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Portal:Water

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The Water Portal

The multiple arches of the Pont du Gard in Roman Gaul (modern-day southern France). The upper tier encloses an aqueduct that carried water to Nimes in Roman times; its lower tier was expanded in the 1740s to carry a wide road across the river.
The multiple arches of thePont du Gard inRoman Gaul (modern-day southernFrance). The upper tier encloses an aqueduct that carried water toNimes in Roman times; its lower tier was expanded in the 1740s to carry a wide road across the river.

Water is aninorganic compound with thechemical formulaH2O. It is a transparent, tasteless, odorless, andnearly colorlesschemical substance. It is the main constituent of Earth'sstreams,lakes, andoceans and thefluids of all known living organisms, in which it acts as asolvent. Water, being apolar molecule, undergoes strong intermolecularhydrogen bonding which is a large contributor to its physical and chemical properties. It is vital for all known forms of life, despite not providingfood energy or being an organicmicronutrient. Due to its presence in all organisms, its chemical stability, its worldwide abundance, and its strong polarity relative to its small molecular size, water is often referred to as the "universal solvent".

Because Earth's surface temperature is relatively close to water'striple point, water exists on Earth as a solid, a liquid, and a gas. It formsprecipitation in the form of rain andaerosols in the form offog. Clouds consist of suspended droplets of water andice, its solid state. When finely divided,crystalline ice may precipitate in the form of snow. The gaseous state of water issteam orwater vapor.

Water covers about 71.0% of the Earth's surface, with seas andoceans making up most of the water volume (about 96.5%). Small portions of water occur asgroundwater (1.7%), in theglaciers and theice caps ofAntarctica andGreenland (1.7%), and in the air asvapor, clouds (consisting of ice and liquid water suspended in air), and precipitation (0.001%). Water moves continually through thewater cycle ofevaporation,transpiration (evapotranspiration),condensation,precipitation, andrunoff, usually reaching the sea. (Full article...)

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Bottle for distilled water in theReal Farmacia in Madrid

Distilled water iswater that has been purified by boiling it intovapor and condensing the vapor back into liquid in a separate container.Any impurities in the original water, such as non-volatile or mineral components, that do not boil below or near theboiling point of water remain in the original container.For example, water escaping as steam from a boiler of heating system or steam engine, leaves behind any dissolved materials, which leads to mineral deposits known asboiler scale.

In general, non-purified water can leave behind mineral deposits, or could cause or interfere with chemical reactions.Distillation is a method for removing impurities from water and other fluids.Distilled water has not been proven to be healthier for drinking than hard water. (Full article...)

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DYK Question Mark
DYK Question Mark

... that theNational Rural Water Association represents more than 26,242 water and wastewater utility members?

... that"water bears" are small, segmented animals that can survive in a dehydrated state for nearly 10 years?

Water News

Note: this section was updated in February 2020

Selected picture

  • Image 1 Lake Mapourika Photo credit: Richard Palmer Morning mist on Lake Mapourika, a lake on the West Coast of New Zealand's South Island. It is the largest of the west coast lakes, a glacier formation from the last ice age. It is filled with fresh rain water which runs through the surrounding forest floor, collecting tannins and giving it its dark colour.
    Image 1

    Morningmist onLake Mapourika, a lake on theWest Coast ofNew Zealand'sSouth Island. It is the largest of the west coast lakes, aglacier formation from the lastice age. It is filled with fresh rain water which runs through the surrounding forest floor, collectingtannins and giving it its dark colour.

  • Image 2 Aral Sea comparison Photographs: NASA; edit: Zafiroblue05 A side-by-side comparison of the Aral Sea in 1989 and 2008, showing its severe shrinkage owing to poor water resource management. The Aral Sea was once the fourth-largest lake in the world. However, the rivers that fed it were diverted by Soviet-era irrigation projects. It had shrunk to 10% of its former size by 2007, and is still shrinking. The near-loss of the Aral Sea, which is now in Kazakhstan and Uzbekistan, has been considered one of the planet's most disastrous examples of poor environmental resource management.
    Image 2

    A side-by-side comparison of theAral Sea in 1989 and 2008, showing its severe shrinkage owing to poorwater resource management. The Aral Sea was once thefourth-largest lake in the world. However, the rivers that fed it were diverted bySoviet-era irrigation projects. It had shrunk to 10% of its former size by 2007, and is still shrinking. The near-loss of the Aral Sea, which is now in Kazakhstan and Uzbekistan, has been considered one of the planet's most disastrous examples of poorenvironmental resource management.

