High-Pressure Mercury Arc Lamp with Monochromatic 365 nm Optical Filter
Emits stabilized UV radiation centered at 365.0 nm with liquid-filtered thermal isolation and a shutter-controlled exposure aperture.
Determine the photochemical quantum yield (Φ) for the sensitized photodecomposition of oxalic acid using uranyl oxalate actinometry at λ = 365 nm and permanganometric redox titration. Explore interactive analytical gravimetry, Class A volumetric glassware and density determination.
Ready to dispense 20.0 min of liquid.
Adjust exposure time 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.
The determination of photochemical quantum yield and photon flux via uranyl oxalate actinometry is subject to several fundamental physical, optical, and chemical constraints: (1) Optical Density and Cell Geometry: The actinometer must maintain an optical absorbance A > 2.0 at the irradiation wavelength to ensure > 99% photon absorption; beam divergence or reflection losses at quartz-air interfaces (~4% per optical surface) require Fresnel reflection corrections; (2) High-Flux Photoproduct Accumulation: If photolysis exceeds 20% conversion of the initial oxalate pool, accumulation of dissolved CO and CO₂ and slight changes in solution pH can alter the coordination equilibria of uranyl-oxalate complexes, causing slight deviation from zero-order photolysis kinetics; (3) Thermal Decomposition: Although the photochemical quantum yield has a minimal temperature coefficient (< 0.3%/°C), high-power UV lamps emit significant infrared radiation; adequate water-jacket cooling is mandatory to prevent thermal heating of the quartz cell; (4) Permanganometric Visual Endpoint: Manual visual detection of the persistent faint pink endpoint introduces an operator-dependent volume uncertainty of ± 0.03 mL, corresponding to an uncertainty of ± 0.75 μmol in photolyzed oxalate; and (5) Uranyl Toxicity and Regulatory Handling: Strict institutional controls governing depleted uranium salts necessitate micro-scale handling and specialized radioactive waste streams. Leighton-Forbes Actinometer System | Photosensitizer: UO₂²⁺ (0.010 M) | Substrate: H₂C₂O₄ (0.020 M) | Light Source: 365 nm Hg Arc (q₀ = 10.00 μeinstein/min) | Φ = 0.570 mol/einstein
Emits stabilized UV radiation centered at 365.0 nm with liquid-filtered thermal isolation and a shutter-controlled exposure aperture.
Precision optical irradiation cell with planar optical entry window (4.00 × 4.00 cm) and internal circulating jacket at 25.00 ± 0.05 °C.
Dispenses standardized 0.0100 M potassium permanganate titrant for quantitative redox residual oxalate quantification.
Maintains the acidified analyte solution at 70 °C to accelerate the permanganate-oxalate redox reaction without non-catalytic thermal decomposition.
Formulated from analytical grade uranyl nitrate hexahydrate (0.0100 M UO₂(NO₃)₂) and primary standard oxalic acid dihydrate (0.0200 M H₂C₂O₄).
Standardized against primary standard sodium oxalate (Na₂C₂O₄) to determine exact normality with 0.05% systematic uncertainty.
Determine the photochemical quantum yield (Φ) for the sensitized photodecomposition of oxalic acid using uranyl oxalate actinometry at λ = 365 nm and permanganometric redox titration. Suggested independent volumetric settings: 5.0, 10.0, 15.0, 20.0, 30.0, 40.0 min.
Pipette a 25.00 mL aliquot of unexposed uranyl oxalate stock into a conical flask. Add 10.00 mL of 3 M sulfuric acid, heat to 70 °C, and titrate with standardized 0.0100 M KMnO₄ to the first persistent pink endpoint to establish blank volume V₀ = 20.00 mL.
Ignite the high-pressure mercury arc lamp and allow 30 minutes for photon flux stabilization. Insert the 365 nm bandpass filter and verify beam collimation perpendicular to the quartz irradiation cell.
Transfer 100.0 mL of uranyl oxalate actinometer solution into the quartz cell at 25.00 °C. Expose the solution under continuous magnetic stirring for scheduled intervals: t = 5.0, 10.0, 15.0, 20.0, 30.0, and 40.0 minutes.
Immediately following each exposure interval, withdraw an exact 25.00 mL aliquot from the photolyzed solution using a calibrated volumetric pipette and transfer into an Erlenmeyer flask containing 10.00 mL of 3 M H₂SO₄.
Heat the acidified aliquot to 70 °C on the thermostatic heating station. Titrate slowly with standardized 0.0100 M KMnO₄ under continuous swirling until a faint pink coloration persists for at least 30 seconds, recording the titrant volume V_t in mL.
Compute the moles of oxalic acid photodecomposed: Δn = (5/2) · c(KMnO₄) · (V₀ − V_t) in micromoles. Plot Δn versus exposure time t. Extract the photolysis rate slope m (μmol/min) and determine the quantum yield Φ = m / q₀ (mol/einstein) with R² ≥ 0.999.
Points are your recorded gravimetric observations. The regression line validates the linear mass-volume proportionality and extracts density.
| # | UV photolysis exposure time t (min) (min) | Permanganate titrant volume V_t (mL) | Photolysis exposure time t (min) | Decomposed oxalic acid Δn (μmol) | Remove |
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No readings yet. Dispense and weigh a volumetric aliquot to record it.