Difference between revisions of "Self-ionization of water"

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The self-ionization of water (also autoionization of water, and autodissociation of water) is the chemical reaction in which two water molecules react to produce a hydronium ion (H3O+) and a hydroxide ion (OH):

2 H2O (l) 15px H3O+ (aq) + OH (aq)

It is an example of autoprotolysis, and relies on the amphoteric nature of water.

Water, however pure, is not a simple collection of H2O molecules. Even in "pure" water, sensitive equipment can detect a very slight electrical conductivity of 0.055 µS·cm−1. According to the theories of Svante Arrhenius, this must be due to the presence of ions.

Concentration and frequency

The preceding reaction has a chemical equilibrium constant of Keq = ([H3O+] [OH]) / [H2O]2 = 3.23 × 10−18. So the acidity constant which is Ka = Keq × [H2O] = ([H3O+] [OH]) / [H2O] = 1.8 × 10−16.[1] For reactions in water (or diluted aqueous solutions), the molarity (a unit of concentration) of water, [H2O], is practically constant and is omitted from the acidity constant expression by convention. The resulting equilibrium constant is called the ionization constant, dissociation constant, or self-ionization constant, or ion product of water and is symbolized by Kw.

Kw = Ka [H2O] = Keq [H2O]2 = [H3O+] [OH]
where
[H3O+] = molarity of hydrogen or hydronium ion, and
[OH] = molarity of hydroxide ion.

At Standard Ambient Temperature and Pressure (SATP), about 25 °C (298 K), Kw = [H3O+][OH] = 1.0×10−14. Pure water ionizes or dissociates into equal amounts of H3O+ and OH, so their molarities are equal:

[H3O+] = [OH].

At SATP, the concentrations of hydroxide and hydronium are both very low at 1.0 × 10−7 mol/L and the ions are rarely produced: a randomly selected water molecule will dissociate within approximately 10 hours.[2] Since the concentration of water molecules in water is largely unaffected by dissociation and [H2O] equals approximately 56 mol/l, it follows that for every 5.6×108 water molecules, one pair will exist as ions. Any solution in which the H3O+ and OH concentrations equal each other is considered a neutral solution. Absolutely pure water is neutral, although even trace amounts of impurities could affect these ion concentrations and the water may no longer be neutral. Kw is sensitive to both pressure and temperature; it increases when either increases.

Deionized water (also called DI water) is water that has had most impurity ions common in tap water or natural water sources (such as Na+ and Cl) removed by means of distillation or some other water purification method. Removal of all ions from water is next to impossible, since water self-ionizes quickly to reach equilibrium.

Dependence on temperature and pressure

File:Temperature dependence water ionization.svg
Temperature dependence of the water ionization constant at 25 MPa
File:Pressure dependence water ionization pKw on P.svg
Pressure dependence of the water ionization constant at 25 °C
By definition, pKw = −log10 Kw. At SATP, pKw = −log10 (1.0×10−14) = 14.0. The value of pKw varies with temperature. As temperature increases, pKw decreases; and as temperature decreases, pKw increases (for temperatures up to about 250 °C). This means that ionization of water typically increases with temperature.

There is also a (usually small) dependence on pressure (ionization increases with increasing pressure). The dependence of the water ionization on temperature and pressure has been well investigated and a standard formulation exists[3].

Acidity

pH is a logarithmic measure of the acidity (or alkalinity) of an aqueous solution. By definition, pH = −log10 [H3O+]. Since [H3O+] = [OH] in a neutral solution, by mathematics, for a neutral aqueous solution pH = 7 at SATP.

Self-ionization is the process that determines the pH of water. Since the concentration of hydronium at SATP (25 °C) is approximately 1.0×10−7mol/l, the pH of pure liquid water at this temperature is 7. Since Kw increases as temperature increases, hot water has a higher concentration of hydronium than cold water, but this does not mean it is more acidic, as the hydroxide concentration is also higher by the same amount.

Mechanism

Geissler et al. have determined that electric field fluctuations in liquid water cause molecular dissociation.[4] They propose the following sequence of events that takes place in about 150 fs: the system begins in a neutral state; random fluctuations in molecular motions occasionally (about once every 10 hours per water molecule) produce an electric field strong enough to break an oxygen-hydrogen bond, resulting in a hydroxide (OH) and hydronium ion (H3O+); the proton of the hydronium ion travels along water molecules by the Grotthuss mechanism; and a change in the hydrogen bond network in the solvent isolates the two ions, which are stabilized by solvation.

Within 1 picosecond, however, a second reorganization of the hydrogen bond network allows rapid proton transfer down the electric potential difference and subsequent recombination of the ions. This timescale is consistent with the time it takes for hydrogen bonds to reorient themselves in water.[5][6][7]

Isotope effects

Heavy water, D2O, self-ionizes less than normal water, H2O; oxygen forms a slightly stronger bond to deuterium because the larger mass of deuterium difference results in a lower zero-point energy, a quantum mechanical effect. The following table compares the values of pKw for H2O and D2O.[8]

T (°C) H2O D2O
10 14.5346 15.439
20 14.1669 15.049
25 13.9965 14.869
30 13.8330 14.699
40 13.5348 14.385
50 13.2617 14.103

See also

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References

  1. McMurry, John. (2004) Organic Chemistry, pg 44
  2. Eigen, M.; de Maeyer, L. (1955). "Untersuchungen über die Kinetik der Neutralisation I". Z. Elektrochem. 59: 986. 
  3. International Association for the Properties of Water and Steam (IAPWS)
  4. Geissler, P. L.; Dellago, C.; Chandler, D.; Hutter, J.; Parrinello, M. (2001). "Autoionization in liquid water". Science. 291 (5511): 2121–2124. doi:10.1126/science.1056991. PMID 11251111. 
  5. Stillinger, F. H. (1975). "Theory and Molecular Models for Water". Adv. Chem. Phys. 31: 1. doi:10.1002/9780470143834.ch1. 
  6. Rapaport, D. C. (1983). "Hydrogen bonds in water". Mol. Phys. 50: 1151. doi:10.1080/00268978300102931. 
  7. Chen, S.-H. & Teixeira, J. (1986). "Structure and Dynamics of Low-Temperature Water as Studied by Scattering Techniques". Adv. Chem. Phys. 64: 1. doi:10.1002/9780470142882.ch1. 
  8. Lide, D. R. (Ed.) (1990). CRC Handbook of Chemistry and Physics (70th Edn.). Boca Raton (FL):CRC Press. 

External links

cs:Autoionizace vody da:Vands autoprotolyse el:Αυτοϊοντισμός νερού es:Autoionización del agua fr:Autoprotolyse it:Autoionizzazione dell'acqua mk:Автојонизација на водата ja:自己解離 pl:Autodysocjacja wody pt:Autoionização da água fi:Autoprotolyysi sv:Vattnets autoprotolys zh:水的电离