Water
Water covers about 71% of the Earth's surface, and roughly 96.5% of all that water sits in the seas and oceans. It is transparent, tasteless, odorless, and nearly colorless, with only a hint of blue. Yet this simple compound of hydrogen and oxygen behaves unlike almost anything else in nature. It is the only common substance that exists as a solid, a liquid, and a gas under normal conditions on Earth. It is so good at dissolving things that it earns the nickname the universal solvent. And it is vital to every known form of life, even though it provides no food energy at all. How can a molecule this small bend the rules of physics, shape entire civilizations, and turn up in clouds 12 billion light years away? The answers begin with the strange way two hydrogen atoms cling to one oxygen.
In a water molecule, the two hydrogen atoms sit at a 104.5 degree angle to the oxygen, with an O-H bond length of about 0.096 nanometers. A perfect tetrahedron would set that angle at 109.5 degrees. The lone pairs of valence electrons at the other two corners push harder than the hydrogen atoms do, bending the structure. Oxygen pulls electrons more strongly than most elements, so it carries a negative partial charge while the hydrogen atoms turn slightly positive. That imbalance gives the molecule an electrical dipole moment and makes it polar. Because of this polarity, a single molecule in liquid or solid water can form up to four hydrogen bonds with its neighbors. These bonds run roughly 23 kilojoules per mole, far weaker than a covalent O-H bond at 492 kilojoules per mole. Yet they are about ten times stronger than the Van der Waals forces that hold most liquids together. They explain why water boils and melts at far higher temperatures than a similar compound like hydrogen sulfide. They drive its high specific heat capacity of about 4.2 joules per gram-kelvin, and its heat of vaporization of 2257 joules per gram. Hydrogen bonding also produces water's high surface tension and its capillary action, the ability to climb a narrow tube against gravity. Every vascular plant, including every tree, depends on that single quiet trick.
At 1 atmosphere of pressure, water reaches its maximum density of 999.972 kilograms per cubic meter at 3.98 degrees Celsius. Below that temperature, instead of contracting, it expands as it cools toward the freezing point. This makes water nearly unique. It is the only known naturally occurring substance that grows less dense while still a liquid. When it finally freezes into ice, it expands by about 9%, dropping to a density of 917 kilograms per cubic meter. That expansion can burst pipes and crack rocks. In a lake, water at 4 degrees sinks to the bottom while ice forms on top and floats. That floating ice insulates the water beneath and stops it freezing solid, sparing most aquatic organisms through winter. The same anomaly feeds the thermohaline circulation that moves heat across the planet's oceans. The reason ice floats also bends another rule. In most substances, the melting point rises with pressure, but because ice is less dense than water, its melting point falls. Under thick glaciers, that pressure melting can carve out subglacial lakes. The normal surface form is ice Ih, built on hexagonal crystals, but as of 2024, twenty distinct phases of ice have been confirmed by experiment. The eighteenth, ice XVIII, emerged when a droplet was hit with a shock wave that drove its pressure to millions of atmospheres, producing rigid oxygen atoms through which hydrogen flowed freely.
At a temperature of 273.16 kelvin and a pressure of 611.657 pascals, all three phases of water meet at a single triple point. It is the lowest pressure at which liquid water can exist, and until 2019 it defined the Kelvin temperature scale. Move along the phase diagram and the curves part again at 647.096 kelvin and 22.064 megapascals, the critical point. Beyond it, liquid and vapor merge into a supercritical fluid that can be squeezed between gas-like and liquid-like densities. In that state, water can mix freely with nonpolar and most organic compounds, which makes it useful as an ecologically gentle solvent and catalyst. Pressure also rewrites where water boils. At sea level the boiling point is 100 degrees Celsius, but it drops by 1 degree for every 274 meters of altitude. At 1524 meters, cooking time must rise by a fourth to match a sea-level result. In Yellowstone's Old Faithful, water stays liquid past 205 degrees, and in hydrothermal vents it exceeds 400 degrees. The supercritical version even appears in Earth's mantle, acting as a solvent while minerals form, dissolve, and settle.
Pure water is visibly blue, a color born from light absorbed in the region of roughly 600 to 800 nanometers. The principal absorption bands are overtones of the O-H stretching vibrations, the same bonds that hold the molecule together. The color deepens with the depth of the water column, following Beer's law, which is why a swimming pool over white tiles looks bluer than a glass on a windowsill. Suspended solids or algae can shift the hue from blue toward green. Light fades fast with depth. Aquatic plants and algae can live hundreds of meters down, but practically no sunlight reaches the ocean below 1000 meters. The refractive index of liquid water is 1.333 at 20 degrees, higher than air but lower than glycerol, benzene, or glass. Sound, by contrast, travels far in water with little loss, especially at low frequencies, around 0.03 decibels per kilometer at 1 kilohertz. Cetaceans and humans both exploit that clarity, whales for their own communication and people for sonar.
