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Solution Concentration and pH Calculations

Calculate molarity, mass-fraction conversions, dilution, and pH. Worked examples explain strong-base mixtures, very dilute acids, and temperature assumptions.

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Solution Concentration and pH Calculations

Concentration calculations describe how much solute is present in a given amount of solution. pH calculations describe acidity on a logarithmic scale. Keep these two ideas separate: the concentration of an acid is not always equal to the hydrogen-ion concentration.

1. Molar concentration and mass fraction

Molar concentration, also called molarity, is

c=nV.c=\frac{n}{V}.

Here nn is the amount of solute in moles and VV is the final solution volume in liters. The volume of water added is not necessarily the final volume of the solution.

If the solution density ρ\rho is in g/mL, the solute molar mass MM is in g/mol, and the mass fraction ww is a decimal, then

c=1000ρwMin mol/L.c=\frac{1000\rho w}{M} \quad\text{in mol/L}.

For a mass percentage of 98%, enter w=0.98w=0.98, not 9898. The factor 10001000 converts a one-liter sample to milliliters: its mass is 1000ρ1000\rho grams, of which 1000ρw1000\rho w grams is solute.

Example: converting a mass percentage

A sulfuric acid solution has density 1.84 g/mL1.84\ \mathrm{g/mL} and mass fraction 0.980.98. Using a molar mass of 98 g/mol98\ \mathrm{g/mol},

c=1000×1.84×0.9898=18.4 mol/L.c=\frac{1000\times1.84\times0.98}{98} =18.4\ \mathrm{mol/L}.

This gives the analytical concentration of sulfuric acid. It does not give the solution's pH, and the example is a calculation rather than a procedure for handling concentrated acid.

2. Preparing a measured solution volume

For a solution of accurately known concentration, a volumetric flask provides a calibrated final volume. Follow the laboratory's procedure and safety instructions.

Illustration of weighing a solid, dissolving it, transferring and rinsing, making up to the calibration mark, and mixing.

For a suitable solid solute, the usual sequence is to weigh it, dissolve it in some solvent, transfer the solution quantitatively, add the rinsings, make up to the mark, and mix. Let the solution reach the appropriate calibration temperature before setting the final volume.

Read the bottom of a clear, concave meniscus at eye level. With the amount of solute fixed, filling above the mark makes the concentration too low; filling below it makes the concentration too high.

For dilution without loss or reaction of the solute,

c1V1=c2V2.c_1V_1=c_2V_2.

Here V2V_2 is the final solution volume, not the volume of solvent added.

3. What pH and pOH mean

Formally, pH is defined using the dimensionless hydrogen-ion activity:

pH=−log⁡10aH+.\mathrm{pH}=-\log_{10}a_{\mathrm{H^+}}.

For dilute solutions, introductory problems often approximate activity using the numerical concentration in mol/L and write pH≈−log⁡10[H+]\mathrm{pH}\approx-\log_{10}[H^+]. In water, H+H^+ is shorthand for hydrated hydrogen ions, commonly represented as H3O+H_3O^+.

Similarly, pOH≈−log⁡10[OH−]\mathrm{pOH}\approx-\log_{10}[OH^-]. At 25∘C25^\circ\mathrm C, the usual dilute-solution approximation gives

pH+pOH≈14.00.\mathrm{pH}+\mathrm{pOH}\approx14.00.
Solution at 25∘C25^\circ\mathrm CIon concentrationspH
Acidic[H+]>[OH−][H^+]>[OH^-]Below 7
Neutral[H+]=[OH−][H^+]=[OH^-]Approximately 7
Basic[H+]<[OH−][H^+]<[OH^-]Above 7

The neutral pH depends on temperature because water's ionization equilibrium changes. Also, 0–14 is a familiar teaching range, not an absolute limit on pH.

4. Mixing strong acids and bases

Do not average pH values. First convert concentrations to amounts, account for neutralization, and then calculate the concentration of the excess ions in the final volume.

For the simple formulas below, assume strong acids or bases dissociate as specified, the solution volumes add, and other reactions and water's contribution are negligible.

  • Mixing acids: add the amounts of H+H^+ supplied, then divide by the total volume.
  • Mixing bases: add the amounts of OH−OH^- supplied, divide by the total volume, and find pOH before pH.
  • Mixing an acid and a base: subtract the reacting amounts. If acid is in excess, use [H+]≈(nH+−nOH−)/Vtotal[H^+]\approx(n_{H^+}-n_{OH^-})/V_{\mathrm{total}}. If base is in excess, use the corresponding excess amount of OH−OH^-.

Use liters when converting mol/L to moles. At exact neutralization of a strong acid and strong base, water's equilibrium determines the pH. Weak acids, weak bases, buffers, and extremely dilute mixtures need an equilibrium calculation rather than these simple excess-ion formulas.

Example: equal volumes of two NaOH solutions

At 25∘C25^\circ\mathrm C, mix equal volumes of NaOH solutions with pH 12 and pH 10. In the dilute-solution approximation,

[OH−]1=10−2 mol/L,[OH−]2=10−4 mol/L.[OH^-]_1=10^{-2}\ \mathrm{mol/L}, \qquad [OH^-]_2=10^{-4}\ \mathrm{mol/L}.

The concentration after mixing is

[OH−]mix=10−2+10−42=5.05×10−3 mol/L.[OH^-]_{\mathrm{mix}} =\frac{10^{-2}+10^{-4}}{2} =5.05\times10^{-3}\ \mathrm{mol/L}.

Thus pOH≈2.30\mathrm{pOH}\approx2.30 and pH≈11.70\mathrm{pH}\approx11.70, not the arithmetic mean of 12 and 10.

Example: an extremely dilute acid

For 1.0×10−8 mol/L1.0\times10^{-8}\ \mathrm{mol/L} HCl at 25∘C25^\circ\mathrm C, taking −log⁡10(10−8)-\log_{10}(10^{-8}) gives 8, but that calculation neglects the hydrogen ions supplied by water.

Using charge balance and water's ionization equilibrium, with concentrations entered numerically in mol/L,

[H+]=Ca+Ca2+4Kw2,[H^+]=\frac{C_a+\sqrt{C_a^2+4K_w}}{2},

where Ca=1.0×10−8C_a=1.0\times10^{-8} and Kw≈1.0×10−14K_w\approx1.0\times10^{-14}. This gives [H+]≈1.05×10−7 mol/L[H^+]\approx1.05\times10^{-7}\ \mathrm{mol/L} and pH approximately 6.98. The solution is slightly acidic, not basic.

Further reading

Content reviewed: 9 September 2026.