Chemistry / Debye-Hückel-Onsager Electrolyte Conduction
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LABORATORY 33 · NATURAL SCIENCES

Molar Conductivity of Strong Electrolytes and the Debye-Hückel-Onsager Limiting Law

Determine the limiting molar conductivity (Λ_m°) of potassium chloride (KCl) and test the validity of the Debye-Hückel-Onsager limiting law across a series of dilute strong electrolyte solutions. Explore interactive analytical gravimetry, Class A volumetric glassware and density determination.

MEASURE · CALIBRATE · ANALYSE

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SPECIFIC ELECTROLYTIC CONDUCTIVITY Κ—
MEASUREMENT STATUS

Ready to dispense 1.0 mM of liquid.

1.0 mM
Electrolyte System: Potassium Chloride (KCl, 0.50 mM to 12.00 mM in Ultrapure Water)

Adjust c(KCl) V, then weigh the dispensed aliquot.

Mass observations are determined by the high-precision thermodynamic equation of state for pure liquid water. Readings reflect thermal equilibrium and analytical balance force restoration.

Physical chemistry assumptions and metrological limits

['The Debye-Hückel-Onsager limiting law is strictly valid only at infinite dilution and low concentrations (c < 0.015 M for 1:1 salts); at higher concentrations, finite ion size and ion association cause deviations.', 'Dissolved atmospheric carbon dioxide (CO₂) forms carbonic acid which can elevate solvent background conductivity if water is not degassed or protected under nitrogen.', 'For multi-valent electrolytes (e.g., 2:2 salts like MgSO₄), strong electrostatic ion pairing requires extended Fuoss-Onsager association models rather than the simple linear square-root law.'] The Debye-Hückel-Onsager limiting law is expressed as Λ_m = Λ_m° - (A_rel · Λ_m° + B_el) · √c = Λ_m° - S · √c, where Λ_m° is the limiting molar conductivity at infinite dilution and S is the theoretical Onsager slope. For a 1:1 univalent electrolyte in water at 25.00 °C, the theoretical coefficients derived from first principles are A_rel = 0.2289 (mol/L)⁻¹/² and B_el = 60.20 S·cm²·mol⁻¹·(mol/L)⁻¹/². For potassium chloride (Λ_m° = 149.85 S·cm²·mol⁻¹), the theoretical slope is S = 94.50 S·cm²·mol⁻¹·(mol/L)⁻¹/². By plotting molar conductivity Λ_m against √c, linear least-squares regression yields an empirical intercept confirming Λ_m° = 149.9 S·cm²·mol⁻¹ and an empirical slope confirming S = 94.5 S·cm²·mol⁻¹·M⁻¹/² with R² > 0.99999, providing authoritative experimental confirmation of electrolyte conduction theory.

Analytical chemistry apparatus & tools.

High-Precision AC Conductivity Bridge

Digital impedance bridge operating at 1.0 kHz with auto-ranging resolution of 0.001 μS·cm⁻¹, 0.05% basic accuracy, and automatic phase-quadrature nulling to eliminate reactive impedance.

Platinized Platinum Dip Cell

Rigid glass dip cell housing two parallel platinum plates (1.0 cm × 1.0 cm, separation 1.0 cm, cell constant K_cell = 1.000 cm⁻¹) electrolytically platinized with colloidal platinum black to suppress electrode polarization.

Thermostatic Double-Walled Conduction Vessel

Water-jacketed cylindrical borosilicate glass cell coupled to a constant-temperature refrigerated circulator maintaining solution temperature at 25.00 ± 0.02 °C.

Class A Volumetric Glassware & Dispensers

Calibrated 100.0 mL, 250.0 mL, and 500.0 mL Class A volumetric flasks and electronic micropipettes (tolerance ±0.2%) for precision serial dilution of KCl standard solutions.

Analytical Dual-Range Microbalance

Five-decimal electronic balance (±0.01 mg precision) used for primary gravimetric preparation of 0.1000 M stock KCl from fused, oven-dried analytical grade salt.

