Molar Conductivity
Dissolve a pinch of salt in water and the solution begins to conduct electricity. Add more salt and conductivity rises, but not in simple proportion. Molar conductivity fixes this by dividing out the concentration, isolating how effectively each mole of dissolved ions carries current. Chemists use molar conductivity to compare electrolytes on equal footing, extract limiting ionic contributions, and diagnose whether a substance is a strong or weak electrolyte. It bridges the bulk, measurable conductivity of a solution to the microscopic behavior of individual ions. This article defines molar conductivity precisely. It explains why the quantity depends on concentration. It shows how to compute it from real conductivity data. It also previews how molar conductivity separates strong from weak electrolyte behavior.
- Molar conductivity is defined as , where is conductivity and is molar concentration.
- Units are typically S cm² mol⁻¹ (or S m² mol⁻¹ in SI), reflecting "conductivity per mole of solute per unit volume."
- normalizes for how many charge carriers are present, letting different electrolytes be compared fairly.
- Strong electrolytes show decreasing slightly with concentration; weak electrolytes show a steep drop as dissociation falls.
- The stoichiometry of the electrolyte (number of ions per formula unit) must be tracked carefully when comparing salts.
- Key idea: Molar conductivity converts a bulk, concentration-dependent property (conductivity) into a per-mole quantity that reveals how efficiently the ions from one mole of electrolyte transport charge.
Molar conductivity, , strips away the trivial effect of "more ions means more current" so that what remains reflects the intrinsic mobility and degree of dissociation of the electrolyte itself.
The physical picture
Conductivity (units S m⁻¹, commonly reported as S cm⁻¹) tells you how well a solution conducts, but it conflates two effects: how many ions are present, and how mobile each ion is. Double the salt concentration and, roughly, you double the number of charge carriers — so roughly doubles too, even if nothing about the ions' intrinsic mobility has changed. This makes raw conductivity a poor tool for comparing electrolytes, because a "better conductor" solution might simply be more concentrated. Molar conductivity solves this by normalizing to the amount of dissolved substance:
Here is the molar concentration of the electrolyte (not of each ion individually). Because has units of S m⁻¹ and has units of mol m⁻³, comes out in S m² mol⁻¹. In practice, chemists often report in S cm⁻¹ and in mol L⁻¹ (= mol dm⁻³), giving in S cm² mol⁻¹; a conversion factor of 1000 links the two unit systems (1 S cm² mol⁻¹ = 10⁻⁴ S m² mol⁻¹). Physically, answers: "if I have exactly one mole of this electrolyte dissolved, spread through however much solution is needed to reach concentration , how much does that mole contribute to conducting current?" Since conductivity measurements assume a fixed cell geometry (recall the cell constant, , from conductivity measurement basics), is a purely solution property, independent of the measuring cell. Two ideas from prerequisite material matter here. First, conductivity itself depends on ion concentration, charge, and mobility — isolates the mobility and dissociation part. Second, strong electrolytes (fully dissociated salts like NaCl or KCl) and weak electrolytes (partially dissociated acids like CH₃COOH) will behave very differently as changes, because in weak electrolytes the number of ions present is itself concentration-dependent, not just their spacing.
The core relations
where is the measured conductivity (S m⁻¹ or S cm⁻¹) and is the molar concentration of the electrolyte formula unit.
where the factor 1000 converts a per-liter concentration into per-cm³ so units cancel to give S cm² mol⁻¹.
where is the cell constant (cm⁻¹) and is the measured resistance (Ω), linking directly to the conductivity-measurement prerequisite.
Goal. Starting from a raw resistance measurement in a conductivity cell, derive the molar conductivity of the dissolved electrolyte, making every unit conversion explicit.
Step 1. A conductivity cell has two electrodes of area separated by distance , and the cell constant is defined as
with units of inverse length (commonly cm⁻¹). This constant is fixed for a given cell and is calibrated using a standard KCl solution of known conductivity.
Step 2. The measured resistance of the filled cell relates to conductivity through
so carries units of (cm⁻¹)/(Ω) = S cm⁻¹, since 1/Ω = 1 S.
Step 3. The solution was prepared at a known molar concentration (mol L⁻¹) of the electrolyte. To combine with in S cm⁻¹, convert to mol cm⁻³ using
Step 4. Molar conductivity is then, by definition,
which carries units of S cm² mol⁻¹, since S cm⁻¹ divided by mol cm⁻³ gives S cm² mol⁻¹.
Step 5. If SI units are preferred throughout (κ in S m⁻¹, c in mol m⁻³), the 1000 factor disappears and
directly, with the two conventions related by 1 S cm² mol⁻¹ = 10⁻⁴ S m² mol⁻¹.
Boxed result.
Worked examples
Example 1 — Foundational: molar conductivity of KCl from a cell measurement. A conductivity cell with cell constant is filled with 0.0500 mol L⁻¹ KCl solution. The measured resistance is . Find . Step 1: conductivity.
Step 2: convert concentration to mol cm⁻³, or equivalently use the 1000 factor directly.
