Fresh water is naturally occurring water on the Earth's surface in ice sheets, ice caps, glaciers, icebergs, bogs, ponds, lakes, rivers and streams, and underground as groundwater in aquifers and underground streams. Fresh water is generally characterized by having low concentrations of dissolved salts and other total dissolved solids. The term specifically excludes seawater and brackish water although it does include mineral-rich waters such as chalybeate springs. The term "sweet water" has been used to describe fresh water in contrast to salt water.1
Scientifically, freshwater habitats are divided into lentic systems, which are the stillwaters including ponds, lakes, swamps and mires; lotic systems, which are running water; and groundwater which flows in rocks and aquifers. There is, in addition, a zone which bridges between groundwater and lotic systems, which is the hyporheic zone, which underlies many larger rivers and can contain substantially more water than is seen in the open channel. It may also be in direct contact with the underlying underground water.
The source of almost all fresh water is precipitation from the atmosphere, in the form of mist, rain and snow. Fresh water falling as mist, rain or snow contains materials dissolved from the atmosphere and material from the sea and land over which the rain bearing clouds have traveled. In industrialized areas rain is typically acidic because of dissolved oxides of sulfur and nitrogen formed from burning of fossil fuels in cars, factories, trains and aircraft and from the atmospheric emissions of industry. In some cases this acid rain results in pollution of lakes and rivers.
In coastal areas fresh water may contain significant concentrations of salts derived from the sea if windy conditions have lifted drops of seawater into the rain-bearing clouds. This can give rise to elevated concentrations of sodium, chloride, magnesium and sulfate as well as many other compounds in smaller concentrations.
In desert areas, or areas with impoverished or dusty soils, rain-bearing winds can pick up sand and dust and this can be deposited elsewhere in precipitation and causing the freshwater flow to be measurably contaminated both by insoluble solids but also by the soluble components of those soils. Significant quantities of iron may be transported in this way including the well-documented transfer of iron-rich rainfall falling in Brazil derived from sand-storms in the Sahara in north Africa.
Water is a critical issue for the survival of all living organisms. Some can use salt water but many organisms including the great majority of higher plants and most mammals must have access to fresh water to live. Some terrestrial mammals, especially desert rodents appear to survive without drinking but they do generate water through the metabolism of cereal seeds and they also have mechanisms to conserve water to the maximum degree.
Out of all the water on Earth, salt water in oceans, seas and saline groundwater make up about 97% of it. Only 2.5–2.75% is fresh water, including 1.75–2% frozen in glaciers, ice and snow, 0.7–0.8% as fresh groundwater and soil moisture, and less than 0.01% of it as surface water in lakes, swamps and rivers.34 Freshwater lakes contain about 87% of this fresh surface water, including 29% in the African Great Lakes, 20% in Lake Baikal in Russia, 21% in the North American Great Lakes, and 14% in other lakes. Swamps have most of the balance with only a small amount in rivers, most notably the Amazon River. The atmosphere contains 0.04% water.5 In areas with no fresh water on the ground surface, fresh water derived from precipitation may, because of its lower density, overlie saline ground water in lenses or layers. Most of the world's fresh water is frozen in ice sheets. Many areas suffer from lack of distribution of fresh water, such as deserts.
|Water salinity based on dissolved salts|
|Fresh water||Brackish water||Saline water||Brine|
|< 0.05%||0.05% – 3%||3% – 5%||> 5%|
Fresh water creates a hypotonic environment for aquatic organisms. This is problematic for some organisms with pervious skins or with gill membranes, whose cell membranes may burst if excess water is not excreted. Some protists accomplish this using contractile vacuoles, while freshwater fish excrete excess water via the kidney.9 Although most aquatic organisms have a limited ability to regulate their osmotic balance and therefore can only live within a narrow range of salinity, diadromous fish have the ability to migrate between fresh water and saline water bodies. During these migrations they undergo changes to adapt to the surroundings of the changed salinities; these processes are hormonally controlled. The eel (Anguilla anguilla) uses the hormone prolactin,10 while in salmon (Salmo salar) the hormone cortisol plays a key role during this process.11
Many sea birds have special glands at the base of the bill through which excess salt is excreted. Similarly the marine iguanas on the Galápagos Islands excrete excess salt through a nasal gland and they sneeze out a very salty excretion.
An important concern for hydrological ecosystems is securing minimum streamflow, especially preserving and restoring instream water allocations.12 Fresh water is an important natural resource necessary for the survival of all ecosystems. The use of water by humans for activities such as irrigation and industrial applications can have adverse impacts on down-stream ecosystems. Chemical contamination of fresh water can also seriously damage eco-systems.
