A1.1 Water
SL & HL+ AHL sectionsSL and HL, with AHL content · Molecules · Theme A
Big questions
- Which features of the water molecule explain why life depends on it?
- How does living in water differ from living in air, and what does that mean for animals?
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Water: the medium of life
Life began in water, and water is still the medium in which almost every process of life takes place. A medium here means the surroundings in which something happens. The first cells are thought to have formed in water over 3.5 billion years ago (hypotheses include deep-sea hydrothermal vents and shallow pools), and every living cell today is filled with an aqueous solution, a solution in which water is the solvent.
- Cytoplasm is mostly water: water makes up about 70% of the mass of a typical cell, and about 60% of an adult human.
- Metabolism happens in solution. Reactants, products and enzymes are dissolved or suspended in water, so they can move and collide.
- Transport: blood plasma, tissue fluid, xylem sap and phloem sap are all aqueous solutions.
- Reproduction and movement: sperm swim through fluid to the egg, and countless organisms live their whole lives in water.
Several features of water make this possible. It is liquid over the range of temperatures found on most of Earth’s surface, it dissolves a very wide range of substances, it sticks to itself and to other surfaces, and it changes temperature only slowly. All of these properties come from one cause: the hydrogen bonds that form between water molecules, explained in the next section.
Polar covalent bonds and hydrogen bonds
- Polar covalent bond within a molecule: the shared electrons are pulled towards O
- Hydrogen bond (dashed) between molecules: δ+ H of one molecule to δ− O of another
- Bond angle ≈ 104.5°: the bent shape keeps δ+ and δ− on opposite sides
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Text description of this visual
Three ball-and-stick models; oxygen atoms are red and hydrogen atoms grey. The first shows a single water molecule: one oxygen atom joined to two hydrogen atoms by polar covalent bonds, with an angle of about 104.5° between the bonds. A faint red cloud around the oxygen marks its partial negative charge (δ−), blue clouds around the hydrogens mark their partial positive charges (δ+), and two lobes on the far side of the oxygen are its lone pairs of electrons. The second model is a small droplet of liquid water: dashed amber lines are hydrogen bonds, each running from a δ+ hydrogen of one molecule to the δ− oxygen of a neighbouring molecule. One highlighted molecule is hydrogen-bonded to four others, the maximum. With motion turned on, bonds keep breaking and re-forming. The third model is ice: every molecule is hydrogen-bonded to four neighbours in a regular tetrahedral arrangement, forming hexagonal rings around open channels, so ice is less dense than liquid water and floats.
One water molecule
- Oxygen atom
- Oxygen has a larger nuclear charge than hydrogen and attracts shared electrons more strongly (it is more electronegative), so electrons in each bond spend more time near the oxygen.
- Hydrogen atoms
- Each hydrogen atom shares one pair of electrons with the oxygen. Because those electrons are pulled towards the oxygen, the hydrogen nucleus is left partly exposed.
- Polar covalent bond
- A covalent bond is a shared pair of electrons. Here the sharing is unequal, so the bond is polar. These bonds are strong and hold the atoms together within one molecule (intramolecular).
- δ− (partial negative charge)
- The oxygen end of the molecule carries a slight negative charge because the shared electrons are pulled towards it. It is a partial charge, not a full charge like that of an ion.
- δ+ (partial positive charge)
- Each hydrogen carries a slight positive charge. Together with the δ− on oxygen, this makes water a polar molecule, with a positive side and a negative side.
- Lone pairs of electrons
- Two pairs of oxygen's electrons are not shared with hydrogen. They point away from the hydrogens and add to the negative charge on that side, where hydrogens of other molecules can bond.
- Bond angle ≈ 104.5°
- The molecule is bent, not straight. Because of this shape the δ+ charges are both on one side and the δ− on the other, so they do not cancel out and the whole molecule is polar.
Liquid water
- A water molecule
- Each molecule is H₂O. In the liquid the molecules are close together but keep moving, sliding past and turning against each other, so water flows.
- Covalent O–H bond (within a molecule)
- The two bonds inside each molecule are covalent. They are much stronger than hydrogen bonds — roughly twenty times stronger — and do not break when water is heated, melts or boils.
