Properties of water

Physical and chemical properties of pure water

"H2O" and "HOH" redirect here. For other uses, see H2O (disambiguation) and HOH (disambiguation).

For broader coverage of this topic, see Water.

Water (H
₂O)

Names
IUPAC name water, oxidane
Other names Hydrogen hydroxide (HH or HOH), hydrogen oxide, dihydrogen monoxide (DHMO) (systematic name[1]), hydrogen monoxide, dihydrogen oxide, hydric acid, hydrohydroxic acid, hydroxic acid, hydrol,[2] μ-oxido dihydrogen, κ1-hydroxyl hydrogen(0)
Identifiers
CAS Number	7732-18-5 Y
3D model (JSmol)	Interactive image
Beilstein Reference	3587155
ChEBI	CHEBI:15377 Y
ChEMBL	ChEMBL1098659 Y
ChemSpider	937 Y
Gmelin Reference	117
PubChem CID	962
RTECS number	ZC0110000
UNII	059QF0KO0R Y
InChI InChI=1S/H2O/h1H2 Y Key: XLYOFNOQVPJJNP-UHFFFAOYSA-N Y
SMILES O
Properties
Chemical formula	H 2O
Molar mass	18.01528(33) g/mol
Appearance	White crystalline solid, almost colorless liquid with a hint of blue, colorless gas[3]
Odor	None
Density	Liquid:[4] 0.9998396 g/mL at 0 °C 0.9970474 g/mL at 25 °C 0.961893 g/mL at 95 °C Solid:[5] 0.9167 g/ml at 0 °C
Melting point	0.00 °C (32.00 °F; 273.15 K) [a]
Boiling point	99.98 °C (211.96 °F; 373.13 K) [6][a]
Solubility in water	N/A
Solubility	Poorly soluble in haloalkanes, aliphatic and aromatic hydrocarbons, ethers.[7] Improved solubility in carboxylates, alcohols, ketones, amines. Miscible with methanol, ethanol, propanol, isopropanol, acetone, glycerol, 1,4-dioxane, tetrahydrofuran, sulfolane, acetaldehyde, dimethylformamide, dimethoxyethane, dimethyl sulfoxide, acetonitrile. Partially miscible with Diethyl ether, Methyl Ethyl Ketone, Dichloromethane, Ethyl Acetate, Bromine.
Vapor pressure	3.1690 kilopascals or 0.031276 atm[8]
Acidity (pKa)	13.995[9][10][b]
Basicity (pKb)	13.995
Conjugate acid	Hydronium
Conjugate base	Hydroxide
Thermal conductivity	0.6065 W/(m·K)[13]
Refractive index (nD)	1.3330 (20 °C)[14]
Viscosity	0.890 cP[15]
Structure
Crystal structure	Hexagonal
Point group	C2v
Molecular shape	Bent
Dipole moment	1.8546 D[16]
Thermochemistry
Heat capacity (C)	75.385 ± 0.05 J/(mol·K)[17]
Std molar entropy (So298)	69.95 ± 0.03 J/(mol·K)[17]
Std enthalpy of formation (ΔfHo298)	−285.83 ± 0.04 kJ/mol[7][17]
Gibbs free energy (ΔfG˚)	−237.24 kJ/mol[7]
Hazards
Main hazards	Drowning Avalanche (as snow) Water intoxication (see also Dihydrogen monoxide parody)
NFPA 704	0 0 0
Flash point	Non-flammable
Related compounds
Other cations	Hydrogen sulfide Hydrogen selenide Hydrogen telluride Hydrogen polonide Hydrogen peroxide
Related solvents	Acetone Methanol
Supplementary data page
Structure and properties	Refractive index (n), Dielectric constant (εr), etc.
Thermodynamic data	Phase behaviour solid–liquid–gas
Spectral data	UV, IR, NMR, MS
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
Y verify (what is YN ?)
Infobox references

Water (H
₂O) is a polar inorganic compound that is at room temperature a tasteless and odorless liquid, which is nearly colorless apart from an inherent hint of blue. It is by far the most studied chemical compound and is described as the "universal solvent" ^[18][19] and the "solvent of life".^[20] It is the most abundant substance on Earth^[21] and the only common substance to exist as a solid, liquid, and gas on Earth's surface.^[22] It is also the third most abundant molecule in the universe.^[21]

Water molecules form hydrogen bonds with each other and are strongly polar. This polarity allows it to dissociate ions in salts and bond to other polar substances such as alcohols and acids, thus dissolving them. Its hydrogen bonding causes its many unique properties, such as having a solid form less dense than its liquid form,^[c] a relatively high boiling point of 100 °C for its molar mass, and a high heat capacity.

Water is amphoteric, meaning that it can exhibit properties of an acid or a base, depending on the pH of the solution that it is in; it readily produces both H⁺
and OH⁻
ions.^[c] Related to its amphoteric character, it undergoes self-ionization. The product of the activities, or approximately, the concentrations of H⁺
and OH⁻
is a constant, so their respective concentrations are inversely proportional to each other.^[23]

Contents

• 
  1 Physical properties
  
  
  
  • 
    1.1 Water, ice, and vapor
    
    
    
    • 
      1.1.1 Heat capacity and heats of vaporization and fusion
      
    
    
    • 
      1.1.2 Density of water and ice
      
    
    
    • 
      1.1.3 Density of saltwater and ice
      
    
    
    • 
      1.1.4 Miscibility and condensation
      
    
    
    • 
      1.1.5 Vapor pressure
      
    
    
    • 
      1.1.6 Compressibility
      
    
    
    • 
      1.1.7 Triple point
      
    
    
    • 
      1.1.8 Melting point
      
    
    
    
    
  
  
  • 
    1.2 Electrical properties
    
    
    
    • 
      1.2.1 Electrical conductivity
      
    
    
    
    
  
  
  • 
    1.3 Polarity and hydrogen bonding
    
    
    
    • 
      1.3.1 Cohesion and adhesion
      
    
    
    • 
      1.3.2 Surface tension
      
    
    
    • 
      1.3.3 Capillary action
      
    
    
    • 
      1.3.4 Water as a solvent
      
    
    
    • 
      1.3.5 Quantum tunneling
      
    
    
    
    
  
  
  • 
    1.4 Electromagnetic absorption
    
  
  
  
  


• 
  2 Structure
  


• 
  3 Chemical properties
  
  
  
  • 
    3.1 Geochemistry
    
  
  
  • 
    3.2 Acidity in nature
    
  
  
  
  


• 
  4 Isotopologues
  


• 
  5 Occurrence
  


• 
  6 Reactions
  
  
  
  • 
    6.1 Acid-base reactions
    
  
  
  • 
    6.2 Ligand chemistry
    
  
  
  • 
    6.3 Organic chemistry
    
  
  
  • 
    6.4 Water in redox reactions
    
  
  
  • 
    6.5 Electrolysis
    
  
  
  
  


• 
  7 History
  


• 
  8 Nomenclature
  


• 
  9 See also
  


• 
  10 Footnotes
  


• 
  11 References
  
  
  
  • 
    11.1 Notes
    
  
  
  • 
    11.2 Bibliography
    
  
  
  
  


• 
  12 Further reading
  


• 
  13 External links
  

Physical properties

See also: Water chemistry analysis

Water is the chemical substance with chemical formula H
₂O; one molecule of water has two hydrogen atoms covalently bonded to a single oxygen atom.^[24]
Water is a tasteless, odorless liquid at ambient temperature and pressure. Liquid water has weak absorption bands at wavelengths of around 750 nm which cause it to appear to have a blue colour.^[3] This can easily be observed in a water-filled bath or wash-basin whose lining is white. Large ice crystals, as in glaciers, also appear blue.