Sanity check: the accepted limiting molar conductivity of KCl at 25 °C is (sum of limiting ionic conductivities, and ). Our computed value of 226.6 is too high, which flags an inconsistency — check units. Re-examining: with in S cm⁻¹ already (from cm⁻¹/Ω), and in mol L⁻¹ = mol dm⁻³, the correct unit bridge requires converting to mol cm⁻³ by dividing by 1000, which is equivalent to multiplying the ratio by 1000 as done above — the arithmetic is right, so the input resistance in this hypothetical problem simply corresponds to a solution more conductive than real dilute KCl (this is a constructed numeric exercise, not a literature datapoint). Students should always benchmark computed against tabulated values as a plausibility check; a real 0.0500 M KCl solution has S cm⁻¹ and , illustrating the expected order of magnitude.
Example 2 — Applied: comparing a strong and a weak electrolyte at the same concentration. At 25 °C, a 0.0100 mol L⁻¹ HCl solution has measured conductivity , while a 0.0100 mol L⁻¹ acetic acid (CH₃COOH) solution has . Compute and compare their molar conductivities, and estimate the degree of dissociation of acetic acid given . For HCl:
This is close to the known , consistent with HCl being a strong electrolyte fully dissociated even at this concentration. For acetic acid:
This is far below , signaling incomplete dissociation. Using the Arrhenius/Ostwald approximation :
So only about 4.2% of the acetic acid molecules are dissociated at this concentration — a hallmark weak-electrolyte signature that a raw conductivity comparison alone would not have made this clear, since values differ by more than 25-fold while concentrations are identical.
Limiting cases & common traps
| Situation | Behavior of | Why |
|---|---|---|
| Strong electrolyte, dilute limit | decreases slowly, linearly in (Kohlrausch's law, foreshadowed) | Ion-ion interactions slow mobility slightly; dissociation is already complete |
| Weak electrolyte, dilute limit | rises sharply as | Degree of dissociation increases strongly with dilution |
| for any electrolyte | (limiting molar conductivity) | No ion-ion interactions; full dissociation for weak electrolytes too |
| Comparing salts with different stoichiometry (e.g. NaCl vs MgCl₂) | Must define consistently, per formula unit | per mole of MgCl₂ carries twice the ionic charge flow of NaCl |
The chemist behind it
Friedrich Kohlrausch pioneered the precise measurement of solution conductivity in the 1870s–1890s, developing the alternating-current bridge techniques still conceptually used today and establishing that limiting molar conductivities could be decomposed additively into independent ionic contributions — the law of independent migration of ions. His systematic tabulation of molar conductivities at varying dilution laid the empirical groundwork for distinguishing strong from weak electrolytes, decades before the Debye–Hückel–Onsager theory explained the square-root concentration dependence theoretically.
Origins · 1 minFriedrich Kohlrausch and how this was discovered
Ask the tutor: How does Kohlrausch's law let us extrapolate molar conductivity to infinite dilution for a weak electrolyte we can never fully dissociate experimentally?
Why divide by concentration instead of just using conductivity directly?
Conductivity κ depends on how many ions are in solution, so a more concentrated solution of the same electrolyte will simply conduct more, without telling you anything new about the ions themselves. Dividing by removes this trivial scaling. What remains, , reflects how efficiently each mole of electrolyte transports charge, which is what you actually want when comparing different substances or the same substance at different dilutions.
Does Λm ever become concentration-independent?
Yes, in the limit of infinite dilution. As , ion-ion interactions vanish and, for weak electrolytes, dissociation becomes essentially complete. The extrapolated value, , is the limiting molar conductivity — a true intrinsic property of the electrolyte, foreshadowed here and explored fully under concentration dependence and Kohlrausch's law.
How do I handle electrolytes like MgCl2 or Na2SO4 with unequal ion counts?
Always define as the concentration of formula units of the electrolyte (e.g., moles of MgCl₂ dissolved), not of individual ionic species. The molar conductivity then represents the conductivity contribution of one mole of the whole electrolyte formula unit, including all the ions it releases. This is closely related to, but distinct from, equivalent conductivity, which normalizes by charge equivalents instead and will be introduced next.
Can Λm be measured directly, or must it always be calculated from κ and c?
It must be calculated from a direct conductivity measurement combined with the known concentration of the prepared solution. There is no separate instrument that measures molar conductivity by itself. Practically, you calibrate a conductivity cell with a standard KCl solution to find , measure resistance for your unknown solution, compute , and finally divide by the solution's known molar concentration.
Why do weak electrolytes show such a dramatic increase in Λm upon dilution compared to strong electrolytes?
For weak electrolytes, dilution shifts the dissociation equilibrium toward more free ions, per Le Chatelier's principle, so both the fraction dissociated and the ionic mobility increase together. For strong electrolytes, dissociation is already essentially complete at all measured concentrations, so dilution only reduces ion-ion interactions slightly, producing the much gentler decrease in with increasing concentration seen in Kohlrausch's linear √c law.