  • Image 3Rain over Beinn Eich, Luss Hills, Scotland
    Image 3Rain over Beinn Eich,Luss Hills, Scotland
  • Image 4A view of the Rosoki River in the eponymous village, Macedonia
    Image 4A view of the Rosoki River in the eponymous village, Macedonia
  • Image 5 Precipitation (meteorology) Image: PZmaps An animated image showing the long-term mean monthly precipitation around the world. Precipitation occurs when a local portion of the atmosphere becomes saturated with water vapor and condenses, forming rain drops or ice crystals within a cloud via collision that then fall to the surface, except for virga, which evaporates while in the air.
    Image 5

    Ananimated image showing the long-termmean monthlyprecipitation around the world. Precipitation occurs when a local portion of theatmosphere becomes saturated withwater vapor andcondenses, forming rain drops or ice crystals within acloud via collision that then fall to the surface, except forvirga, whichevaporates while in the air.

  • Image 6Waterfall Shypit (height 14 m), Mizhhiria Raion, Zakarpattia Oblast of western Ukraine
    Image 6Waterfall Shypit (height 14 m), Mizhhiria Raion, Zakarpattia Oblast of western Ukraine
  • Image 7A wastewater treatment plant in Cuxhaven, Germany. Wastewater treatment is a process used to remove contaminants from wastewater or sewage and convert it into an effluent that can be returned to the water cycle with acceptable impact on the environment, or reused for various purposes (called water reclamation)
    Image 7Awastewater treatment plant in Cuxhaven, Germany. Wastewater treatment is a process used to removecontaminants fromwastewater orsewage and convert it into aneffluent that can be returned to thewater cycle with acceptable impact on the environment, or reused for various purposes (calledwater reclamation)
  • Image 8 Guttation Photo credit: Luc Viatour An example of guttation, the appearance of drops of xylem sap on the tips or edges of leaves of some vascular plants, on an Equisetum. At night, transpiration usually does not occur because most plants have their stomata closed. When there is a high soil moisture level, water will enter plant roots, because the water potential of the roots is lower than in the soil solution. The water will accumulate in the plant creating a slight root pressure. The root pressure forces some water to exude through special leaf tip or edge structures, hydathodes, forming drops. Guttation is not to be confused with dew, which condenses from the atmosphere onto the plant surface.
    Image 8

    An example ofguttation, the appearance of drops ofxylem sap on the tips or edges of leaves of somevascular plants, on anEquisetum. At night,transpiration usually does not occur because most plants have theirstomata closed. When there is a highsoil moisture level, water will enter plant roots, because thewater potential of the roots is lower than in the soil solution. The water will accumulate in the plant creating a slightroot pressure. The root pressure forces some water to exude through specialleaf tip or edge structures,hydathodes, forming drops. Guttation is not to be confused withdew, whichcondenses from the atmosphere onto the plant surface.

  • Image 9Waves on rocks at sunset in Sète, France
    Image 9Waves on rocks at sunset inSète, France
  • Image 10The water cycle
    Image 10Thewater cycle
  • Image 11 Haditha Dam Photograph credit: NASA, Kjell N. Lindgren The Haditha Dam is an earth-filled dam in Iraq, holding back the waters of the Euphrates to create Lake Qadisiyah. The area around Haditha is very arid, with a hot desert climate; the annual precipitation is about 127 millimetres (5 in), mainly occurring during the winter. This photograph, taken from the International Space Station in November 2015, shows the reservoir at a low water level, surrounded by an expanse of dry lakebed; the Haditha Dam is visible near the top of the image. Lake Qadisiyah has a maximum water-storage capacity of 8.3 cubic kilometres (2.0 cu mi) and a maximum surface area of 500 square kilometres (190 sq mi). The associated hydroelectric power station is capable of generating 660 megawatts of electricity, and outlets at the foot of the dam can discharge 3,000 cubic metres (110,000 cu ft) of water per second for irrigation.
    Image 11

