation is a technique in which rock is fractured by a pressurised liquid.
groundwater aquifers abstaction
- The main reason is for irrigation, which is a voracious consumer of water.
- Comparatively cheap pumping technology, minimal legislation to regulate its use and threats from climate change-induced drought have combined to put pressure on supplies, leading to a falling water table as the groundwater supplies are being extracted faster than they can be replenished.
- Excessive withdrawals lead to land subsidence (as in Mexico City) and intrusion of salt water in coastal districts (as in coastal North Africa).
- The conclusion is that groundwater can no longer be regarded as an unlimited supplement to surface water supplies, which are themselves being diminished by overuse.
Water availability gap
The underlying concept is that of a water availability gap between the ‘have-nots’, largely in developing nations (for example in sub-Saharan Africa), and the ‘haves’, largely in developed nations. There is an imbalance of usage, with richer countries using up to ten times more water per head: they have a water profile that includes large percentages of embedded water as well as direct water use. Embedded water is known as virtual water, which comes embedded in all the farm products, food and manufactured goods that are imported.
Figure 3.4 (page 48) compares the water profiles of contrasting countries. Many countries will experience water stress (under 1700 m3 per person per year), especially in some parts of western Asia, such as Pakistan, South Africa and Ethiopia and, in recent years, California in the USA. With the onset of climate change and the associated desertification of ecosystems, by 2050 some 4 billion people could be experiencing water stress.
By 2025, it is estimated that nearly half of the world’s population will be water vulnerable (under 2500 m3 per person per year). A state of vulnerability means that there is insufficient water and risks to supplies, especially when unusually hot or dry conditions result from short-term climate change. The list of vulnerable countries includes: Spain, Belgium, the UK, Bulgaria and Poland in Europe, and countries such as India, Ghana, Nigeria and most parts of China.
If there is around 3000 m3 per person available, supplies are declared to be sufficient. This includes virtually the whole of the Americas (if complete countries are considered), Russia, Scandinavia and many countries in equatorial regions. Australia is a surprising example of a country which overall has sufficient water on a per capita basis but, with many drought-prone areas, has regional problems (for example in the Murray-Darling Basin, see page 27).
Virtual water:
The hidden flow of water when food or other commodities are traded.
Causes of water insecurity
Physical factors determining the supply of water
At a macro scale, climate determines the global distribution of water supply by means of annual and seasonal distribution of precipitation (rain and snow). Precipitation varies globally as a result of atmospheric pressure systems, with the low-pressure zone of mid-latitudes and equatorial regions having the highest totals and, therefore, being generally water secure. Also important is the seasonal distribution of rainfall, its reliability and its availability for use as water supply. As the study of the Sahel shows (page 26),
lower annual totals of rainfall often have greater variation and therefore poorer reliability of supply. Short-term climate change (the ENSO and climate warming) are exacerbating the water security situation.
On a more regional scale, topography and distance from the sea have significant impacts. High relief promotes increased precipitation and rapid run-off, but may also provide greater opportunities for surface water storage in natural lakes and artificial reservoirs, especially where it is combined with impermeable geology. Snowfall and glaciers can be extremely important locally, as in the Bolivian Andes where climate warming has led to widespread melting, diminishing the cryosphere storage and threatening water supplies for La Paz-El Alto. The same issue is also affecting Nepal’s water supply.
The world’s major river systems store large quantities of water and transfer it across continents. The Amazon, for example, has an average annual discharge of 175,000 cubic metres per second from its catchment areas of 6,915,000 square kilometres shared by Brazil and six other South American countries. Recent severe droughts in 2005 and 2010, with a dry period in between (a 1-in-100-years event), covered an area twice the size of California and had a huge impact on Brazil’s water supply. Flows in the main river were at an all-time low, with several tributaries completely dry, along with record sea temperatures off the north-eastern coast of Brazil. Many experts argued that deforestation was a contributor to the drought affecting the Amazon’s hydrological pump.
Geology controls the distribution of aquifers (water-bearing rocks) that provide the groundwater storage.
Permeable chalk and porous sandstones can store vast quantities of water underground, which is valuable as it is not subject to evaporation loss. The water supply comes from springs and can also be accessed by wells, giving an even supply throughout the year, despite the uneven distribution and variability of rainfall - provided they are not overused by demand rising at a faster rate than they can be replenished by natural recharge.