Triple-Distilled Ultrapure Water Source

Polished Milli-Q deionized water system delivering solvent with resistivity ρ > 18.2 MΩ·cm (solvent background conductivity κ_w < 0.055 μS·cm⁻¹ at 25 °C).

FOLLOW THE METHOD

A reason behind every step.

Determine the limiting molar conductivity (Λ_m°) of potassium chloride (KCl) and test the validity of the Debye-Hückel-Onsager limiting law across a series of dilute strong electrolyte solutions. Suggested independent volumetric settings: 0.5, 1.0, 2.0, 4.0, 8.0, 12.0 mM.

01

Solvent Background Conductivity Determination

Rinse the platinized platinum cell four times with freshly drawn ultrapure water. Fill the thermostatic vessel with 80.0 mL of ultrapure water equilibrated at 25.00 ± 0.02 °C. Record the solvent background conductivity κ_w (typically 0.04 to 0.06 μS·cm⁻¹), which must be subtracted from all subsequent electrolyte measurements.

02

Cell Constant Verification with Primary KCl Standard

Prepare a 0.0100 M KCl calibration standard from desiccated primary-standard salt. Equilibrate at 25.00 °C in the thermostatic bath and measure conductivity κ_std = 1408.7 μS·cm⁻¹ to confirm the cell constant K_cell = 1.000 ± 0.004 cm⁻¹.

03

Serial Dilution of Strong Electrolyte Series

Using calibrated Class A volumetric flasks, prepare six precision test solutions of KCl spanning the dilute Debye-Hückel regime: 0.50 mM, 1.00 mM, 2.00 mM, 4.00 mM, 8.00 mM, and 12.00 mM (concentrations c from 0.0005 M to 0.0120 M).

04

Thermostatic Equilibration of Analyte Samples

Transfer the lowest concentration test solution (0.50 mM KCl) into the double-walled conduction cell. Allow 10 minutes of closed-loop thermal equilibration at 25.00 ± 0.02 °C under gentle magnetic stirring, pausing stirring prior to logging.

05

Conductance Acquisition & Frequency Independence Check

Measure specific electrolytic conductivity κ on the 1.0 kHz bridge. Verify frequency independence by switching briefly to 2.0 kHz to confirm that capacitive electrode reactance is negligible (< 0.02%). Repeat sequentially for all six concentrations from lowest to highest.

06

Molar Conductivity Computation & Onsager Linearization

Subtract solvent background conductivity (κ_corr = κ - κ_w). Compute molar conductivity Λ_m = 1000 × κ_corr / c_M (S·cm²·mol⁻¹). Calculate the square root of molarity √c_M, construct the Kohlrausch plot (Λ_m vs √c), and perform least-squares linear regression to extract limiting molar conductivity Λ_m° and the empirical Onsager slope S.

YOUR NOTEBOOK · 0 OBSERVATIONS

Turn measurements into quantitative chemical insight.

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Points are your recorded gravimetric observations. The regression line validates the linear mass-volume proportionality and extracts density.

ORDINARY LEAST-SQUARES FIT · m = ρ·V + m₀
\Lambda_m = -S \cdot \sqrt{c} + \Lambda_m^\circ \implies \Lambda_m = -94.54 \cdot \sqrt{c} + 149.85 \implies \Lambda_m^\circ = 149.9\text{ S}\cdot\text{cm}^2\cdot\text{mol}^{-1}
#Potassium Chloride Concentration c (mM)Specific Electrolytic Conductivity κ (μS·cm⁻¹)Square Root of Concentration √c (M¹/²)Molar Conductivity Λ_m (S·cm²·mol⁻¹)Remove

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CHECK YOUR UNDERSTANDING

Explain what the gravimetric measurements mean.

What is the physical cause of the decrease in molar conductivity with increasing concentration in strong electrolytes?

According to the Debye-Hückel-Onsager limiting law, how does molar conductivity Λ_m vary with electrolyte concentration c in dilute solutions?

Why does the electrophoretic effect retard ionic motion in an electric field?

For a 1:1 electrolyte in water at 25 °C with Λ_m° = 149.9 S·cm²·mol⁻¹, what is the theoretical Debye-Hückel-Onsager slope S?