Unlike other analogous hydrides of the oxygen family, water is primarily a liquid under standard conditions due to hydrogen bonding. The molecules of water are constantly moving in relation to each other, and the hydrogen bonds are continually breaking and reforming at timescales faster than 200 femtoseconds (2×10⁻¹³ seconds).^[25]
However, these bonds are strong enough to create many of the peculiar properties of water, some of which make it integral to life.

Water, ice, and vapor

Within the Earth's atmosphere and surface, the liquid phase is the most common and is the form that is generally denoted by the word "water". The solid phase of water is known as ice and commonly takes the structure of hard, amalgamated crystals, such as ice cubes, or loosely accumulated granular crystals, like snow. Aside from common hexagonal crystalline ice, other crystalline and amorphous phases of ice are known. The gaseous phase of water is known as water vapor (or steam). Visible steam and clouds are formed from minute droplets of water suspended in the air.

Water also forms a supercritical fluid. The critical temperature is 647 K and the critical pressure is 22.064 MPa. In nature this only rarely occurs in extremely hostile conditions. A likely example of naturally occurring supercritical water is in the hottest parts of deep water hydrothermal vents, in which water is heated to the critical temperature by volcanic plumes and the critical pressure is caused by the weight of the ocean at the extreme depths where the vents are located. This pressure is reached at a depth of about 2200 meters: much less than the mean depth of the ocean (3800 meters).^[26]

Heat capacity and heats of vaporization and fusion

Heat of vaporization of water from melting to critical temperature

Water has a very high specific heat capacity of 4.1814 J/(g·K) at 25 °C – the second highest among all the heteroatomic species (after ammonia), as well as a high heat of vaporization (40.65 kJ/mol or 2257 kJ/kg at the normal boiling point), both of which are a result of the extensive hydrogen bonding between its molecules. These two unusual properties allow water to moderate Earth's climate by buffering large fluctuations in temperature. Most of the additional energy stored in the climate system since 1970 has accumulated in the oceans.^[27]

The specific enthalpy of fusion (more commonly known as latent heat) of water is 333.55 kJ/kg at 0 °C: the same amount of energy is required to melt ice as to warm ice from −160 °C up to its melting point or to heat the same amount of water by about 80 °C. Of common substances, only that of ammonia is higher. This property confers resistance to melting on the ice of glaciers and drift ice. Before and since the advent of mechanical refrigeration, ice was and still is in common use for retarding food spoilage.

The specific heat capacity of ice at −10 °C is 2.03 J/(g·K)^[28]
and the heat capacity of steam at 100 °C is 2.08 J/(g·K).^[29]

Density of water and ice

Density of ice and water as a function of temperature

The density of water is about 1 gram per cubic centimetre (62 lb/cu ft): this relationship was originally used to define the gram.^[30] The density varies with temperature, but not linearly: as the temperature increases, the density rises to a peak at 3.98 °C (39.16 °F) and then decreases.^[31] This unusual negative thermal expansion below 4 °C (39 °F) is also observed in molten silica.^[32] Regular, hexagonal ice is also less dense than liquid water—upon freezing, the density of water decreases by about 9%.^[33] Other substances that expand on freezing are silicon (melting point of 1,687 K (1,414 °C; 2,577 °F)), gallium (melting point of 303 K (30 °C; 86 °F)|, germanium (melting point of 1,211 K (938 °C; 1,720 °F)), antimony (melting point of 904 K (631 °C; 1,168 °F)), and bismuth (melting point of 545 K (272 °C; 521 °F)). Also, fairly pure silicon has a negative coefficient of thermal expansion for temperatures between about 18 and 120 kelvins.^[34]

These effects are due to the reduction of thermal motion with cooling, which allows water molecules to form more hydrogen bonds that prevent the molecules from coming close to each other.^[31] While below 4 °C the breakage of hydrogen bonds due to freezing allows water molecules to pack closer despite the increase in the thermal motion (which tends to expand a liquid), above 4 °C water expands as the temperature increases.^[31] Water near the boiling point is about 4% less dense than water at 4 °C (39 °F).^[33][d]

Under increasing pressure, ice undergoes a number of transitions to other polymorphs with higher density than liquid water, such as ice II, ice III, high-density amorphous ice (HDA), and very-high-density amorphous ice (VHDA).^[35][36]

Temperature distribution in a lake in summer and winter

The unusual density curve and lower density of ice than of water is vital to life—if water were most dense at the freezing point, then in winter the very cold water at the surface of lakes and other water bodies would sink, the lake could freeze from the bottom up, and all life in them would be killed.^[33] Furthermore, given that water is a good thermal insulator (due to its heat capacity), some frozen lakes might not completely thaw in summer.^[33] The layer of ice that floats on top insulates the water below.^[37] Water at about 4 °C (39 °F) also sinks to the bottom, thus keeping the temperature of the water at the bottom constant (see diagram).^[33]

Density of saltwater and ice

WOA surface density

The density of salt water depends on the dissolved salt content as well as the temperature. Ice still floats in the oceans, otherwise they would freeze from the bottom up. However, the salt content of oceans lowers the freezing point by about 1.9 °C^[38] (see here for explanation) and lowers the temperature of the density maximum of water to the former freezing point at 0 °C. This is why, in ocean water, the downward convection of colder water is not blocked by an expansion of water as it becomes colder near the freezing point. The oceans' cold water near the freezing point continues to sink. So creatures that live at the bottom of cold oceans like the Arctic Ocean generally live in water 4 °C colder than at the bottom of frozen-over fresh water lakes and rivers.

As the surface of salt water begins to freeze (at −1.9 °C^[38] for normal salinity seawater, 3.5%) the ice that forms is essentially salt-free, with about the same density as freshwater ice. This ice floats on the surface, and the salt that is "frozen out" adds to the salinity and density of the sea water just below it, in a process known as brine rejection. This denser salt water sinks by convection and the replacing seawater is subject to the same process. This produces essentially freshwater ice at −1.9 °C^[38] on the surface. The increased density of the sea water beneath the forming ice causes it to sink towards the bottom. On a large scale, the process of brine rejection and sinking cold salty water results in ocean currents forming to transport such water away from the Poles, leading to a global system of currents called the thermohaline circulation.

Miscibility and condensation

Red line shows saturation

Main article: Humidity

See also: List of water-miscible solvents

Water is miscible with many liquids, including ethanol in all proportions. Water and most oils are immiscible usually forming layers according to increasing density from the top. This can be predicted by comparing the polarity. Water being a relatively polar compound will tend to be miscible with liquids of high polarity such as ethanol and acetone, whereas compounds with low polarity will tend to be immiscible and poorly soluble such as with hydrocarbons.