    TheHaditha Dam is anearth-filled dam in Iraq, holding back the waters of theEuphrates to createLake Qadisiyah. The area aroundHaditha is very arid, with ahot desert climate; the annual precipitation is about 127 millimetres (5 in), mainly occurring during the winter. This photograph, taken from theInternational Space Station in November 2015, shows the reservoir at a low water level, surrounded by an expanse of dry lakebed; the Haditha Dam is visible near the top of the image. Lake Qadisiyah has a maximum water-storage capacity of 8.3 cubic kilometres (2.0 cu mi) and a maximum surface area of 500 square kilometres (190 sq mi). The associatedhydroelectric power station is capable of generating 660 megawatts of electricity, and outlets at the foot of the dam can discharge 3,000 cubic metres (110,000 cu ft) of water per second forirrigation.

  • Image 12 Impact sprinkler Photograph: JJ Harrison The head of an impact sprinkler, a type of irrigation sprinkler in which the sprinkler head, driven in a circular motion by the force of the outgoing water, pivots on a bearing on top of its threaded attachment nut. Invented in 1935 by Orton Englehardt, it quickly found widespread use.
    Image 12

    The head of animpact sprinkler, a type ofirrigation sprinkler in which the sprinkler head, driven in a circular motion by the force of the outgoing water, pivots on abearing on top of itsthreaded attachment nut. Invented in 1935 by Orton Englehardt, it quickly found widespread use.

  • Image 13 Drop impact Photograph: José Manuel Suárez When a liquid drop impacts the surface of a liquid reservoir it can float, bounce, coalesce with the reservoir, or splash. A floating drop remains on the surface for several seconds. Drop bouncing can occur on perturbed liquid surfaces. If the drop is able to rupture the thin film of gas which separates it from the liquid reservoir, it can coalesce. Additionally, higher Weber number drop impacts produce splashing. In the splashing regime, the impacting drop creates a crater in the fluid surface, followed by a crown around the crater. Finally, a central jet, called the "Rayleigh jet" or "Worthington jet", protrudes from the center of the crater. If the impact energy is high enough, the jet rises to the point where it pinches off, sending one or more droplets upward out of the surface.
    Image 13

    Photograph: José Manuel Suárez

    When a liquiddrop impacts the surface of a liquid reservoir it can float, bounce, coalesce with the reservoir, or splash. A floating drop remains on the surface for several seconds. Drop bouncing can occur on perturbed liquid surfaces. If the drop is able to rupture the thin film of gas which separates it from the liquid reservoir, it can coalesce. Additionally, higherWeber number drop impacts produce splashing. In the splashing regime, the impacting drop creates a crater in the fluid surface, followed by a crown around the crater. Finally, a central jet, called the "Rayleigh jet" or "Worthington jet", protrudes from the center of the crater. If the impact energy is high enough, the jet rises to the point where it pinches off, sending one or more droplets upward out of the surface.

  • Image 14Breaking waves at Porto Covo, Portugal
    Image 14Breakingwaves atPorto Covo, Portugal
  • Image 15Surface irrigation system using siphon tubes
    Image 15Surfaceirrigation system using siphon tubes
  • Image 16A cooling pond at The Maasvlakte
    Image 16Acooling pond at TheMaasvlakte
  • Image 17 Snow Photo credit: Wilson Bentley Plate XIX of "Studies among the Snow Crystals ... " by Wilson Bentley (1902), the first person known to photograph snowflakes. He did so by catching an individual snowflake on a blackboard, rushing it onto some black velvet, which he would then photograph using a bellows camera he had attached to a microscope. His first photograph of a snowflake was on January 15, 1885 and he would capture over 5000 images of crystals in his lifetime. Bentley also photographed all forms of ice and natural water formations including clouds and fog. He was the first American to record raindrop sizes and was one of the first cloud physicists.
    Image 17