- Hydrogen bond (between molecules)
- A weak attraction between the δ+ hydrogen of one molecule and the δ− oxygen of another, drawn as a dashed line. Hydrogen bonds are intermolecular; they are not bonds inside a molecule.
- δ+ hydrogen attracted to δ− oxygen
- Opposite partial charges attract. The hydrogen of one molecule lines up with a lone pair on the oxygen of its neighbour, so the O–H···O atoms lie in a roughly straight line.
- Up to four hydrogen bonds
- A molecule can donate two hydrogen bonds (one from each hydrogen) and accept two (one at each lone pair), so it can bond to four neighbours. In the liquid most molecules have three or four at any instant.
- A constantly changing network
- Each hydrogen bond lasts only around a picosecond (10⁻¹² s) before breaking, and new ones form at once. Turn on motion to see bonds break and re-form as molecules move.
Ice
- Four hydrogen bonds per molecule
- In ice every molecule is hydrogen-bonded to exactly four neighbours, arranged tetrahedrally. Two of the bonds use its own hydrogens and two use its lone pairs.
- Hexagonal ring
- The molecules form rings of six, which is why snowflakes and ice crystals are hexagonal. The rings are slightly puckered, not flat.
- Open space in the lattice
- The regular hydrogen-bond lattice holds the molecules further apart than in liquid water, leaving open channels through the rings.
- Less dense than liquid water
- Ice is about 9% less dense than liquid water (0.92 compared with 1.00 g cm⁻³), so it floats. A floating layer of ice insulates the water beneath, which stays liquid for aquatic organisms.
- Hydrogen bond
- Each link between two molecules has exactly one hydrogen on it, covalently bonded to one oxygen and hydrogen-bonded (dashed) to the other.
- Covalent O–H bond
- The covalent bonds inside each molecule are unchanged when water freezes. Only the arrangement of hydrogen bonds between molecules changes.
Why water is polar
A water molecule (H₂O) has one oxygen atom joined to two hydrogen atoms by covalent bonds: each bond is a pair of electrons shared between the two atoms. The sharing is unequal. The oxygen nucleus has a much larger positive charge (8 protons) than a hydrogen nucleus (1 proton), so oxygen attracts the shared electrons more strongly; oxygen is more electronegative. The electrons spend more time near the oxygen.
- The oxygen end gains a slight negative charge, written δ− (delta minus).
- Each hydrogen gains a slight positive charge, δ+.
Bonds like this are polar covalent bonds. Because the molecule is bent, with an angle of about 104.5° between the bonds, both δ+ charges are on one side and the δ− on the other. The charges do not cancel out, so the whole molecule is polar.
Hydrogen bonds
Opposite charges attract. The δ+ hydrogen of one water molecule is attracted to the δ− oxygen of a neighbouring molecule. This attraction is a hydrogen bond.
| Covalent O–H bond | Hydrogen bond | |
|---|---|---|
| Where | Within one molecule (intramolecular) | Between molecules (intermolecular) |
| Cause | Shared pair of electrons | Attraction between δ+ H and δ− O |
| Strength | Strong | Weak, about 1/20 as strong |
| Drawn as | Solid line | Dashed line |
Each molecule can form up to four hydrogen bonds: two through its own hydrogen atoms and two through the two lone pairs of electrons on its oxygen. Individual hydrogen bonds are weak and in liquid water each lasts only about a picosecond (10⁻¹² s), but water molecules are so small and numerous that, at any instant, a huge number of them exist. Collectively they give water its unusual properties. In ice, every molecule is held by four hydrogen bonds in an open hexagonal lattice, which is why ice is less dense than liquid water (see the Ice model above).
Cohesion and adhesion
Hydrogen bonds make water molecules stick to each other and to other polar surfaces. These two effects have different names.
Cohesion
Cohesion is the attraction of water molecules to one another by hydrogen bonds. It has two important consequences for organisms.
Transport under tension in xylem. In plants, water evaporates from the walls of cells inside the leaves and diffuses out through the stomata (transpiration). This pulls on the water in the xylem vessels, putting it under tension (a negative pressure). Because of cohesion, the column of water does not break: the whole column is pulled up from the roots, even to the top of trees over 100 m tall. No energy from the plant is used to lift the water. (More on this in B3.2 Transport.)
