### pH

pH (potential of hydrogen) is a measure of the activity of hydrogen ions (H+) in a solution and, therefore, its acidity or alkalinity. In aqueous systems, the hydrogen ion activity is dictated by the dissociation constant of water (Kw = 1.011 x 10-14 at 25 °C) and interactions with other ions in solution. Due to this dissociation constant a neutral solution (hydrogen ion activity equals hydroxide ion activity) has a pH of approximately 7. Aqueous solutions with pH values lower than 7 are considered acidic, while pH values higher than 7 are considered alkaline.

The concept was introduced by S.P.L. Sorensen in 1909, and is purported to mean "pondus hydrogenii" in Dutch. However, most other sources attribute the name to the French term pouvoir hydrogène. In English, pH can stand for "hydrogen power," "power of hydrogen," or "potential of hydrogen." All of these terms are technically correct.

### Definition

Though a pH value has no unit, it is not an arbitrary scale; the number arises from a definition based on the activity of hydrogen ions in the solution.

The precise formula for calculating pH is: aH+ denotes the activity of H+ ions , and is unitless. In dilute solutions (like river or tap water) the activity is approximately equal to the numeric value of the concentration of the H+ ion, denoted as [H+] (or more accurately written, [H3O+]), measured in moles per litre (also known as molarity): Therefore, it is often convenient to define pH as: For both definitions, log10 denotes the base-10 logarithm, therefore pH defines a logarithmic scale of acidity. For example, a solution of pH = 8.2 will have an [H+] activity (concentration) of 10-8.2 mol/L, or about 6.31 x 10-9 mol/L; a solution with an [H+] activity of 4.5 x 10-4 mol/L will have a pH value of -log10(4.5 x 10-4), or about 3.35.

In solution at 25 °C, a pH of 7 indicates neutrality (i.e. the pH of pure water) because water naturally dissociates into H+ and OH- ions with equal concentrations of 1 x 10-7 mol/L. A lower pH value (for example pH 3) indicates increasing strength of acidity, and a higher pH value (for example pH 11) indicates increasing strength of alkalinity.

Neutral pH is not exactly 7; this would imply that the H+ ion concentration is exactly 1x10-7 mol/L, which is not the case. The value is close enough, however, for neutral pH to be 7.00 to two significant figures, which is near enough for most people to assume that it is exactly 7. At temperatures other than 25 °C, or room temperature, the pH of pure water will not be 7. (Note also that pure water, when exposed to the atmosphere, will take in carbon dioxide, some of which reacts with water to form carbonic acid and H+, thereby lowering the pH to about 5.7.)

Most substances have a pH in the range 0 to 14, although extremely acidic or basic substances may have pH less than 0 or greater than 14.

### Cell potential

pH can also be measured by measuring the cell potential of the sample: where epsilon (ε) is the electromotive force (EMF) or cell potential of a galvanic cell.

The formula for pH was derived from the application of the Nernst Equation to concentration cells, or galvanic cells where the half cells are at different concentrations. In the Nernst Equation,

#### However, in a concentration cell both eo are equal so the equation becomes By using the standard hydrogen electrode, with H2 gas at 1 atm and an unknown molarity of H+ ions, and in which 2 moles of electrons are transferred for every mole of reaction, the equation may be set up as follows: Arbitrarily, the potential of hydrogen, or pH, is defined as -\log ([\mbox{H}+]). Therefore,

pH = - log10[H + ]

or, by substitution, The "pH" of any other substance may also be found (e.g. the potential of silver ions, or pAg+) by deriving a similar equation using the same process. These other equations for potentials will not be the same, however, as the number of moles of electrons transferred (n) will differ for the different reactions.

### Measuring

pH can be measured:

- by addition of a pH indicator into the studying solution. The indicator color varies depending on the pH of the solution. Using indicators, qualitative determinations can be made with universal indicators that have broad color variability over a wide pH range and quantitative determinations can be made using indicators that have strong color variability over a small pH range. Extremely precise measurements can be made over a wide pH range using indicators that have multiple equilibriums (ie H2I) in conjunction with spectrophotometric methods to determine the relative abundance of each pH dependent component that make up the color of solution.
- by using a pH meter together with pH-selective electrodes (pH glass electrode, hydrogen electrode, quinhydrone electrode, ion sensitive field effect transistor and other). ### pOH

There is also pOH, in a sense the opposite of pH, which measures the concentration of OH- ions. Since water self ionizes, and notating [OH-] as the concentration of hydroxide ions, we have (*)

where Kw is the ionization constant of water.

Now, since by logarithmic identities, we then have the relationship: and thus
pOH = -log10 aOH- = 14 + log10 aH+ = 14 - pH (*)

(*) This formula is valid exactly for temperature = 298.15 K (25 °C) only, acceptable for most lab calculations.

### Calculation of pH for weak and strong acids

Values of pH for weak and strong acids can be approximated using certain assumptions.

Under the Bronsted-Lowry theory, stronger or weaker acids are a relative concept. But here we define a strong acid as a species which is a much stronger acid than the hydronium (H3O+) ion. In that case the dissociation reaction (strictly HX+H2O<-->H3O++X- but simplified as HX<-->H++X-) goes to completion, i.e. no unreacted acid remains in solution. Dissolving the strong acid HCl in water can therefore be expressed:

HCl(aq) --> H+ + Cl-

This means that in a 0.01 mol/L solution of HCl it is approximated that there is a concentration of 0.01 mol/L dissolved hydrogen ions. From above, the pH is: pH = -log10 [H+]:

pH = -log (0.01)

which equals 2.

For weak acids, the dissociation reaction does not go to completion. An equilibrium is reached between the hydrogen ions and the conjugate base. The following shows the equilibrium reaction between methanoic acid and its ions:

HCOOH(aq) <-->H+ + HCOO-

It is necessary to know the value of the equilibrium constant of the reaction for each acid in order to calculate its pH. In the context of pH, this is termed the acidity constant of the acid but is worked out in the same way:

Ka = [hydrogen ions][acid ions] / [acid]

For HCOOH, Ka = 1.6 x 10-4

When calculating the pH of a weak acid, it is usually assumed that the water does not provide any hydrogen ions. This simplifies the calculation, and the concentration provided by water, 1x10-7 mol, is usually insignificant.

With a 0.1 mol/L solution of methanoic acid (HCOOH), the acidity constant is equal to:

Ka = [H+][HCOO-] / [HCOOH]

Given that an unknown amount of the acid has dissociated, [HCOOH] will be reduced by this amount, while [H+] and [HCOO-] will each be increased by this amount. Therefore, [HCOOH] may be replaced by 0.1 - x, and [H+] and [HCOO-] may each be replaced by x, giving us the following equation: Solving this for x yields 3.9×10-3, which is the concentration of hydrogen ions after dissociation. Therefore the pH is -log(3.9x10-3), or about 2.4.

### Indicators

An indicator is used to measure the pH of a substance. Common indicators are litmus paper, phenolphthalein, methyl orange, phenol red, and bromothymol blue.

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