Dropping Mercury Electrode (DME) Assembly
Marine-grade marine capillary tube (internal bore ~0.05 mm) connected to a leveling mercury reservoir establishing an exact 50.0 cm hydrostatic head (m = 2.000 mg/s, drop life t = 3.50 s).
Determine the aqueous diffusion coefficient of the cadmium(II) ion (Cd²⁺) and verify the Ilkovič equation in classical DC polarography using a dropping mercury electrode (DME) across concentrations from 0.200 mM to 2.500 mM in 0.100 M KCl supporting electrolyte. Explore interactive analytical gravimetry, Class A volumetric glassware and density determination.
Ready to dispense 1.0 mM of liquid.
Adjust c(Cd²⁺) 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.
['Classical DC polarography is limited to analyte concentrations above 10 μM due to non-faradaic capacitive charging currents (i_c ∝ m²/³ t⁻¹/³).', 'Capillary bore clogging by particulate debris or mercury oxidation can alter the capillary characteristic m²/³ t¹/⁶, requiring re-calibration.', 'Mercury cannot be utilized at potentials positive of +0.25 V vs SCE due to the anodic dissolution of metallic mercury (2 Hg + 2 Cl⁻ → Hg₂Cl₂ + 2 e⁻).'] The Ilkovič equation for the mean diffusion current at a dropping mercury electrode is i_d = 607 · n · D¹/² · m²/³ · t¹/⁶ · c, where n = 2 for Cd²⁺, m = 2.000 mg/s is the calibrated mercury mass flow rate, and t = 3.500 s is the drop lifetime. The capillary constant m²/³ t¹/⁶ equals 1.956 mg²/³·s⁻¹/². Across cadmium concentrations from 0.200 mM to 2.500 mM, the half-wave potential remains strictly invariant at E_1/2 = -0.600 ± 0.002 V vs SCE, confirming reversible two-electron amalgam formation. Linear least-squares regression of mean diffusion current i_d against cadmium concentration c yields a slope of 6.3719 μA·mM⁻¹ with R² = 0.9999996, extracting an aqueous Cd²⁺ diffusion coefficient D = 7.20 × 10⁻⁶ cm²·s⁻¹, in complete agreement with authoritative electrochemical literature benchmarks.
Marine-grade marine capillary tube (internal bore ~0.05 mm) connected to a leveling mercury reservoir establishing an exact 50.0 cm hydrostatic head (m = 2.000 mg/s, drop life t = 3.50 s).
H-type double-jacketed polarographic cell featuring a quiet mercury pool anode and constant-temperature circulation at 25.00 ± 0.02 °C.
External SCE reference cell connected via an agar-saturated KCl salt bridge with a fine porous ceramic plug to provide stable potential reference.
Linear potential ramp generator (-0.200 V to -1.000 V vs SCE at 2.0 mV/s) with a low-pass analog RC damping filter (time constant τ = 1.0 s) to measure mean diffusion currents.
Gas train with vanadous chloride deoxygenating scrubbers and water presaturator to remove electroactive dissolved O₂.
Optical photodiode drop detector linked to a quartz microsecond chronometer to measure individual mercury drop lifetimes with ±0.005 s resolution.
Determine the aqueous diffusion coefficient of the cadmium(II) ion (Cd²⁺) and verify the Ilkovič equation in classical DC polarography using a dropping mercury electrode (DME) across concentrations from 0.200 mM to 2.500 mM in 0.100 M KCl supporting electrolyte. Suggested independent volumetric settings: 0.2, 0.5, 1.0, 1.5, 2.0, 2.5 mM.
Adjust the mercury leveling bulb to establish a precise 50.0 cm column height. Collect 50 falling drops under deionized water into a tared weighing bottle to calibrate mercury mass flow rate m = 2.000 ± 0.005 mg/s.
Prepare standardized Cd²⁺ solutions (0.200, 0.500, 1.000, 1.500, 2.000, 2.500 mM) in 0.1000 M KCl containing 0.002% w/v Triton X-100 to suppress polarographic streaming maxima.
Transfer 25.0 mL of analyte into the jacketed H-cell at 25.00 °C. Bubble high-purity nitrogen for 15 minutes to purge dissolved oxygen, then divert gas flow over the solution surface.
Configure the polarograph from E_initial = -0.200 V to E_final = -1.000 V vs SCE at a slow scan rate of 2.0 mV/s. Record the residual non-faradaic charging current prior to the reduction wave onset.
Initiate the linear potential ramp. Record the sigmoidal polarographic wave. Measure the limiting plateau current (i_lim) between -0.80 V and -0.90 V and subtract the extrapolated residual current to obtain the true diffusion current (i_d).
Verify half-wave potential invariance (E_1/2 = -0.600 V vs SCE). Plot mean diffusion current i_d against cadmium concentration c. Perform linear least-squares regression to extract slope d(i_d)/dc and calculate D using the Ilkovič equation.
Points are your recorded gravimetric observations. The regression line validates the linear mass-volume proportionality and extracts density.
| # | Cadmium(II) Concentration c (mM) | Mean Limiting Diffusion Current i_d (μA) | Cadmium(II) Concentration c (mM) | Mean Limiting Diffusion Current i_d (μA) | Remove |
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No readings yet. Dispense and weigh a volumetric aliquot to record it.