Surface tension. A molecule inside the liquid is pulled equally in all directions, but molecules at the surface have no water molecules above them, so they are pulled sideways and inwards. The hydrogen-bonded surface behaves like a stretched film that resists being broken. Small animals use this film as a habitat: pond skaters (Gerris) stand and run on it, and mosquito larvae hang from it to breathe.
Adhesion
Adhesion is the attraction of water to other materials that are polar or charged, by hydrogen bonds or by attraction between water’s partial charges and charged groups. Water adheres to glass, to clay and humus particles in soil, and to cellulose, whose many –OH groups form hydrogen bonds with water.
Adhesion and cohesion together produce capillary action: water is drawn along narrow spaces because it adheres to the walls, and cohesion pulls more water along behind. The narrower the space, the higher the water rises.
- In soil, water moves through the narrow pores between particles, including upwards from wetter layers, so roots can reach it.
- In plant cell walls, water spreads through the network of cellulose fibres. Cell walls stay wet, and walls inside leaves are refilled from the xylem as water evaporates from them.
Reduced motion is on: use the arrows to step through. Change this in Display settings.
Text description of this animation
Five panels. First, water molecules joined by hydrogen bonds: molecules inside the liquid are pulled equally in all directions, but those at the surface are pulled sideways and inwards only. Second, a pond skater standing on the surface film, which bends but does not break. Third, a xylem vessel running from root to leaf: water evaporates from the leaf and the column of water molecules, held together by cohesion, is pulled upwards under tension. Fourth, water molecules forming hydrogen bonds with the polar surface of a glass or cellulose wall (adhesion), which curves the water surface into a meniscus. Fifth, capillary action: water rises higher in narrower tubes, and water is drawn through the narrow spaces between soil particles.
- Cohesion. Hydrogen bonds attract water molecules to one another — this is cohesion. A molecule inside the liquid is pulled equally in every direction, but at the surface there are no water molecules above, so surface molecules are pulled sideways and inwards.
- Surface tension as a habitat. The hydrogen-bonded surface layer resists being stretched or broken (surface tension). A pond skater (Gerris) stands on the surface without sinking in: its weight is spread over long, water-repellent legs, and the surface film bends but does not break.
- Water pulled up xylem under tension. Water evaporates from the cell walls inside leaves (transpiration). This pulls on the water in the xylem, putting it under tension. Cohesion holds the column of molecules together, so the whole column is drawn upwards from the roots without breaking.
- Adhesion to polar surfaces. Water forms hydrogen bonds with polar or charged surfaces, such as glass or the cellulose in plant cell walls — this is adhesion. Water molecules cling to the wall and creep up it, curving the surface into a meniscus.
- Capillary action. In a narrow space, adhesion to the walls pulls water upwards and cohesion pulls more water along behind, so water rises higher in narrower tubes. This capillary action draws water through narrow pores in soil and through cellulose in cell walls.
Water as a solvent
A wide variety of substances dissolve in water. They are called hydrophilic (“water-loving”):
- Ions such as Na⁺ and Cl⁻ dissolve because water molecules are attracted to their charges. The δ− oxygen atoms face positive ions and the δ+ hydrogen atoms face negative ions. Each ion becomes surrounded by a hydration shell of water molecules, which separates it from other ions and keeps it in solution.
- Polar molecules such as glucose, amino acids and urea dissolve because they form hydrogen bonds with water, through groups such as –OH and –NH₂.
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Text description of this animation
Six panels. A crystal of sodium chloride sits in water. Water molecules surround ions at the edge of the crystal: their δ− oxygens face each positive sodium ion and their δ+ hydrogens face each negative chloride ion. Each ion is pulled into solution inside its own shell of water molecules (a hydration shell). Next, a glucose molecule forms hydrogen bonds with water through its polar hydroxyl (–OH) groups, so it dissolves. Then two droplets of oil (a non-polar lipid) stay separate from the water and merge with each other, because water molecules hydrogen-bond with each other rather than with the lipid. The last panel shows dissolved substances carried in blood plasma and in xylem sap.
- An ionic crystal in water. Sodium chloride is made of positive sodium ions (Na⁺) and negative chloride ions (Cl⁻) held in a lattice by ionic bonds. Polar water molecules move randomly around the crystal.