    Photo credit:Wilson Bentley

    Plate XIX of "Studies among theSnow Crystals ... " byWilson Bentley (1902), the first person known to photograph snowflakes. He did so by catching an individual snowflake on a blackboard, rushing it onto some black velvet, which he would then photograph using abellows camera he had attached to amicroscope. His first photograph of a snowflake was on January 15, 1885 and he would capture over 5000 images of crystals in his lifetime. Bentley also photographed all forms ofice and naturalwater formations includingclouds andfog. He was the firstAmerican to recordraindrop sizes and was one of the firstcloud physicists.

  • Image 18A fire hydrant in Alkmaar, the Netherlands. Fire hydrants are a source of water provided by most metropolitan communities to enable firefighters to tap into the municipal water supply to assist in extinguishing a fire.
    Image 18Afire hydrant inAlkmaar, the Netherlands. Fire hydrants are a source of water provided by most metropolitan communities to enable firefighters to tap into the municipal water supply to assist in extinguishing a fire.
  • Image 19Goðafoss is a waterfall in northern Iceland
    Image 19Goðafoss is awaterfall in northern Iceland
  • Image 20Worm Bay at Port Campbell National Park, Peterborough, Victoria, Australia
    Image 20Worm Bay atPort Campbell National Park, Peterborough, Victoria, Australia
  • Image 21 Iceberg Photograph credit: Andreas Weith An iceberg is a large piece of freshwater ice that has broken off a glacier or an ice shelf and is floating freely in the open sea. Because the sea around this iceberg is so calm, the underwater portion is visible through the clear water. The largest iceberg ever detected was B-15, which split from the Ross Ice Shelf in Antarctica in 2000, and had a flat top; it had a surface area of 11,000 km2 (4,200 sq mi) and broke into several pieces in 2002 and 2003. This picture depicts an irregularly shaped iceberg with a rounded top, calved from a glacier in the Arctic and photographed in the Arctic Ocean north of Svalbard.
    Image 21

    Photograph credit:Andreas Weith

    Aniceberg is a large piece of freshwater ice that has broken off aglacier or anice shelf and is floating freely in the open sea. Because the sea around this iceberg is so calm, the underwater portion is visible through the clear water. The largest iceberg ever detected wasB-15, which split from theRoss Ice Shelf in Antarctica in 2000, and had a flat top; it had a surface area of 11,000 km2 (4,200 sq mi) and broke into several pieces in 2002 and 2003. This picture depicts an irregularly shaped iceberg with a rounded top, calved from a glacier in the Arctic and photographed in theArctic Ocean north ofSvalbard.

  • Image 22 Rain Painting credit: Vincent van Gogh Rain is an oil-on-canvas painting by Dutch painter Vincent van Gogh, part of The Wheat Field, a series that he executed in 1889 while a voluntary patient in the Saint-Paul asylum near Saint-Rémy-de-Provence, France. Through his cell window on the upper floor, he could see an enclosed wheat field, and he made about a dozen paintings of it over the changing seasons. In this work, he represented falling rain with diagonal lines of paint. The style is reminiscent of Japanese prints, but the effect is stylistically personal to Van Gogh. Seen through his rain-splattered window, he shows its bleak aspect in November, with grey clouds overhead and the wheat already harvested. The painting is now in the collection of the Philadelphia Museum of Art.
    Image 22

    Painting credit:Vincent van Gogh

    Rain is an oil-on-canvas painting by Dutch painterVincent van Gogh, part ofThe Wheat Field, a series that he executed in 1889 while a voluntary patient in theSaint-Paul asylum nearSaint-Rémy-de-Provence, France. Through his cell window on the upper floor, he could see an enclosed wheat field, and he made about a dozen paintings of it over the changing seasons. In this work, he represented falling rain with diagonal lines of paint. The style is reminiscent ofJapanese prints, but the effect is stylistically personal to Van Gogh. Seen through his rain-splattered window, he shows its bleak aspect in November, with grey clouds overhead and the wheat already harvested. The painting is now in the collection of thePhiladelphia Museum of Art.

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