As a gas, water vapor is completely miscible with air. On the other hand, the maximum water vapor pressure that is thermodynamically stable with the liquid (or solid) at a given temperature is relatively low compared with total atmospheric pressure.
For example, if the vapor's partial pressure is 2% of atmospheric pressure and the air is cooled from 25 °C, starting at about 22 °C water will start to condense, defining the dew point, and creating fog or dew. The reverse process accounts for the fog burning off in the morning. If the humidity is increased at room temperature, for example, by running a hot shower or a bath, and the temperature stays about the same, the vapor soon reaches the pressure for phase change, and then condenses out as minute water droplets, commonly referred to as steam.

A saturated gas or one with 100% relative humidity is when the vapor pressure of water in the air is at equilibrium with vapor pressure due to (liquid) water; water (or ice, if cool enough) will fail to lose mass through evaporation when exposed to saturated air. Because the amount of water vapor in air is small, relative humidity, the ratio of the partial pressure due to the water vapor to the saturated partial vapor pressure, is much more useful.
Vapor pressure above 100% relative humidity is called super-saturated and can occur if air is rapidly cooled, for example, by rising suddenly in an updraft.^[e]

Vapor pressure

Main article: Vapor pressure of water

Vapor pressure diagrams of water

Compressibility

The compressibility of water is a function of pressure and temperature. At 0 °C, at the limit of zero pressure, the compressibility is 6990510000000000000♠5.1×10⁻¹⁰ Pa⁻¹. At the zero-pressure limit, the compressibility reaches a minimum of 6990440000000000000♠4.4×10⁻¹⁰ Pa⁻¹ around 45 °C before increasing again with increasing temperature. As the pressure is increased, the compressibility decreases, being 6990390000000000000♠3.9×10⁻¹⁰ Pa⁻¹ at 0 °C and 100 megapascals (1,000 bar).^[39]

The bulk modulus of water is about 2.2 GPa.^[40] The low compressibility of non-gases, and of water in particular, leads to their often being assumed as incompressible. The low compressibility of water means that even in the deep oceans at 4 km depth, where pressures are 40 MPa, there is only a 1.8% decrease in volume.^[40]

Triple point

Main article: Triple point § Triple point of water

The Solid/Liquid/Vapour triple point of liquid water, ice I_h and water vapor in the lower left portion of a water phase diagram.

The temperature and pressure at which ordinary solid, liquid, and gaseous water coexist in equilibrium is a triple point of water. Since 1954, this point had been used to define the base unit of temperature, the kelvin^[41][42] but, starting in 2019, the kelvin will be defined using the Boltzmann constant, rather than the triple point of water.^[43]

Due to the existence of many polymorphs (forms) of ice, water has other triple points, which have either three polymorphs of ice or two polymorphs of ice and liquid in equilibrium.^[42]Gustav Heinrich Johann Apollon Tammann in Göttingen produced data on several other triple points in the early 20th century. Kamb and others documented further triple points in the 1960s.^[44][45][46]

The various triple points of water

Phases in stable equilibrium	Pressure	Temperature
liquid water, ice Ih, and water vapor	611.657 Pa[47]	273.16 K (0.01 °C)
liquid water, ice Ih, and ice III	209.9 MPa	251 K (−22 °C)
liquid water, ice III, and ice V	350.1 MPa	−17.0 °C
liquid water, ice V, and ice VI	632.4 MPa	0.16 °C
ice Ih, Ice II, and ice III	213 MPa	−35 °C
ice II, ice III, and ice V	344 MPa	−24 °C
ice II, ice V, and ice VI	626 MPa	−70 °C

Melting point

The melting point of ice is 0 °C (32 °F; 273 K) at standard pressure; however, pure liquid water can be supercooled well below that temperature without freezing if the liquid is not mechanically disturbed. It can remain in a fluid state down to its homogeneous nucleation point of about 231 K (−42 °C; −44 °F).^[48] The melting point of ordinary hexagonal ice falls slightly under moderately high pressures, by 0.0073 °C (0.0131 °F)/atm^[f] or about 0.5 °C (0.90 °F)/70 atm^[g][49] as the stabilization energy of hydrogen bonding is exceeded by intermolecular repulsion, but as ice transforms into its allotropes (see crystalline states of ice) above 209.9 MPa (2,072 atm), the melting point increases markedly with pressure, i.e., reaching 355 K (82 °C) at 2.216 GPa (21,870 atm) (triple point of Ice VII^[50]).

Electrical properties

Electrical conductivity

Pure water containing no exogenous ions is an excellent insulator, but not even "deionized" water is completely free of ions. Water undergoes auto-ionization in the liquid state, when two water molecules form one hydroxide anion (OH⁻
) and one hydronium cation (H
₃O⁺
).

Because water is such a good solvent, it almost always has some solute dissolved in it, often a salt. If water has even a tiny amount of such an impurity, then the ions can carry charges back and forth, allowing the water to conduct electricity far more readily.

It is known that the theoretical maximum electrical resistivity for water is approximately 18.2 MΩ·cm (182 kΩ·m) at 25 °C.^[51] This figure agrees well with what is typically seen on reverse osmosis, ultra-filtered and deionized ultra-pure water systems used, for instance, in semiconductor manufacturing plants. A salt or acid contaminant level exceeding even 100 parts per trillion (ppt) in otherwise ultra-pure water begins to noticeably lower its resistivity by up to several kΩ·m.^{[citation needed]}

In pure water, sensitive equipment can detect a very slight electrical conductivity of 0.05501 ± 0.0001 µS/cm at 25.00 °C.^[51] Water can also be electrolyzed into oxygen and hydrogen gases but in the absence of dissolved ions this is a very slow process, as very little current is conducted. In ice, the primary charge carriers are protons (see proton conductor).^[52] Ice was previously thought to have a small but measurable conductivity of 1×10⁻¹⁰ S/cm, but this conductivity is now thought to be almost entirely from surface defects, and without those, ice is an insulator with an immeasurably small conductivity.^[31]

Polarity and hydrogen bonding

See also: Chemical polarity

A diagram showing the partial charges on the atoms in a water molecule

An important feature of water is its polar nature. The structure has a bent molecular geometry for the two hydrogens from the oxygen vertex. The oxygen atom also has two lone pairs of electrons. One effect usually ascribed to the lone pairs is that the H–O–H gas phase bend angle is 104.48°,^[53] which is smaller than the typical tetrahedral angle of 109.47°. The lone pairs are closer to the oxygen atom than the electrons sigma bonded to the hydrogens, so they require more space. The increased repulsion of the lone pairs forces the O–H bonds closer to each other.^[54]

Another consequence of its structure is that water is a polar molecule. Due to the difference in electronegativity, a bond dipole moment points from each H to the O, making the oxygen partially negative and each hydrogen partially positive. A large molecular dipole, points from a region between the two hydrogen atoms to the oxygen atom. The charge differences cause water molecules to aggregate (the relatively positive areas being attracted to the relatively negative areas). This attraction, hydrogen bonding, explains many of the properties of water, such as its solvent properties.^[55]

Although hydrogen bonding is a relatively weak attraction compared to the covalent bonds within the water molecule itself, it is responsible for a number of water's physical properties. These properties include its relatively high melting and boiling point temperatures: more energy is required to break the hydrogen bonds between water molecules. In contrast, hydrogen sulfide (H
₂S), has much weaker hydrogen bonding due to sulfur's lower electronegativity. H
₂S is a gas at room temperature, in spite of hydrogen sulfide having nearly twice the molar mass of water. The extra bonding between water molecules also gives liquid water a large specific heat capacity. This high heat capacity makes water a good heat storage medium (coolant) and heat shield.