Pollution from human activity, including oil spills, also presents a problem for freshwater resources. The largest petroleum spill that has ever occurred in fresh water was caused by a Royal Dutch Shell tank ship in Magdalena, Argentina, on January 15, 1999, polluting the environment, drinkable water, plants and animals.13
Fresh and unpolluted water accounts for 0.003% of total water available globally.14
Changing landscape for the use of agriculture has a great effect on the flow of fresh water. Changes in landscape by the removal of trees and soils changes the flow of fresh water in the local environment and also affects the cycle of fresh water. As a result more fresh water is stored in the soil which benefits agriculture. However, since agriculture is the human activity that consumes the most fresh water,15 this can put a severe strain on local freshwater resources resulting in the destruction of local ecosystems. In Australia, over-abstraction of fresh water for intensive irrigation activities has caused 33% of the land area to be at risk of salination.15 With regards to agriculture, the World Bank targets food production and water management as an increasingly global issue that will foster debate.16
Fresh water is a renewable and variable, but finite natural resource. Fresh water can only be replenished through the process of the water cycle, in which water from seas, lakes, forests, land, rivers, and reservoirs evaporates, forms clouds, and returns as precipitation. Locally however, if more fresh water is consumed through human activities than is naturally restored, this may result in reduced fresh water availability from surface and underground sources and can cause serious damage to surrounding and associated environments.
Fresh water withdrawal is the quantity of water removed from available sources for use in any purpose, excluding evaporation losses. Water drawn off is not necessarily entirely consumed and some portion may be returned for further use downstream.
There are many causes of the apparent decreasecitation needed in our fresh water supply. Principal amongst these is the increase in population through increasing life expectancy, the increase in per capita water use and the desire of many people to live in warm climates that have naturally low levels of fresh water resources.citation needed Climate change is also likely to change the availability and distribution of fresh water across the planet:
"If global warming continues to melt glaciers in the polar regions, as expected, the supply of fresh water may actually decrease. First, fresh water from the melting glaciers will mingle with salt water in the oceans and become too salty to drink. Second, the increased ocean volume will cause sea levels to rise, contaminating freshwater sources along coastal regions with seawater”.17
The World Bank adds that the response by freshwater ecosystems to a changing climate can be described in terms of three interrelated components: water quality, water quantity or volume, and water timing. A change in one often leads to shifts in the others as well.18 Water pollution and subsequent eutrophication also reduces the availability of fresh water.19
Also, there is an uneven distribution of fresh water. While some countries have an abundant supply of fresh water, others do not have as much. For example, Canada has 20% of the world's fresh water supply, while India has only 10% of the world's fresh water supply; what more India's population is more than 30 times larger than that of Canada. A reason for the uneven distribution of fresh water supply may be the differences in climate. For example, in some countries in Africa, the frequent lack of rain has led to insufficient water supply for irrigation. This has affected agriculture and has led to a shortage of food for the people.20
Many areas of the world are already experiencing stress on water availability. Due to the accelerated pace of population growth and an increase in the amount of water a single person uses, it is expected that this situation will continue to get worse. A shortage of water in the future would be detrimental to the human population as it would affect everything from sanitation, to overall health and the production of grain.21
With one in eight people in the world not having access to safe water22 it is important to use this resource in a prudent manner. Making the best use of water on a local basis probably provides the best solution. Local communities need to plan their use of fresh water and should be made aware of how certain crops and animals use water.
As a guide the following tables provide some indicators.
Table 1 Recommended basic water requirements for human needs.
|Activity||Minimum litres per day||Range litres per day|
|Cooking and Kitchen||10||10–50|
Table 2. Water Requirements of different classes of livestock
|Animal||Average Gallons per day||Range gallons per day||Average in litres|
Table 3 Approximate values of seasonal crop water needs.
|Crop||Crop water needs mm / total growing period|
Canada has approximately 7% of the world’s renewable fresh water.26 Canadians access their water from ground water, lakes and streams; it is then cleaned and purified in water treatment plants. More than half of Canada’s water drains into the Hudson Bay and the Arctic Ocean, but 85% of Canada’s population lives along the southern border,27 not near this free flowing northern draining water. Water in Canada may be abundant, but it is stressed and heavily used.28
The United States uses much more water per capita than developing countries. For example, the average American’s daily shower uses more water than a person in a developing country would use for an entire day.29 Las Vegas, a city that uses an extreme amount of water to support spectacular lush greenery and golf courses, as well as huge fountains and swimming pools gets 90% of its water from Lake Mead,30 which is now at a record all time low.
In developing countries, 780 million people lack access to clean water.31 Half of the population of the developing world suffers from at least one disease caused by insufficient water supply and sanitation.32
- African Great Lakes
- Aral Sea
- Freshwater ecology
- Great Lakes
- Lake Baikal
- List of countries by freshwater withdrawal
- List of countries by total renewable water resources
- Water crisis
- Water cycle
- Properties of water
- Water resources
- Drinking water
- Water well
- "sweet-water, n.". Oxford English Dictionary. Second edition (Online version November 2010. ed.). 1989. Retrieved 16 February 2011. Unknown parameter
- USGS – Earth's water distribution. Ga.water.usgs.gov (2012-12-11). Retrieved on 2012-12-29.
