Unlike metallic conductors where electrical charge is transported solely by the drift of delocalized electrons without chemical decomposition, electrolytic conductors transport electrical current through the physical migration of solvated cations and anions toward oppositely charged electrodes, accompanied by chemical oxidation-reduction transformations at the electrode interfaces.
| Physical Quantity | Symbol & Formula | SI & Practical Units | Physical Significance |
|---|---|---|---|
| Resistance | R = ρ · (l / A) | Ohm (Ω) | Opposition offered by the electrolytic solution to the migration of ions. |
| Conductance | G = 1 / R | Siemens (S) or Ω−1 | Ease with which current flows through the electrolytic column. |
| Conductivity (Specific Conductance) | κ = G · (l / A) = G* / R | S cm−1 or S m−1 | Conductance of an electrolytic solution enclosed between two electrodes of 1 cm² cross-sectional area separated by 1 cm (conductance of 1 cm³ of solution). |
| Cell Constant | G* = l / A = κ · R | cm−1 or m−1 | Geometric characteristic of a conductivity cell; determined experimentally using a standard KCl solution of known conductivity. |
Molar Conductivity (Λm): The conducting power of all the ions produced by dissolving exactly one mole of an electrolyte in a given volume of solution between two large parallel electrodes placed 1 cm apart:
In SI units: Λm = κ / (1000 · C) [where κ is in S m−1, C is in mol m−3, Λm is in S m2 mol−1]
Relationship with Equivalent Conductivity (Λeq):
Λm = nfactor · Λeq (where nfactor is the total positive or negative valency of the electrolyte; for example, for Al2(SO4)3, nfactor = 6, so Λm = 6 Λeq).
Conductivity is the conductance of 1 cm³ (unit volume) of the electrolytic solution. Upon dilution, although the total volume of solution increases, the number of current-carrying ions per unit volume (per cm³) decreases for both strong and weak electrolytes. Hence, κ invariably decreases upon dilution.
Molar conductivity is related to conductivity by Λm = κ · Vm, where Vm is the volume of solution containing 1 mole of electrolyte. Upon dilution, the decrease in κ is more than compensated by the large increase in volume Vm. The mechanistic reason differs fundamentally between electrolyte classes:
- For Strong Electrolytes (KCl, NaCl, HCl): Strong electrolytes are 100% dissociated even at moderate concentrations. At high concentrations, strong interionic electrostatic attractions (asymmetric effect and electrophoretic drag) retard ionic mobility. Dilution separates the ions, reducing interionic attractions and maximizing ionic velocity. The variation follows the Debye-Hückel-Onsager equation:
Λm = Λm° − A √CA plot of Λm versus √C yields a straight line with y-intercept equal to the limiting molar conductivity (Λm°).
- For Weak Electrolytes (CH3COOH, NH4OH): Weak electrolytes have a very low degree of dissociation (α ≪ 1). According to Ostwald's dilution law, dilution shifts the ionization equilibrium forward (α → 1 at C → 0). Near infinite dilution, Λm increases steeply, asymptotically approaching the y-axis. Consequently, Λm° for weak electrolytes cannot be obtained by linear extrapolation to zero concentration.
Statement: At infinite dilution, when all interionic forces become negligible, the limiting molar conductivity of an electrolyte is equal to the sum of the individual contributions (limiting ionic conductivities) of its constituent cations and anions:
where λ+° and λ−° are the limiting molar ionic conductivities of the cation and anion respectively, and ν+ and ν− are the stoichiometric numbers of cations and anions produced per formula unit of the electrolyte (e.g., for Al2(SO4)3, Λm° = 2λ°(Al3+) + 3λ°(SO42−)).
- Calculation of Λm° of Weak Electrolytes:
Λm°(CH3COOH) = Λm°(CH3COONa) + Λm°(HCl) − Λm°(NaCl). - Determination of Degree of Dissociation (α) of Weak Electrolytes:
α = Λm / Λm°. - Calculation of Dissociation Constant (Ka) of Weak Acids:
Ka = (C · α2) / (1 − α) = [C · (Λm / Λm°)2] / [1 − (Λm / Λm°)]. - Determination of Solubility (S) & Solubility Product (Ksp) of Sparingly Soluble Salts (AgCl, BaSO4):
Since a saturated solution of a sparingly soluble salt is extremely dilute, Λm ≈ Λm°. Therefore:
S (in mol L−1) = (1000 · κsalt) / Λm° [where κsalt = κsolution − κwater], and Ksp = S2 (for 1:1 salts like AgCl).