Cohesion and adhesion

Dew drops adhering to a spider web

Water molecules stay close to each other (cohesion), due to the collective action of hydrogen bonds between water molecules. These hydrogen bonds are constantly breaking, with new bonds being formed with different water molecules; but at any given time in a sample of liquid water, a large portion of the molecules are held together by such bonds.^[56]

Water also has high adhesion properties because of its polar nature. On extremely clean/smooth glass the water may form a thin film because the molecular forces between glass and water molecules (adhesive forces) are stronger than the cohesive forces.
In biological cells and organelles, water is in contact with membrane and protein surfaces that are hydrophilic; that is, surfaces that have a strong attraction to water. Irving Langmuir observed a strong repulsive force between hydrophilic surfaces. To dehydrate hydrophilic surfaces—to remove the strongly held layers of water of hydration—requires doing substantial work against these forces, called hydration forces. These forces are very large but decrease rapidly over a nanometer or less.^[57] They are important in biology, particularly when cells are dehydrated by exposure to dry atmospheres or to extracellular freezing.^[58]

Surface tension

This paper clip is under the water level, which has risen gently and smoothly. Surface tension prevents the clip from submerging and the water from overflowing the glass edges.

Temperature dependence of the surface tension of pure water

Water has an unusually high surface tension of 71.99 mN/m at 25 °C^[59] which is caused by the strength of the hydrogen bonding between water molecules.^[60] This allows insects to walk on water.^[60]

Capillary action

Because water has strong cohesive and adhesive forces, it exhibits capillary action.^[61] Strong cohesion from hydrogen bonding and adhesion allows trees to transport water more than 100 m upward.^[60]

Water as a solvent

Main article: Aqueous solution

Presence of colloidal calcium carbonate from high concentrations of dissolved lime turns the water of Havasu Falls turquoise.

Water is an excellent solvent due to its high dielectric constant.^[62] Substances that mix well and dissolve in water are known as hydrophilic ("water-loving") substances, while those that do not mix well with water are known as hydrophobic ("water-fearing") substances.^[63] The ability of a substance to dissolve in water is determined by whether or not the substance can match or better the strong attractive forces that water molecules generate between other water molecules. If a substance has properties that do not allow it to overcome these strong intermolecular forces, the molecules are precipitated out from the water. Contrary to the common misconception, water and hydrophobic substances do not "repel", and the hydration of a hydrophobic surface is energetically, but not entropically, favorable.

When an ionic or polar compound enters water, it is surrounded by water molecules (hydration). The relatively small size of water molecules (~ 3 angstroms) allows many water molecules to surround one molecule of solute. The partially negative dipole ends of the water are attracted to positively charged components of the solute, and vice versa for the positive dipole ends.

In general, ionic and polar substances such as acids, alcohols, and salts are relatively soluble in water, and non-polar substances such as fats and oils are not. Non-polar molecules stay together in water because it is energetically more favorable for the water molecules to hydrogen bond to each other than to engage in van der Waals interactions with non-polar molecules.

An example of an ionic solute is table salt; the sodium chloride, NaCl, separates into Na⁺
cations and Cl⁻
anions, each being surrounded by water molecules. The ions are then easily transported away from their crystalline lattice into solution. An example of a nonionic solute is table sugar. The water dipoles make hydrogen bonds with the polar regions of the sugar molecule (OH groups) and allow it to be carried away into solution.

Quantum tunneling

Main article: Quantum tunneling of water

The quantum tunneling dynamics in water was reported as early as 1992. At that time it was known that there are motions which destroy and regenerate the weak hydrogen bond by internal rotations of the substituent water monomers.^[64] On 18 March 2016, it was reported that the hydrogen bond can be broken by quantum tunneling in the water hexamer. Unlike previously reported tunneling motions in water, this involved the concerted breaking of two hydrogen bonds.^[65] Later in the same year, the discovery of the quantum tunneling of water molecules was reported.^[66]

Electromagnetic absorption

Main article: Electromagnetic absorption by water

Water is relatively transparent to visible light, near ultraviolet light, and far-red light, but it absorbs most ultraviolet light, infrared light, and microwaves. Most photoreceptors and photosynthetic pigments utilize the portion of the light spectrum that is transmitted well through water. Microwave ovens take advantage of water's opacity to microwave radiation to heat the water inside of foods. Water's light blue colour is caused by weak absorption in the red part of the visible spectrum.^[3][67]

Structure

Model of hydrogen bonds (1) between molecules of water

A single water molecule can participate in a maximum of four hydrogen bonds because it can accept two bonds using the lone pairs on oxygen and donate two hydrogen atoms. Other molecules like hydrogen fluoride, ammonia and methanol can also form hydrogen bonds. However, they do not show anomalous thermodynamic, kinetic or structural properties like those observed in water because none of them can form four hydrogen bonds: either they cannot donate or accept hydrogen atoms, or there are steric effects in bulky residues. In water, intermolecular tetrahedral structures form due to the four hydrogen bonds, thereby forming an open structure and a three-dimensional bonding network, resulting in the anomalous decrease in density when cooled below 4 °C. This repeated, constantly reorganizing unit defines a three-dimensional network extending throughout the liquid. This view is based upon neutron scattering studies and computer simulations, and it makes sense in the light of the unambiguously tetrahedral arrangement of water molecules in ice structures.

However, there is an alternative theory for the structure of water. In 2004, a controversial paper from Stockholm University suggested that water molecules in liquid form typically bind not to four but to only two others; thus forming chains and rings. The term "string theory of water" (which is not to be confused with the string theory of physics) was coined. These observations were based upon X-ray absorption spectroscopy that probed the local environment of individual oxygen atoms.^[68]

Chemical properties

At standard conditions, water is a polar liquid that slightly dissociates disproportionately into a hydronium ion and hydroxide ion.

2 H
₂O ⇌ H
₃O⁺
+ OH⁻

The ionic product of pure water,K_w has a value of about 10⁻¹⁴ at 25 °C; see data page for values at other temperatures. Pure water has a concentration of the hydroxide ion (OH⁻
) equal to that of the hydrogen ion (H⁺
), which gives a pH of 7 at 25 °C.^[69]

Geochemistry

Action of water on rock over long periods of time typically leads to weathering and water erosion, physical processes that convert solid rocks and minerals into soil and sediment, but under some conditions chemical reactions with water occur as well, resulting in metasomatism or mineral hydration, a type of chemical alteration of a rock which produces clay minerals. It also occurs when Portland cement hardens.

Water ice can form clathrate compounds, known as clathrate hydrates, with a variety of small molecules that can be embedded in its spacious crystal lattice. The most notable of these is methane clathrate, 4 CH
₄·23H
₂O, naturally found in large quantities on the ocean floor.

Acidity in nature

Rain is generally mildly acidic, with a pH between 5.2 and 5.8 if not having any acid stronger than carbon dioxide.^[70] If high amounts of nitrogen and sulfur oxides are present in the air, they too will dissolve into the cloud and rain drops, producing acid rain.