- Where is Earth's water?, United States Geological Survey.
- Physicalgeography.net. Physicalgeography.net. Retrieved on 2012-12-29.
- Gleick, Peter; et al. (1996). Stephen H. Schneider, ed. Encyclopedia of Climate and Weather. Oxford University Press.
- "Groundwater Glossary". 2006-03-27. Retrieved 2006-05-14.
- "Freshwater". Glossary of Meteorology. American Meteorological Society. June 2000. Retrieved 2009-11-27.
- "Freshwater". Fishkeeping glossary. Practical Fishkeeping. Retrieved 2009-11-27.dead link
- "Vertebrate Kidneys". 2002-11-03. Retrieved 2006-05-14.
- Kalujnaia, S.; et. al. (2007). "Salinity adaptation and gene profiling analysis in the European eel (Anguilla anguilla) using microarray technology". Gen Comp Endocrinol. (National Center for Biotechnology Information) 152 (2007): 274–80. doi:10.1016/j.ygcen.2006.12.025. PMID 17324422.
- Bisal, G.A.; Specker, J.L. (24 Jan 2006). "Cortisol stimulates hypo-osmoregulatory ability in Atlantic salmon, Salmo salar L". Journal of Fish biology (Wiley) 39 (3): 421–432. doi:10.1111/j.1095-8649.1991.tb04373.x.
- Peter Gleick, Peter; Heather Cooley, David Katz (2006). The world's water, 2006–2007: the biennial report on freshwater resources. Island Press. pp. 29–31. ISBN 1-59726-106-8. Retrieved 2009-09-12.
- Petroleomagdalena.com. Petroleomagdalena.com (1999-01-15). Retrieved on 2012-12-29.
- Nitti, Gianfranco (May 2011). "Water is not an infinite resource and the world is thirsty". The Italian Insider (Rome). p. 8.
- Gordon L., D. M. (2003). "Land cover change and water vapour flows: learning from Australia". Philosophical Transactions of the Royal Society B: Biological Sciences 358 (1440): 1973–1984. doi:10.1098/rstb.2003.1381. JSTOR 3558315.
- "Reengaging in Agricultural Water Management: Challenges and Options". The World Bank. pp. 4–5. Retrieved 2011-10-30.
- Environment.about.com, Larry West – Water Now More Valuable Than Oil?
- The World Bank, 2009 "Water and Climate Change: Understanding the Risks and Making Climate-Smart Investment Decisions". pp. 19–22. Retrieved 2011-10-24.
- "Nutrients in fresh water"
- EARTH our home Geography textbook
- "Fresh Water in the Future". Un.org (2010-12-17). Retrieved on 2012-12-29.
- Water Aid. "Water". Retrieved 17 March 2012.
- Gleick, P. "Basic Water Requirements for Human Activities". Retrieved 17 March 2012.
- Filley, S. "How much does a cow need ?". Retrieved 17 March 2012.
- Natural Resource Management and Environmental Dept. "Crops Need Water". Retrieved 17 March 2012.
- "Canada's Fresh Water". Ec.gc.ca (2012-02-16). Retrieved on 2012-12-29.
- "Water Facts". Ec.gc.ca (2009-11-19). Retrieved on 2012-12-29.
- "Project Blue Water in Canada". Janegoodall.ca. Retrieved on 2012-12-29.
- "Water Facts". Water.org. Retrieved on 2012-12-29.
- "The Drying of the West". Economist.com (2011-01-27). Retrieved on 2012-12-29.
- "Water Facts"
- "Water in the Developing World"
- Jackson, Robert B., Stephen R. Carpenter, Clifford N. Dahm, Diane M. McKnight, Robert J. Naiman, Sandra L. Postel, and Steven W. Running. 2001. Water in a changing world. Ecological Applications 11(4): 1027–1045.
- Moustakas, A. & I. Karakassis. How diverse is aquatic biodiversity research?, Aquatic Ecology, 39, 367–375
- Richter, Brian D., Ruth Mathews, David L. Harrison, and Robert Wigington. 2003. Ecologically sustainable water management: managing river flows for ecological integrity. Ecological Applications 13(1): 206–224.
- The World Bank's work and publications on water resources
- World Bank report on Agricultural water management
- FBA.org.uk, Freshwater Biological Association
- Review of freshwater ecology in the UK
- Environment-agency.gov.uk UK Environment Agency website
- UK National pond monitoring network
- U.S. Geological Survey
- Fresh Water National Geographic
- Safe and Sustainable Water for Haiti web site hosted by Grand Valley State University