- Water pulls ions away. Water molecules turn to face the ions at the edge of the crystal. Their δ− oxygen atoms are attracted to Na⁺ and their δ+ hydrogen atoms to Cl⁻. These attractions pull the ions out of the lattice.
- Hydration shells. Each dissolved ion is surrounded by a shell of water molecules, oxygen inwards around Na⁺ and hydrogen inwards around Cl⁻. The shells keep the ions apart, so they stay in solution. Substances that dissolve like this are hydrophilic.
- Polar molecules dissolve too. Glucose has five polar –OH groups (and an oxygen in its ring). They form hydrogen bonds with water molecules, so glucose dissolves readily. Amino acids, urea and many other polar molecules dissolve in the same way.
- Non-polar molecules do not dissolve. Oil (triglyceride) molecules are non-polar. Water is not repelled by them, but water molecules are much more strongly attracted to each other, so the lipid is excluded and its droplets merge. Such hydrophobic substances are insoluble in water.
- Transport in solution. Blood plasma carries dissolved glucose, amino acids, ions and urea around the body, and xylem sap carries mineral ions up from the roots. Hydrophobic fats and cholesterol cannot dissolve, so blood carries them inside lipoprotein particles.
A medium for metabolism
Because so many substances dissolve in it, water is the medium in which most metabolic reactions happen. Most reactions catalysed by enzymes take place in water-based (aqueous) solutions: in the cytoplasm, in the matrix of mitochondria and in the stroma of chloroplasts. Dissolved substrates and enzymes move about freely, so they collide often. Water is also itself a reactant in hydrolysis reactions and a product of condensation reactions.
A medium for transport
- Animals: blood plasma carries glucose, amino acids, mineral ions, urea, hormones and carbon dioxide (mostly as hydrogencarbonate ions) in solution.
- Plants: xylem sap carries water and mineral ions from the roots; phloem sap carries sucrose and amino acids.
When being insoluble matters
Non-polar substances, such as fats, oils and the hydrocarbon tails of phospholipids, are hydrophobic. They are not repelled by water; water molecules simply attract each other more strongly than they attract the non-polar molecules, so the non-polar molecules are excluded and clump together. Some molecules work precisely because they are hydrophobic and insoluble:
- the hydrophobic core of membranes is a barrier to ions and polar molecules (see B1.1 Carbohydrates and lipids);
- waxy cuticles on leaves and oils on skin reduce water loss;
- triglyceride fat stores do not dissolve, so they do not affect osmosis in the cells that store them.
Hydrophobic molecules in blood need help: fats and cholesterol are carried inside lipoprotein particles, and oxygen, which is non-polar and only slightly soluble, is carried mostly by haemoglobin.
Living in water and in air
Water and air have very different physical properties, so animals that swim face different challenges from those that fly or live on land. Two animals that use the far north show the contrasts well:
- the ringed seal (Pusa hispida), a mammal of Arctic seas, which spends most of its life in the water and comes out onto the sea ice to rest, moult and give birth;
- the black-throated loon (Gavia arctica), a diving bird that breeds on northern lakes, catches fish underwater and flies between lakes and to the coast.
| Property | Water compared with air (20 °C) | Consequence |
|---|---|---|
| Buoyancy | About 830× denser, so it gives far more upward force | Water supports a seal’s weight; a loon in flight must generate lift |
| Viscosity | About 55× more viscous (resistance to flow) | Swimming meets more resistance than flying; streamlined bodies reduce drag |
| Thermal conductivity | About 23× higher | Animals lose heat much faster in water than in air at the same temperature |
| Specific heat capacity | 4.18 J g⁻¹ °C⁻¹: about 4× air per gram, about 3,450× per litre | Water temperature changes slowly, so aquatic habitats are thermally stable |
The high viscosity, specific heat capacity and cohesion of water all come from hydrogen bonding, which also explains why water is liquid at all at Earth’s temperatures (part 2 of the simulation compares it with methane).
1 · Water compared with air (20 °C, sea-level pressure)
Buoyancy (density)
Water ≈ 830× air
A body of density 1030 kg m⁻³: seawater supports 99.5% of its weight (it is almost neutrally buoyant and sinks very slowly); air supports only 0.12%.
- Ringed seal: its body density is close to that of seawater, so the water supports almost all its weight and it can float at the surface with little effort.