Isotopologues

Several isotopes of both hydrogen and oxygen exist, giving rise to several known isotopologues of water. Vienna Standard Mean Ocean Water is the current international standard for water isotopes. Naturally occurring water is almost completely composed of the neutron-less hydrogen isotope protium. Only 155 ppm include deuterium (²
H or D), a hydrogen isotope with one neutron, and fewer than 20 parts per quintillion include tritium (³
H or T), which has two neutrons. Oxygen also has three stable isotopes, with ¹⁶
O present in 99.76%, ¹⁷
O in 0.04%, and ¹⁸
O in 0.2% of water molecules.^[71]

Deuterium oxide, D
₂O, is also known as heavy water because of its higher density. It is used in nuclear reactors as a neutron moderator. Tritium is radioactive, decaying with a half-life of 4500 days; THO exists in nature only in minute quantities, being produced primarily via cosmic ray-induced nuclear reactions in the atmosphere. Water with one protium and one deuterium atom HDO occurs naturally in ordinary water in low concentrations (~0.03%) and D
₂O in far lower amounts (0.000003%) and any such molecules are temporary as the atoms recombine.

The most notable physical differences between H
₂O and D
₂O, other than the simple difference in specific mass, involve properties that are affected by hydrogen bonding, such as freezing and boiling, and other kinetic effects. This is because the nucleus of deuterium is twice as heavy as protium, and this causes noticeable differences in bonding energies. The difference in boiling points allows the isotopologues to be separated. The self-diffusion coefficient of H
₂O at 25 °C is 23% higher than the value of D
₂O.^[72] Because water molecules exchange hydrogen atoms with one another, hydrogen deuterium oxide (DOH) is much more common in low-purity heavy water than pure dideuterium monoxide D
₂O.

Consumption of pure isolated D
₂O may affect biochemical processes – ingestion of large amounts impairs kidney and central nervous system function. Small quantities can be consumed without any ill-effects; humans are generally unaware of taste differences,^[73] but sometimes report a burning sensation^[74] or sweet flavor.^[75] Very large amounts of heavy water must be consumed for any toxicity to become apparent. Rats, however, are able to avoid heavy water by smell, and it is toxic to many animals.^[76]

Light water refers to deuterium-depleted water (DDW), water in which the deuterium content has been reduced below the standard 155 ppm level.

Occurrence

It is the most abundant substance on Earth and also the third most abundant molecule in the universe, after H
₂ and CO.^[21] 0.23 ppm of the earth's mass is water and 97.39% of the global water volume of 1.38×10⁹ km³ is found in the oceans.^[77]

Reactions

Acid-base reactions

Water is amphoteric: it has the ability to act as either an acid or a base in chemical reactions.^[78] According to the Brønsted-Lowry definition, an acid is a proton (H⁺
) donor and a base is a proton acceptor.^[79] When reacting with a stronger acid, water acts as a base; when reacting with a stronger base, it acts as an acid.^[79] For instance, water receives an H⁺
ion from HCl when hydrochloric acid is formed:

HCl
(acid) + H
₂O
(base) ⇌ H
₃O⁺
+ Cl⁻

In the reaction with ammonia, NH
₃, water donates a H⁺
ion, and is thus acting as an acid:

NH
₃
(base) + H
₂O
(acid) ⇌ NH⁺
₄ + OH⁻

Because the oxygen atom in water has two lone pairs, water often acts as a Lewis base, or electron pair donor, in reactions with Lewis acids, although it can also react with Lewis bases, forming hydrogen bonds between the electron pair donors and the hydrogen atoms of water. HSAB theory describes water as both a weak hard acid and a weak hard base, meaning that it reacts preferentially with other hard species:

H⁺

(Lewis acid) + H
₂O
(Lewis base) → H
₃O⁺

Fe³⁺

(Lewis acid) + H
₂O
(Lewis base) → Fe(H
₂O)³⁺
₆

Cl⁻

(Lewis base) + H
₂O
(Lewis acid) → Cl(H
₂O)⁻
₆

When a salt of a weak acid or of a weak base is dissolved in water, water can partially hydrolyze the salt, producing the corresponding base or acid, which gives aqueous solutions of soap and baking soda their basic pH:

Na
₂CO
₃ + H
₂O ⇌ NaOH + NaHCO
₃

Ligand chemistry

Water's Lewis base character makes it a common ligand in transition metal complexes, examples of which include metal aquo complexes such as Fe(H
₂O)²⁺
₆ to perrhenic acid, which contains two water molecules coordinated to a rhenium center. In solid hydrates, water can be either a ligand or simply lodged in the framework, or both. Thus, FeSO
₄·7H
₂O consists of [Fe₂(H₂O)₆]²⁺ centers and one "lattice water". Water is typically a monodentate ligand, i.e., it forms only one bond with the central atom.^[80]

Some hydrogen-bonding contacts in FeSO₄^.7H₂O. This metal aquo complex crystallizes with one molecule of "lattice" water, which interacts with the sulfate and with the [Fe(H₂O)₆]²⁺ centers.

Organic chemistry

As a hard base, water reacts readily with organic carbocations; for example in a hydration reaction, a hydroxyl group (OH⁻
) and an acidic proton are added to the two carbon atoms bonded together in the carbon-carbon double bond, resulting in an alcohol. When addition of water to an organic molecule cleaves the molecule in two, hydrolysis is said to occur. Notable examples of hydrolysis are the saponification of fats and the digestion of proteins and polysaccharides. Water can also be a leaving group in S_N2 substitution and E2 elimination reactions; the latter is then known as a dehydration reaction.

Water in redox reactions

Water contains hydrogen in the oxidation state +1 and oxygen in the oxidation state −2.^[81] It oxidizes chemicals such as hydrides, alkali metals, and some alkaline earth metals.^[82][83] One example of an alkali metal reacting with water is:^[84]

2 Na + 2 H
₂O → H
₂ + 2 Na⁺
+ 2 OH⁻

Some other reactive metals, such as aluminum and beryllium, are oxidized by water as well, but their oxides adhere to the metal and form a passive protective layer.^[85] Note that the rusting of iron is a reaction between iron and oxygen^[86] that is dissolved in water, not between iron and water.

Water can be oxidized to emit oxygen gas, but very few oxidants react with water even if their reduction potential is greater than the potential of O
₂/H
₂O. Almost all such reactions require a catalyst.^[87]
An example of the oxidation of water is:

4 AgF
₂ + 2 H
₂O → 4 AgF + 4 HF + O
₂

Electrolysis

Main article: Electrolysis of water

Water can be split into its constituent elements, hydrogen and oxygen, by passing an electric current through it.^[88] This process is called electrolysis.
The cathode half reaction is:

2 H⁺
+ 2
e⁻
→ H
₂

The anode half reaction is:

2 H
₂O → O
₂ + 4 H⁺
+ 4
e⁻

The gases produced bubble to the surface, where they can be collected or ignited with a flame above the water if this was the intention. The required potential for the electrolysis of pure water is 1.23 V at 25 °C.^[88] The operating potential is actually 1.48 V or higher in practical electrolysis.