Every known form of life depends on water, both as a solvent for the body's solutes and as a working part of metabolism itself. In anabolism, water is pulled out of molecules to build larger ones like starches, triglycerides, and proteins. In catabolism, it is used to break bonds and release smaller molecules like glucose and amino acids for fuel. Photosynthesis splits water's hydrogen from its oxygen using the sun's energy, then recombines hydrogen to form glucose and release oxygen. Water also sets the baseline for acid-base chemistry, holding a neutral pH of 7 where acids fall below and bases rise above. The human body is, on average, 50 to 60% water, though individuals range from 45% to 75%. The U.S. National Academies of Sciences, Engineering, and Medicine recommend a daily intake of 3.7 liters for adult men and 2.7 liters for women, with about 20% of intake coming from food. The popular claim that a person should drink eight glasses a day appears to have no real basis in science. Drinking far more than needed during exercise can cause water intoxication, which can be fatal. The single largest freshwater resource suitable for drinking is Lake Baikal in Siberia.
More than 660 million people do not have access to safe drinking water. Roughly 70% of the fresh water humans use goes to agriculture, and irrigated farming can account for as much as 80 to 90% of total human water consumption. The pressure is uneven and growing. A 2007 assessment by the International Water Management Institute in Sri Lanka found that more than 1.2 billion people, a fifth of the world, live in areas of physical water scarcity. A further 1.6 billion face economic water scarcity, where missing investment or capacity leaves demand unmet. Some products carry staggering hidden costs. One kilogram of cotton, about the weight of a pair of jeans, requires 10.9 cubic meters of water, and a single kilogram of beef requires 15,000 liters. The Soviet diversion of the Amu Darya and Syr Darya rivers to grow cotton was largely responsible for the disappearance of the Aral Sea. Poor water quality and bad sanitation kill some five million people a year. In 2026, the United Nations declared that humanity had entered the era of water bankruptcy. More than half of large lakes have declined since the 1990s, 35% of wetlands have vanished since 1970, and 4 billion people now face water scarcity for at least one month each year, with droughts costing 307 billion dollars annually.
On the 22nd of July 2011, researchers reported a gigantic cloud of water vapor holding 140 trillion times more water than all of Earth's oceans combined, surrounding a quasar 12 billion light years away. The discovery, they said, shows that water has been prevalent in the universe for nearly its entire existence. Much of that water is a byproduct of star formation, created when outflowing gas and dust slam into surrounding material, heating and compressing it. Closer to home, water turns up across the Solar System. It exists as vapor in the atmospheres of Mercury, Venus, Mars, and the giant planets, and even in the atmospheres of hot stars like Betelgeuse and Antares. Liquid water sits beneath the surfaces of Saturn's moons Enceladus and Titan, with Enceladus holding a 10-kilometer ocean some 30 to 40 kilometers below its south pole. Jupiter's moon Europa shows surface features hinting at a hidden ocean. In September 2009, NASA's Moon Mineralogy Mapper aboard India's Chandrayaan-1 spacecraft detected water molecules on the Moon. Earth itself sits in the habitable zone, and if it were about 5% nearer or farther from the Sun, around 8 million kilometers, the conditions allowing all three phases at once would be far less likely. James Joyce caught this universality in the 1922 novel Ulysses, whose water hymn praises the ocean's unplumbed profundity in the Sundam trench of the Pacific, exceeding 8,000 fathoms.
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Common questions
What is water made of and why is it called the universal solvent?
Water is an inorganic compound of hydrogen and oxygen, and it is often called the universal solvent because it dissolves more substances than any other liquid. Its strong polarity relative to its small molecular size lets it dissolve many salts, sugars, and simple alcohols, though it is poor at dissolving nonpolar substances.
Why does ice float on water?
Ice floats because water becomes about 9% less dense when it freezes, reaching a density of 917 kilograms per cubic meter compared to liquid water's maximum density of 999.972 kilograms per cubic meter at 3.98 degrees Celsius. This floating ice insulates the water below and prevents lakes from freezing solid, which protects most aquatic organisms through winter.
How much of the Earth's surface is covered by water?
Water covers about 71% of the Earth's surface, and seas and oceans make up roughly 96.5% of the total water volume. Groundwater accounts for about 1.7%, and the glaciers and ice caps of Antarctica and Greenland hold another 1.7%.
How much water should a person drink each day?
The U.S. National Academies of Sciences, Engineering, and Medicine recommend a daily intake of 3.7 liters for adult men and 2.7 liters for women, with about 20% of that coming from food. The popular claim that a person should drink eight glasses of water per day appears to have no real basis in science.
Why is water important for life?
All known forms of life depend on water, which acts both as a solvent for the body's solutes and as an essential part of metabolism. It is central to photosynthesis and cellular respiration, and the human body is on average 50 to 60% water.
Where has water been found beyond Earth?
Water has been detected throughout the Solar System and the wider universe, including a cloud of water vapor around a quasar 12 billion light years away that holds 140 trillion times more water than all of Earth's oceans. Within the Solar System, liquid water exists beneath the surfaces of Saturn's moons Enceladus and Titan, and NASA detected water molecules on the Moon in September 2009.
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