- Black-throated loon: air gives almost no support, so in flight it must keep flapping to generate lift. It floats on water, and its bones are less air-filled than those of most birds, which helps it dive.
Viscosity
Water ≈ 55× air
- Ringed seal: water is far more viscous (and denser), so swimming meets much more resistance; a streamlined, torpedo-shaped body and smooth fur reduce drag.
- Black-throated loon: air offers little resistance, so it flies fast. Underwater it swims with powerful feet set far back on a streamlined body.
Thermal conductivity
Water ≈ 23× air
With a 30 °C difference across a 1 cm still layer: water conducts 1,790 W m⁻², air only 77.1 W m⁻².
- Ringed seal: water draws heat from the body about 23 times faster than air at the same temperature, so the seal has a thick layer of blubber (fat), a poor conductor, under its skin.
- Black-throated loon: air conducts heat poorly. Air trapped in its dense, waterproof plumage insulates it in flight and on the water.
Specific heat capacity
Water ≈ 4.2× air per gram, but ≈ 3,450× per litre (4.17 kJ vs 1.21 J per °C)
Cooling 1 litre by 5 °C releases 20.9 kJ from water but only 6.05 J from air.
- Ringed seal: seawater changes temperature slowly, so its habitat is thermally stable: Arctic seawater stays close to its freezing point (about −1.8 °C) even when the air above the ice is far colder.
- Black-throated loon: air temperature swings widely between day and night and between seasons. In winter its breeding lakes freeze, so loons move to coastal seas, which cool so slowly (high specific heat capacity) that they stay ice-free.
2 · Water compared with methane: why hydrogen bonds matter
Methane (CH₄) is a small molecule of similar mass to water (16 compared with 18 g mol⁻¹), but it is non-polar and forms no hydrogen bonds between its molecules.
At 20 °C, water is liquid and methane is a gas.
Show data table
| Property | Water | Air | Water ÷ air |
|---|---|---|---|
| Density (kg m⁻³) | 998 | 1.2 | 829 |
| Viscosity (mPa s) | 1 | 0.0181 | 55.2 |
| Thermal conductivity (W m⁻¹ K⁻¹) | 0.598 | 0.0257 | 23.3 |
| Specific heat capacity (J g⁻¹ K⁻¹) | 4.18 | 1 | 4.16 |
| Heat capacity per litre (J K⁻¹) | 4,170 | 1.21 | 3,450 |
| Property | Water | Methane |
|---|---|---|
| Molar mass (g mol⁻¹) | 18.02 | 16.04 |
| Melting point (°C) | 0 | -182.5 |
| Boiling point (°C) | 100 | -161.5 |
| Latent heat of vaporization (J g⁻¹) | 2,260 | 510 |
| Specific heat capacity of the liquid (J g⁻¹ K⁻¹) | 4.18 | ≈ 3.5 |
| Hydrogen bonds between molecules? | Yes | No |
Reference values at 20 °C; heat flow uses conduction through a still layer only (real heat loss also involves convection, and the animals' insulation). Values are rounded.
Text description of this simulation
Part 1 compares water with air at 20 °C. Water is about 830 times denser than air, so it gives far more buoyancy; a slider sets an animal's body density to show how much of its weight the water or the air supports. Water is about 55 times more viscous, conducts heat about 23 times better, and its heat capacity per volume is about 3,450 times that of air; sliders show the heat lost through a still layer of water or air and the heat released when a litre of each cools. Each property is linked to the ringed seal, which lives in Arctic seawater, and the black-throated loon, which flies, swims and dives. Part 2 compares water with methane, a molecule of similar size without hydrogen bonds: a temperature slider shows that methane melts at −182.5 °C and boils at −161.5 °C, while water is liquid from 0 °C to 100 °C.
The two animals
- Ringed seal. Its body density is close to that of seawater, so the water supports almost all its weight. A streamlined body and flippers reduce resistance in viscous water. Because water draws heat away so quickly, it has a thick layer of blubber (fat), a poor conductor of heat. Its habitat is thermally stable: the seawater under the ice stays close to −1.8 °C, its freezing point, while the air above may be far colder. Seals keep breathing holes open in the ice with their claws, and pups are born in snow lairs on the ice. Ice can form this floating roof only because it is less dense than water.