History

Henry Cavendish showed that water was composed of oxygen and hydrogen in 1781.^[89] The first decomposition of water into hydrogen and oxygen, by electrolysis, was done in 1800 by English chemist William Nicholson and Anthony Carlisle.^[89][90] In 1805, Joseph Louis Gay-Lussac and Alexander von Humboldt showed that water is composed of two parts hydrogen and one part oxygen.^[91]

Gilbert Newton Lewis isolated the first sample of pure heavy water in 1933.^[92]

The properties of water have historically been used to define various temperature scales. Notably, the Kelvin, Celsius, Rankine, and Fahrenheit scales were, or currently are, defined by the freezing and boiling points of water. The less common scales of Delisle, Newton, Réaumur and Rømer were defined similarly. The triple point of water is a more commonly used standard point today.

Nomenclature

The accepted IUPAC name of water is oxidane or simply water,^[93] or its equivalent in different languages, although there are other systematic names which can be used to describe the molecule. Oxidane is only intended to be used as the name of the mononuclear parent hydride used for naming derivatives of water by substituent nomenclature.^[94] These derivatives commonly have other recommended names. For example, the name hydroxyl is recommended over oxidanyl for the –OH group. The name oxane is explicitly mentioned by the IUPAC as being unsuitable for this purpose, since it is already the name of a cyclic ether also known as tetrahydropyran.^[95][96]

The simplest systematic name of water is hydrogen oxide. This is analogous to related compounds such as hydrogen peroxide, hydrogen sulfide, and deuterium oxide (heavy water). Using chemical nomenclature for type I ionic binary compounds, water would take the name hydrogen monoxide ,^[97] but this is not among the names published by the International Union of Pure and Applied Chemistry (IUPAC).^[93] Another name is dihydrogen monoxide, which is a rarely used name of water, and mostly used in the dihydrogen monoxide hoax.

Other systematic names for water include hydroxic acid, hydroxylic acid, and hydrogen hydroxide, using acid and base names.^[h] None of these exotic names are used widely. The polarized form of the water molecule, H⁺
OH⁻
, is also called hydron hydroxide by IUPAC nomenclature.^[98]

Water substance is a term used for hydrogen oxide (H₂O) when one does not wish to specify whether one is speaking of liquid water, steam, some form of ice, or a component in a mixture or mineral.

See also

• 
  Water portal
  

• Chemical bonding of H2O


• Water (data page)


• Dihydrogen monoxide hoax


• Double distilled water


• Electromagnetic absorption by water


• Water model


• Fluid dynamics


• Optical properties of water and ice


• Superheated water


• Hydrogen polyoxide


• Viscosity of water


• Water cluster


• Water dimer


• Water thread experiment

Footnotes

1. 
   ^ ^ab Vienna Standard Mean Ocean Water (VSMOW), used for calibration, melts at 273.1500089(10) K (0.000089(10) °C, and boils at 373.1339 K (99.9839 °C). Other isotopic compositions melt or boil at slightly different temperatures.
   


2. 
   ^
   A commonly quoted value of 15.7 used mainly in organic chemistry for the pK_a of water is incorrect.^[11][12]
   


3. 
   ^ ^ab H+ represents H
   ₃O⁺
   (H
   ₂O)
   _n and more complex ions that form.
   


4. 
   ^ (1-0.95865/1.00000) × 100% = 4.135%
   


5. 
   ^ Adiabatic cooling resulting from the ideal gas law
   


6. 
   ^ The source gives it as 0.0072°C/atm. However the author defines an atmosphere as 1,000,000 dynes/cm² (a bar). Using the standard definition of atmosphere, 1,013,250 dynes/cm², it works out to 0.0073°C/atm
   


7. 
   ^
   Using the fact that 0.5/0.0073 = 68.5
   


8. 
   ^ Both acid and base names exist for water because it is amphoteric (able to react both as an acid or an alkali)
   

References

Notes

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7. 
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17. 
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95. 
    ^ Leigh, Favre & Metanomski 1998, p. 99.
    


96. 
    ^ "Tetrahydropyran". Pubchem. National Institutes of Health. Retrieved 2016-07-31.
    


97. 
    ^ Leigh, Favre & Metanomski 1998, pp. 27–28.
    


98. 
    ^ "Compound Summary for CID 22247451". Pubchem Compound Database. National Center for Biotechnology Information.
    

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  Boyd, Claude E. (2000). "pH, Carbon Dioxide, and Alkalinity". Water Quality. Boston, Massachusetts: Springer. pp. 105–122. doi:10.1007/978-1-4615-4485-2_7. ISBN 9781461544852.
  


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  Campbell, Mary K.; Farrell, Shawn O. (2007). Biochemistry (6th ed.). Cengage Learning. ISBN 978-0-495-39041-1.
  


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  Campbell, Neil A.; Reece, Jane B. (2009). Biology (8th ed.). Pearson. ISBN 978-0-8053-6844-4.
  


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  Campbell, Neil A.; Williamson, Brad; Heyden, Robin J. (2006). Biology: Exploring Life. Boston, Massachusetts: Pearson Prentice Hall. ISBN 978-0-13-250882-7.
  


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  Charlot, G. (2007). Qualitative Inorganic Analysis. Read Books. ISBN 978-1-4067-4789-8.
  


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  Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 978-0-08-037941-8.
  


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  International Union of Pure and Applied Chemistry (2005-11-22). Nomenclature of Inorganic Chemistry: IUPAC Recommendations 2005 (PDF). Royal Society of Chemistry. ISBN 978-0-85404-438-2. Retrieved 2016-07-31.
  


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  Leigh, G. J.; Favre, H. A; Metanomski, W. V. (1998). Principles of chemical nomenclature: a guide to IUPAC recommendations (PDF). Oxford: Blackwell Science. ISBN 978-0-86542-685-6. OCLC 37341352. Archived from the original (PDF) on 2011-07-26.
  


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  Lewis, William C.M.; Rice, James (1922). A System of Physical Chemistry. Longmans, Green and Co.
  


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  Lide, David R. (2003-06-19). CRC Handbook of Chemistry and Physics, 84th Edition. CRC Handbook. CRC Press. ISBN 9780849304842.
  


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  Reece, Jane B.; Urry, Lisa A.; Cain, Michael L.; Wasserman, Steven A.; Minorsky, Peter V.; Jackson, Robert B. (2013-11-10). Campbell Biology (10th ed.). Boston, Mass.: Pearson. ISBN 9780321775658.
  


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  Riddick, John (1970). Organic Solvents Physical Properties and Methods of Purification. Techniques of Chemistry. Wiley-Interscience. ISBN 978-0471927266.
  


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  Sharp, Robert Phillip (1988-11-25). Living Ice: Understanding Glaciers and Glaciation. Cambridge University Press. ISBN 978-0-521-33009-1.
  


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  Zumdahl, Steven S.; Zumdahl, Susan A. (2013). Chemistry (9th ed.). Cengage Learning. ISBN 978-1-13-361109-7.
  

Further reading

• 
  Ben-Naim, A. (2011), Molecular Theory of Water and Aqueous Solutions, World Scientific
  

External links

Wikimedia Commons has media related to Water molecule.

Wikimedia Commons has media related to Water.

• 
  "Water Properties and Measurements". usgs.gov. United States Geological Survey. May 2, 2016. Retrieved August 31, 2016.
  


• 
  Release on the IAPWS Formulation 1995 for the Thermodynamic Properties of Ordinary Water Substance for General and Scientific Use (simpler formulation)


• Online calculator using the IAPWS Supplementary Release on Properties of Liquid Water at 0.1 MPa, September 2008


• 
  Chaplin, Martin. "Water Structure and Science". London South Bank University. Retrieved 2009-07-07.
  


