PH

(CC) Drawing: Milton Beychok
The pH scale

The pH scale measures the acidity or alkalinity of an aqueous solution. Values for pH range from 0 (strongly acidic) to 14 (strongly alkaline or basic). The pH of a neutral solution (neither acid or basic), such as pure water at room temperature and atmospheric pressure is 7, whereas the pH of an acidic solution is less than 7 and the pH of a basic solution is greater than 7. The pH scale is logarithmic which means that a difference of one pH unit is equivalent to a ten-fold difference in hydrogen ion concentration. The notation pH is sometimes referred to as the power of hydrogen or the potential of hydrogen.

The traditional way to determine whether a solution is acidic or basic is by wetting litmus paper with the solution. If the wet litmus paper turns red, the solution has a pH less than 7 and is acidic. If it turns blue, the solution has a pH greater than 7 and is acidic. Measuring the actual pH value of a solution is more accurately done with a pH meter.

The pH scale was originally defined by Danish biochemist Søren Peter Lauritz Sørensen in 1909, who wrote it as P_H. It was subsequently changed to the modern notation of pH in 1920 by William Mansfield Clark, an American biochemist, for typographical convenience in his book The Determination of Hydrogen Ions.

Definitions and discussion

H+ and OH- ions molar concentrations vs. pH H+ concentration (mole/litre OH- concentration (mole/litre) pH 1 0.00000000000001 0 0.1 0.0000000000001 1 0.01 0.000000000001 2 0.001 0.00000000001 3 0.0001 0.0000000001 4 0.00001 0.000000001 5 0.000001 0.00000001 6 0.0000001 0.0000001 7 0.00000001 0.000001 8 0.000000001 0.00001 9 0.0000000001 0.0001 10 0.00000000001 0.001 11 0.000000000001 0.01 12 0.0000000000001 0.1 13 0.00000000000001 1 14

A molar concentration of a compound, in moles per litre of solution, is commonly written as the symbol of the compound surrounded by square brackets. Thus, the hydrogen (H⁺) ion concentration in an aqueous solution is written simply as [H⁺] or as hydronium [H₃O⁺] and both describe the equivalent entity.

For very dilute solutions, the pH value can be defined by this simple expression:

(1)      ${\rm {pH}}=-\log _{10}\left[{\rm {H^{+}}}\right]=\log _{10}{\frac {1}{\left[{\rm {H^{+}}}\right]}}$

and the corresponding expression for the hydroxide (OH^-) ions can be expressed as:

(2)      ${\rm {pOH}}=-\log _{10}\left[{\rm {OH^{-}}}\right]=\log _{10}{\frac {1}{\left[{\rm {OH^{-}}}\right]}}$

Since the product of the concentration of hydrogen ions and the concentration of hydroxide ions is a constant, namely:

(3)       $\left[{\rm {H^{+}}}\right]\left[{\rm {OH^{-}}}\right]=1\times 10^{-14}$

taking logarithms gives:

(4)       $\left({\rm {pH}}+{\rm {pOH}}\right)=14$

The mid-point of 7 in the pH scale indicates ionic neutrality of the solution, namely when [H⁺] equals [OH⁻] (see the adjacent table).

As the theory behind chemical reactions became more sophisticated, the definition of pH was reexamined. Specifically, as the role of electrical charge in chemical reactions became better understood, the definition of pH was changed to refer to the active hydrogen ion concentration. The more theoretical definition of pH, while not generally covered in many introductory chemistry textbooks, is the definition adopted by the International Union of Pure and Applied Chemistry (IUPAC):

(5)       ${\rm {pH}}=-\log _{10}\,(a_{\rm {H^{+}}})\equiv -\log _{10}\,\left(\gamma \,\left[{\rm {H^{+}}}\right]\right)$

where $a_{\rm {H^{+}}}$ is the hydrogen ion activity and the factor $\gamma$ is the hydrogen ion activity coefficient.

Only in dilute solutions (about 0.001 moles per litre or less) are all anion and cations so far apart that they are free to be at their maximum activity where:

(6)       $\gamma =1\,$   and thus   $a_{\rm {H^{+}}}=\left[{\rm {H^{+}}}\right]\,$

At higher acid and base concentrations, the space between cations and anions decreases, so that they begin to obstruct each other and shield each others charge. Thus, the mobility of the any particular ion is impaired by interactions with other ions and their associated electrical fields. These local electric field interactions affect the extent to which the ions can participate in chemical reactions, and give an apparent concentration that is always smaller than the real concentration, that is, the dimensionless parameter γ becomes less than unity. In other words, the ion activity is "slowed down" and [H⁺] becomes greater than a_H⁺. The coefficient γ (ion activity over concentration) decreases with the increasing acid concentration. Therefore, for acid concentrations greater than about 0.001 moles per liter, it is advisable to use activities instead of concentrations in order to accurately predict pH.

pH of some common substances

The two tables below list the pH ranges for each of a number of fairly common substances:

Substance pH Human gastric juice 1.0 − 3.0 Car battery acid 1.1 − 1.7 Lime juice 1.8 − 2.0 Soft drinks 2.0 − 4.0 Lemon juice 2.2 − 2.4 Vinegar 2.4 − 3.4 Apple juice 2.9 − 3.3 Wine 3.4 − 3.7 Tomato juice 4.0 − 4.4 Beer 4.0 − 5.0 Coffee 5.0 − 6.5 Rainwater 5.1 − 5.6		Substance pH Banana juice 4.5 − 4.7 Human urine 4.8 − 8.4 Cow milk 6.3 − 6.6 Human saliva 6.5 − 7.5 Soap suds 7.0 − 10.0 Human blood plasma 7.3 − 7.5 Sea water 7.4 − 8.3 Egg white 7.6 − 8.0 Baking soda solution 8.3 − 8.8 Milk of Magnesia 10.6 − 10.7 Household ammonia 11.0 − 12.0 Household lye 13.6 − 14.0
Notes: (1) Car battery acid is an aqueous solution of 65 weight % sulfuric acid, H2SO4 (2) Baking soda solution is an aqueous solution of sodium bicarbonate, NaHC03 (3) Milk of Magnesia is an aqueous solution of magnesium hydroxide, Mg(OH)2 (4) Household ammonia is ammonium hydroxide, NH4OH, a dilute aqueous     solution of ammonia (5) Household lye is an aqueous solution of sodium hydroxide, NaOH