- Black-throated loon. Air gives almost no buoyancy, so in flight the loon must keep flapping to generate lift, and it needs a long run across the water to take off. Air’s low viscosity lets it fly fast. Its dense, waterproof plumage traps air, a poor conductor, for insulation. On water it floats; to dive it presses air out of its feathers, and its bones are less air-filled than those of most birds. Its feet are set far back for swimming underwater, which makes walking on land awkward. In winter the lakes where it breeds freeze over, so loons migrate to coastal seas that stay ice-free: the large volume of seawater, with its high specific heat capacity, loses heat slowly and does not freeze over.
Where Earth's water came from, and why it stayed
Earth has about 1.4 billion km³ of water, and it has had liquid oceans for most of its 4.5-billion-year history. This long-lasting abundance of water is what allowed life to begin and evolve. But where did the water come from?
The asteroid hypothesis
When the Solar System formed from a disc of gas and dust, the inner region near the young Sun was too hot for water to condense as ice. The rocky planets, including Earth, formed there from mostly dry material, and the young Earth was itself very hot. Further out, beyond the “snow line” in the outer asteroid belt, ice and water-bearing minerals could form. The leading hypothesis is that much of Earth’s water was delivered by water-rich asteroids that collided with Earth during and after its formation.
Evidence comes from the ratio of deuterium (heavy hydrogen, ²H) to ordinary hydrogen in water. Different parts of the Solar System have different D/H ratios, a little like a fingerprint:
- water in carbonaceous chondrites, meteorites from asteroids, has a D/H ratio close to that of Earth’s oceans;
- most comets measured, such as comet 67P studied by the Rosetta spacecraft, have much higher D/H ratios, so they are unlikely to be the main source.
Why Earth kept its water
Two factors let the water stay on Earth, as liquid, for billions of years:
- Gravity. Earth is massive enough for its gravity to hold on to its atmosphere, including water vapour. Small bodies such as the Moon have too little gravity and have lost almost all their gases.
- Temperatures low enough for water to condense. As the young Earth cooled, water vapour condensed into liquid oceans. At Earth’s distance from the Sun, the surface stays mostly between 0 °C and 100 °C, and the upper atmosphere is cold enough that water vapour condenses before it can rise high enough to be split by ultraviolet light and lost to space. Venus, closer to the Sun, appears to have lost most of its water in this way.
Water and the search for life beyond Earth
Every living thing on Earth depends on liquid water as its solvent and medium for metabolism, and no form of life is known that does without it. So when scientists search for life beyond Earth, a guiding strategy is to “follow the water”: they look first for places where liquid water exists now or existed in the past.
The Goldilocks zone
A planet can only have liquid water on its surface if its temperature lies between the melting and boiling points of water. That depends mainly on the planet’s distance from its star. The Goldilocks zone (also called the habitable zone) is the range of distances from a star within which a planet with a suitable atmosphere could keep liquid water on its surface: not too hot, not too cold, but “just right”. Its position depends on how bright the star is: it is closer in around a cool, dim star and further out around a hot, bright one.
- Venus is too close and too hot (about 464 °C); any oceans were lost.
- Earth is in the zone and has had liquid water for billions of years.
- Mars is near the outer edge. It once had rivers and lakes, but it is small: its weak gravity made it easier for most of its atmosphere to escape to space, and today its water is mainly ice.
Where astronomers look
- Exoplanets (planets orbiting other stars) that lie in their star’s Goldilocks zone are the main targets; thousands of exoplanets have been found, and telescopes now analyse some of their atmospheres for water vapour.
- Mars is explored for signs of past life in ancient lake beds.
- Some icy moons outside the zone, such as Europa (Jupiter) and Enceladus (Saturn), are thought to have liquid water oceans beneath their ice, kept warm by tidal heating.
Must-know definitions
- Polar covalent bond
- A covalent bond in which the shared electrons are pulled more strongly towards one atom. In water, oxygen attracts the electrons more than hydrogen does, so oxygen gains a partial negative charge (δ−) and each hydrogen a partial positive charge (δ+).
- Hydrogen bond
- A weak attraction between a δ+ hydrogen atom bonded to an electronegative atom (here oxygen) and a δ− atom of another molecule. It is intermolecular, about one-twentieth the strength of a covalent bond, and drawn as a dashed line.