Currently, there is a crisis caused by over-digging of tube wells, leading to massive abstraction and a falling water table, combined in many places with a less predictable pattern of rains, for example in the monsoon areas of India and Pakistan.
Figure 3.5 (page 50) shows how these physical factors can combine to affect the water supply of India, a country that is vulnerable to water insecurity, especially in the Indo-Gangetic Plains, the backbone of the water intensive Green Revolution.
Defining water security levels
There are a number of measures used to define water shortages: if there is less than 1000 m3 per capita of available water, a state of water scarcity occurs. There are two types:
Physical scarcity
occurs when more than 75 per cent of a countrys or a region’s blue water flows are being used - this currently applies to around 25 per cent of the world’s population (water-scarce countries are clustered in the Middle East and North Africa, and regionally in some larger countries, such as North East China and parts of the Great Plains of the USA). Some Middle Eastern countries, such as the desert kingdom of Saudi Arabia, are using up to four per cent more water than their supplies and therefore have to rely on desalination
Economic scarcity
occurs when the development of blue water sources is limited by lack of capital, technology and good governance. Around 1 billion people currently have satisfactory physical availability but can only access some 25 per cent of the water supplies because of the high levels of poverty prevalent in these developing countries. Solutions may be reliant on privatisation (research Tanzania or Ghana in Africa, or Bolivia in South America).
By 2050, 1.5 billion people will be experiencing water scarcity, especially in Middle East and parts of sub-Saharan Africa.
Human factors influencing the security of water supplies
Human activities can lead both to diminishing supply and rising demands. Humans can also impact on both the quantity of available water and its quality.
Quality
Human actions can pollute both surface water and groundwater supplies, so diminishing the quality of both sources and having a knock-on effect on the security of supplies. Pollution is widespread throughout the world, although its impact is felt especially in developing countries (1 billion people are without safe water and 2.3 billion lack adequate sanitation). The difference of impact is related to the ability of developed countries to do something about it, either by prevention or remediation of supplies.
The pollution of surface water in rivers, streams and lakes is a cause for concern, for example in China where 300 million people use contaminated water daily and
190 million suffer from water-related illnesses annually.
In China, one-third of all rivers, 75 per cent of major lakes and 25 per cent of coastal zones are currently classified as highly polluted. It has been reported that longer-term 2 million Chinese people may suffer from water-related diseases, including those in the
‘cancer cluster’ villages in Guandong province where liver and digestive cancers were responsible for 80 per cent of recent deaths (heavy metal toxins from the Dabaoshan mine had washed into the Hengshi River).
Contaminants usually enter waterways via run-off or sewage. However, groundwater contamination is potentially even more serious if important aquifers are irreversibly damaged by the high levels of toxicity. Nearly 20 per cent of all the tube wells sunk in Bangladesh, often concentrated in particular villages, were found to be unsafe because of a high concentration of arsenic. This led to major health problems, with correlated social impacts, as the victims developed arsenicosis with skin lesions. Worldwide, 137 million people in over 70 countries have some signs of arsenic poisoning from drinking water.
Some common types of pollution include:
• Untreated sewage disposal, especially in developing countries where sanitation is poorer. This causes water-borne diseases such as typhoid, cholera and hepatitis. As many people are forced to use unsafe water, it is estimated by WHO that, by 2020, 135 million people could die unnecessarily from these water-borne diseases. In India, only 20 per cent of sewage is treated before being discharged in rivers.
• Chemical fertilisers, used increasingly by farmers (part of the Green Revolution) contaminate groundwater as well as rivers, causing eutrophication in lakes and rivers. This leads to hypoxia and the formation of dead zones in coastal waters. Many of the pesticides used are banned in developed countries because of the health hazards.
• Industrial waste is dumped into rivers and, subsequently, oceans. Heavy metals and chemical waste are particularly toxic. The Ganges is a useful example to study; many toxic industries, such as tanneries, discharge their waste directly into the holy river.
• As over 60 per cent of the world’s major rivers are impeded by large dams, this has a major impact on sediment movement, which can impact on river ecology.