• Calculation of vapor pressure, liquid density, dynamic liquid viscosity, surface tension of water


• Water Density Calculator


• 
  Why does ice float in my drink?, NASA
  

Wikiversity has small "student" steam tables suitable for classroom use.

v t e Water
Overviews	Outline Data Model Properties
States	Liquid Ice Vapor Steam
Forms	Deuterium-depleted Semiheavy Heavy Tritiated Hydronium
On Earth	Cycle Distribution Hydrosphere Hydrology Hydrobiology Origin Pollution Resources management policy Supply
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v t e Hydrogen compounds H3AsO3 H3AsO4 HArF HAt HSO3F HBF4 HBr HBrO HBrO2 HBrO3 HBrO4 HCl HClO HClO2 HClO3 HClO4 HCN HCNO H2CrO4/H2Cr2O7 H2CO3 H2CS3 HF HFΟ HI HIO HIO2 HIO3 HIO4 HMnO4 H2MoO4 HNC NaHCO3 HNCO HNO HNO2 HNO3 H2N2O2 HNO5S H3NSO3 H2O H2O2 H2O3 H3PO2 H3PO3 H3PO4 H4P2O7 H5P3O10 H2PtCl6 H2S H2S2 H2Se H2SeO3 H2SeO4 H4SiO4 H2SiF6 HSCN HNSC H2SO3 H2SO4 H2SO5 H2S2O3 H2S2O6 H2S2O7 H2S2O8 CF3SO3H H2Te H2TeO3 H6TeO6 H4TiO4 H2Po HCo(CO)4 v t e Oxygen compounds AgO Al2O3 AmO2 Am2O3 As2O3 As2O5 Au2O3 B2O3 BaO BeO Bi2O3 BiO2 Bi2O5 BrO2 Br2O3 Br2O5 CO CO2 C2O3 CaO CaO2 CdO CeO2 Ce3O4 Ce2O3 ClO2 Cl2O Cl2O3 Cl2O4 Cl2O6 Cl2O7 CoO Co2O3 Co3O4 CrO3 Cr2O3 Cr2O5 Cr5O12 CsO2 Cs2O3 CuO D2O Dy2O3 Er2O3 Eu2O3 OF 2 O 2F 2 O 3F 2 O 4F 2 FeO Fe2O3 Fe3O4 Ga2O Ga2O3 GeO GeO2 H2O H218O H2O2 HfO2 HgO Hg2O Ho2O3 I2O4 I2O5 I2O6 I4O9 In2O3 IrO2 KO2 K2O2 La2O3 Li2O Li2O2 Lu2O3 MgO Mg2O3 MnO MnO2 Mn2O3 Mn2O7 MoO2 MoO3 Mo2O3 NO NO2 N2O N2O3 N2O4 N2O5 NaO2 Na2O Na2O2 NbO NbO2 Nd2O3 Chemical formulas v t e Oxides Mixed oxidation states Antimony tetroxide (Sb2O4) Cobalt(II,III) oxide (Co3O4) Europium(II,III) oxide (Eu3O4) Iron(II,III) oxide (Fe3O4) Lead(II,IV) oxide (Pb3O4) Manganese(II,III) oxide (Mn3O4) Silver(I,III) oxide (Ag2O2) Triuranium octoxide (U3O8) Carbon suboxide (C3O2) Mellitic anhydride (C12O9) Praseodymium(III,IV) oxide (Pr6O11) Terbium(III,IV) oxide (Tb4O7) +1 oxidation state Copper(I) oxide (Cu2O) Caesium oxide (Cs2O) Dicarbon monoxide (C2O) Dichlorine monoxide (Cl2O) Gallium(I) oxide (Ga2O) Lithium oxide (Li2O) Potassium oxide (K2O) Rubidium oxide (Rb2O) Silver oxide (Ag2O) Thallium(I) oxide (Tl2O) Sodium oxide (Na2O) Water (hydrogen oxide) (H2O) +2 oxidation state Aluminium(II) oxide (AlO) Barium oxide (BaO) Beryllium oxide (BeO) Cadmium oxide (CdO) Calcium oxide (CaO) Carbon monoxide (CO) Chromium(II) oxide (CrO) Cobalt(II) oxide (CoO) Copper(II) oxide (CuO) Europium(II) oxide (EuO) Germanium monoxide (GeO)) Iron(II) oxide (FeO) Lead(II) oxide (PbO) Magnesium oxide (MgO) Manganese(II) oxide (MnO) Mercury(II) oxide (HgO) Nickel(II) oxide (NiO) Nitric oxide (NO) Palladium(II) oxide (PdO) Silicon monoxide (SiO) Strontium oxide (SrO) Sulfur monoxide (SO) Disulfur dioxide (S2O2) Thorium monoxide (ThO) Tin(II) oxide (SnO) Titanium(II) oxide (TiO) Vanadium(II) oxide (VO) Zinc oxide (ZnO) +3 oxidation state Aluminium oxide (Al2O3) Antimony trioxide (Sb2O3) Arsenic trioxide (As2O3) Bismuth(III) oxide (Bi2O3) Boron trioxide (B2O3) Cerium(III) oxide (Ce2O3) Dibromine trioxide (Br2O3) Chromium(III) oxide (Cr2O3) Dinitrogen trioxide (N2O3) Dysprosium(III) oxide (Dy2O3) Erbium(III) oxide (Er2O3) Europium(III) oxide (Eu2O3) Gadolinium(III) oxide (Gd2O3) Gallium(III) oxide (Ga2O3) Holmium(III) oxide (Ho2O3) Indium(III) oxide (In2O3) Iron(III) oxide (Fe2O3) Lanthanum oxide (La2O3) Lutetium(III) oxide (Lu2O3) Manganese(III) oxide (Mn2O3) Neodymium(III) oxide (Nd2O3) Nickel(III) oxide (Ni2O3) Phosphorus trioxide (P4O6) Praseodymium(III) oxide (Pr2O3) Promethium(III) oxide (Pm2O3) Rhodium(III) oxide (Rh2O3) Samarium(III) oxide (Sm2O3) Scandium oxide (Sc2O3) Terbium(III) oxide (Tb2O3) Thallium(III) oxide (Tl2O3) Thulium(III) oxide (Tm2O3) Titanium(III) oxide (Ti2O3) Tungsten(III) oxide (W2O3) Vanadium(III) oxide (V2O3) Ytterbium(III) oxide (Yb2O3) Yttrium(III) oxide (Y2O3) +4 oxidation state Americium dioxide (AmO2) Carbon dioxide (CO2) Carbon trioxide (CO3) Cerium(IV) oxide (CeO2) Chlorine dioxide (ClO2) Chromium(IV) oxide (CrO2) Dinitrogen tetroxide (N2O4) Germanium dioxide (GeO2) Hafnium(IV) oxide (HfO2) Lead dioxide (PbO2) Manganese dioxide (MnO2) Neptunium(IV) oxide (NpO2) Nitrogen dioxide (NO2) Osmium dioxide (OsO2) Plutonium(IV) oxide (PuO2) Praseodymium(IV) oxide (PrO2) Protactinium(IV) oxide (PaO2) Rhodium(IV) oxide (RhO2) Ruthenium(IV) oxide (RuO2) Selenium dioxide (SeO2) Silicon dioxide (SiO2) Sulfur dioxide (SO2) Tellurium dioxide (TeO2) Terbium(IV) oxide (TbO2) Thorium dioxide (ThO2) Tin dioxide (SnO2) Titanium dioxide (TiO2) Tungsten(IV) oxide (WO2) Uranium dioxide (UO2) Vanadium(IV) oxide (VO2) Zirconium dioxide (ZrO2) +5 oxidation state Antimony pentoxide (Sb2O5) Arsenic pentoxide (As2O5) Dinitrogen pentoxide (N2O5) Niobium pentoxide (Nb2O5) Phosphorus pentoxide (P2O5) Protactinium(V) oxide (Pa2O5) Tantalum pentoxide (Ta2O5) Vanadium(V) oxide (V2O5) +6 oxidation state Chromium trioxide (CrO3) Molybdenum trioxide (MoO3) Rhenium trioxide (ReO3) Selenium trioxide (SeO3) Sulfur trioxide (SO3) Tellurium trioxide (TeO3) Tungsten trioxide (WO3) Uranium trioxide (UO3) Xenon trioxide (XeO3) Iridium trioxide (IrO3) +7 oxidation state Dichlorine heptoxide (Cl2O7) Manganese heptoxide (Mn2O7) Rhenium(VII) oxide (Re2O7) Technetium(VII) oxide (Tc2O7) +8 oxidation state Osmium tetroxide (OsO4) Ruthenium tetroxide (RuO4) Xenon tetroxide (XeO4) Iridium tetroxide (IrO4) Hassium tetroxide (HsO4) Related Oxocarbon Suboxide Oxyanion Ozonide Peroxide Superoxide Oxides are sorted by oxidation state. Category:Oxides v t e Hydroxides H2O He LiOH Be(OH)2 B C NH3.H2O O F Ne NaOH Mg(OH)2 Al(OH)3 Si P S Cl HArF (ArHF) KOH Ca(OH)2 Sc(OH)3 Ti V Cr(OH)2 Cr(OH)3 Mn(OH)2 Fe(OH)2 Fe(OH)3 Co(OH)2 Ni(OH)2 CuOH Cu(OH)2 Zn(OH)2 Ga(OH)3 Ge(OH)2 As Se Br Kr RbOH Sr(OH)2 Y(OH)3 Zr(OH)4 Nb Mo Tc Ru Rh Pd AgOH Cd(OH)2 In(OH)3 Sn(OH)2 Sn(OH)4 Sb(OH)3 Te I Xe CsOH Ba(OH)2 * Hf Ta W Re Os Ir Pt Au(OH)3 Hg(OH)2 TlOH Tl(OH)3 Pb(OH)2 Pb(OH)4 Bi(OH)3 Po At Rn Fr Ra ** Rf Db Sg Bh Hs Mt Ds Rg Cn Nh Fl Mc Lv Ts Og ↓ * La(OH)3 Ce(OH)3 Pr(OH)3 Nd(OH)3 Pm(OH)3 Sm(OH)3 Eu(OH)3 Gd(OH)3 Tb(OH)3 Dy(OH)3 Ho(OH)3 Er(OH)3 Tm(OH)3 Yb(OH)3 Lu(OH)3 ** Ac Th(OH)4 Pa UO2(OH)2 Np Pu Am Cm(OH)3 Bk Cf Es Fm Md No Lr v t e Binary compounds of hydrogen Alkali metal hydrides LiH NaH KH RbH CsH Lithium hydride, LiH ionic metal hydride Beryllium hydride Left (gas phase): BeH2 covalent metal hydride Right: (BeH2)n (solid phase) polymeric metal hydride Borane and diborane Left: BH3 (special conditions), covalent metalloid hydride Right: B2H6 (standard conditions), dimeric metalloid hydride Methane, CH4 covalent nonmetal hydride Ammonia, NH3 covalent nonmetal hydride Water, H2O covalent nonmetal hydride Hydrogen fluoride, HF covalent nonmetal hydride Alkaline earth hydrides Monohydrides BeH MgH CaH SrH BaH Dihydrides BeH2 MgH2 CaH2 SrH2 BaH2 Group 13 hydrides Boranes BH3 B2H6 B2H2 B2H4 B4H10 B5H9 B5H11 B6H10 B6H12 B10H14 B18H22 Alanes AlH3 Al2H6 Gallanes GaH3 Ga2H6 Indiganes InH3 In2H6 Thallanes TlH3 Tl2H6 Group 14 hydrides Linear alkanes CH4 C2H6 C3H8 C4H10 C5H12 C6H14 C7H16 C8H18 C9H20 C10H22 more... Linear alkenes C2H4 C3H6 C4H8 C5H10 C6H12 C7H14 C8H16 C9H18 C10H20 more... Linear alkynes C2H2 C3H4 C4H6 C5H8 C6H10 C7H12 C8H14 C9H16 C10H18 more... Silanes SiH4 Si2H6 Si3H8 Si4H10 Si5H12 Si6H14 Si7H16 Si8H18 Si9H20 Si10H22 more... Silenes Si2H4 Silynes Si2H2 SiH Germanes GeH4 Ge2H6 Ge3H8 Ge4H10 Ge5H12 Stannanes SnH4 Sn2H6 Plumbanes PbH4 CH CH2 CH3 C2H Cycloalkanes Cycloalkenes Annulenes Many more Pnictogen hydrides Azanes NH3 N2H4 N3H5 N4H6 N5H7 N6H8 N7H9 N8H10 N9H11 N10H12 more... Azenes N2H2 N3H3 N4H4 Phosphanes PH3 P2H4 P3H5 P4H6 P5H7 P6H8 P7H9 P8H10 P9H11 P10H12 more... Phosphenes P2H2 P3H3 P4H4 Arsanes AsH3 As2H4 Stibanes SbH3 Bismuthanes BiH3 HN3 NH radical Hydrogen chalcogenides Polyoxidanes H2O H2O2 H2O3 H2O4 H2O5 H2O6 H2O7 H2O8 H2O9 H2O10 more... Polysulfanes H2S H2S2 H2S3 H2S4 H2S5 H2S6 H2S7 H2S8 H2S9 H2S10 more... Selanes H2Se H2Se2 Tellanes H2Te H2Te2 Polanes PoH2 HO HO2 HO3 H2O+–O– H2S=S (HS)2S+–S– HS HDO D2O T2O Hydrogen halides HF HCl HBr HI HAt Transition metal hydrides ScH2 YH2 YH3 TiH2 ZrH2 HfH2 VH VH2 NbH NbH2 TaH CrH CrH2 CrHx NiH PdHx (x < 1) FeH FeH2 FeH5 CuH ZnH2 CdH2 HgH2 Lanthanide hydrides LaH2 LaH3 LaH10 CeH2 CeH3 PrH2 PrH3 NdH2 NdH3 SmH2 SmH3 EuH2 GdH2 GdH3 TbH2 TbH3 DyH2 DyH3 HoH2 HoH3 ErH2 ErH3 TmH2 TmH3 YbH2 YbH2.5 LuH2 LuH3 Actinide hydrides AcH2 ThH2 Th4H15 PaH3 UH3 NpH2 NpH3 PuH2 PuH3 AmH2 AmH3 CmH2

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