- Cohesion
- Water molecules sticking to each other because of hydrogen bonds. It lets water be pulled up xylem vessels under tension without the column breaking, and it causes surface tension.
- Surface tension
- The resistance of a water surface to being stretched or broken, because molecules at the surface are held by hydrogen bonds to the molecules beside and below them. It lets small animals such as pond skaters live on the surface.
- Adhesion and capillary action
- Adhesion is water sticking to other polar or charged materials by hydrogen bonds or attraction to charges. Capillary action is the movement of water through narrow spaces, such as soil pores and plant cell walls, caused by adhesion together with cohesion.
- Hydrophilic and hydrophobic
- Hydrophilic substances (polar molecules and ions) are attracted to water and usually dissolve in it. Hydrophobic substances (non-polar molecules such as lipids) are not attracted to water and are insoluble, because water molecules bond more strongly to each other.
- Solvent and hydration shell
- Water dissolves many substances, so it is the medium for metabolism and transport. Each dissolved ion is surrounded by a hydration shell: δ− oxygen atoms face positive ions and δ+ hydrogen atoms face negative ions.
- Buoyancy and viscosity
- Buoyancy is the upward force from a fluid on an object in it; water is about 830 times denser than air, so it supports animals far better. Viscosity is resistance to flow; water is about 55 times more viscous than air.
- Thermal conductivity and specific heat capacity
- Thermal conductivity is how well heat passes through a material (water about 23× air). Specific heat capacity is the energy needed to raise 1 g by 1 °C (water 4.18 J g−1 °C−1), so water bodies heat and cool slowly.
- Extraplanetary origin of waterAHL
- The hypothesis that most of Earth's water was delivered by water-rich asteroids that collided with the young Earth. Earth kept it because its gravity is strong enough to hold water vapour and temperatures were low enough for it to condense into oceans.
- Goldilocks zoneAHL
- The range of distances from a star within which a planet with a suitable atmosphere could have liquid water on its surface: not so close that water boils away, not so far that it all freezes.
Common exam mistakes
Loses marks Hydrogen bonds hold the hydrogen and oxygen atoms together inside a water molecule.
Write instead The O–H bonds inside a molecule are covalent (intramolecular). Hydrogen bonds are weaker attractions between molecules (intermolecular).
Loses marks Water is polar because it contains hydrogen and oxygen, or because oxygen has more electrons.
Write instead Water is polar because electrons are shared unequally: oxygen attracts the shared electrons more strongly (it is more electronegative). The bent shape (≈104.5°) keeps δ+ and δ− on opposite sides, so they do not cancel.
Loses marks Drawing a hydrogen bond as a solid line, or between two hydrogen atoms or two oxygen atoms.
Write instead Draw it as a dashed line from the δ+ hydrogen of one molecule to the δ− oxygen of a different molecule, and label δ+ and δ− on every molecule.
Loses marks Cohesion and adhesion mean the same thing.
Write instead Cohesion is water sticking to water; adhesion is water sticking to other polar or charged materials, such as cellulose. Both depend on hydrogen bonding or attraction to charges.
Loses marks Water rises to the top of tall trees by capillary action.
Write instead It is pulled up by tension created when water evaporates from leaves (transpiration), and cohesion keeps the column unbroken. Capillary action alone could lift water only a short distance.
Loses marks Hydrophobic molecules are repelled by water.
Write instead There is no repulsion: non-polar molecules are simply not attracted to water as strongly as water molecules are attracted to each other, so they are pushed together and do not dissolve.
Loses marks Water has a high specific heat capacity, so it heats up quickly.
Write instead A high specific heat capacity means a lot of energy is needed to change its temperature, so water heats up and cools down slowly, making aquatic habitats thermally stable.
Loses marks Water is a good insulator, so aquatic mammals lose less heat than land animals.
Write instead Water conducts heat about 23 times better than air, so animals in water lose heat faster. That is why the ringed seal needs a thick layer of blubber.
Loses marks Earth's water must have come from comets, because comets are made of ice.
Write instead The leading hypothesis is delivery by asteroids: the deuterium-to-hydrogen ratio of water in carbonaceous asteroids matches Earth's oceans much better than that of most comets measured.
AHLLoses marks A planet in the Goldilocks zone must have water, and so life.
Write instead Being in the zone only means liquid water could exist on the surface; the planet also needs enough gravity and a suitable atmosphere to keep it. Liquid water is necessary for life as we know it, but not proof of life.
AHL
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Why is water described as the medium of life?
The first cells originated in water, and most processes of life still happen in aqueous solution — in the cytoplasm, in blood plasma and in xylem and phloem sap. A typical cell is about 70% water.
What makes the covalent bonds in water polar?
Electrons are shared unequally. Oxygen attracts the shared electrons more strongly than hydrogen (it is more electronegative), so oxygen becomes δ− and each hydrogen δ+.
Why don't the partial charges on a water molecule cancel out?
The molecule is bent (H–O–H angle ≈ 104.5°), so both δ+ hydrogens are on one side and the δ− oxygen on the other.
Define a hydrogen bond (in water).
A weak intermolecular attraction between the δ+ hydrogen of one water molecule and the δ− oxygen of another. Drawn as a dashed line.
How many hydrogen bonds can one water molecule form, and how?
Up to four — two through its own two hydrogen atoms and two through the two lone pairs of electrons on its oxygen. In ice every molecule has all four.
Cohesion vs adhesion
Cohesion is water molecules sticking to each other (hydrogen bonds between water molecules). Adhesion is water sticking to other polar or charged materials, such as cellulose or glass.
How does cohesion allow transport in xylem?
Evaporation from leaves (transpiration) pulls water up the xylem, putting it under tension. Cohesion keeps the column of water molecules continuous, so it is pulled up from the roots without breaking.
What is surface tension, and how do organisms use it?
Surface water molecules are held by hydrogen bonds to those beside and below them, so the surface resists stretching and breaking. Pond skaters stand on it; mosquito larvae hang from it.
What is capillary action and where does it matter?
Water drawn through narrow spaces by adhesion to the walls plus cohesion. It moves water through pores in soil and through the cellulose of plant cell walls.
How do ions dissolve in water?
Water molecules surround each ion in a hydration shell — δ− oxygen towards positive ions (e.g. Na⁺), δ+ hydrogen towards negative ions (e.g. Cl⁻) — separating the ions and keeping them in solution.
Why are non-polar substances such as fats insoluble in water?
They are not repelled; water molecules are simply more strongly attracted to each other than to non-polar molecules, so the non-polar molecules are excluded and clump together (hydrophobic).
Give three examples of molecules whose function depends on being hydrophobic.
Phospholipid tails forming the barrier in membranes; waxy cuticle on leaves (reduces water loss); triglyceride fat stores (insoluble, so no osmotic effect). Oils on skin also reduce water loss.
Water vs air — buoyancy and viscosity, with consequences
Water is ≈830× denser (more buoyancy) and ≈55× more viscous. The ringed seal is supported by seawater but meets more resistance, so it is streamlined. The loon in flight gets almost no support and must flap to generate lift.
Water vs air — thermal conductivity and specific heat capacity, with consequences
Water conducts heat ≈23× better, so the ringed seal needs thick blubber. Water's specific heat capacity (4.18 J g⁻¹ °C⁻¹) is high, so aquatic habitats change temperature slowly; air temperatures swing more, and loons migrate from frozen lakes to coastal seas.
What is the leading hypothesis for the origin of Earth's water, and what evidence supports it?
Delivery by water-rich asteroids colliding with the young Earth. The D/H (deuterium-to-hydrogen) ratio of water in carbonaceous asteroids closely matches Earth's oceans; most comets measured have higher ratios.
Why has Earth retained its water?
Its gravity is strong enough to hold its atmosphere, including water vapour, and temperatures are low enough for water vapour to condense into liquid oceans rather than escape.
What is the Goldilocks zone?
The range of distances from a star within which a planet with a suitable atmosphere could have liquid water on its surface — not so hot that water boils away, not so cold that it all freezes.
Why does the search for extraterrestrial life focus on water?
All known life needs liquid water as its solvent and medium for metabolism, so places with liquid water — planets in the Goldilocks zone, Mars in the past, icy moons such as Europa and Enceladus — are the most likely to support life.
Last reviewed 19 October 2026. Spotted a mistake? Report it.