Calculator
Plotly Graph
The chart compares simple transmission, slab escape, and sphere escape across a practical optical depth range.
Example Data Table
| Optical Depth τ | Simple Transmission | Slab Escape | Sphere Escape | Slab Trapped Fraction |
|---|---|---|---|---|
| 0.20 | 0.8187 | 0.9063 | 0.8648 | 0.0937 |
| 0.50 | 0.6065 | 0.7869 | 0.7073 | 0.2131 |
| 1.00 | 0.3679 | 0.6321 | 0.5273 | 0.3679 |
| 2.00 | 0.1353 | 0.4323 | 0.3324 | 0.5677 |
Formula Used
T = e-τThis gives the fraction of photons crossing the medium directly.
βslab = (1 - e-τ) / τThis estimates the mean escape probability for photons created throughout a slab.
βsphere = (3 / 4τ) [1 - 1 / (2τ²) + (1 / τ + 1 / 2τ²)e-2τ]This estimates average escape from a uniformly emitting sphere.
τ = 2.303 ε c lA = ε c lτ = 2.303 AThese relations convert absorbance-style inputs into optical depth.
τ = αLUse this when attenuation coefficient and physical distance are known.
τ = σnLUse this for particle-based media with number density and absorption cross section.
How to Use This Calculator
- Choose the input mode that matches your chemistry data.
- Select the escape model for your assumed geometry.
- Enter optical, path, or concentration values in consistent units.
- Press the calculate button to show the result above the form.
- Review escape probability, trapped fraction, and equivalent absorbance.
- Download CSV or PDF files for reporting or sharing.
FAQs
1. What does photon escape probability mean?
It is the estimated fraction of photons that leave a medium without being reabsorbed. Larger values mean photons escape easily. Smaller values indicate stronger trapping.
2. Which model should I choose?
Use simple transmission for direct passage through an absorbing path. Use slab for planar media. Use sphere for roughly isotropic emission inside a bulk particle or droplet.
3. Why is slab escape often higher than direct transmission?
Direct transmission assumes every photon crosses the full path. Slab escape averages photons created at many depths, so some photons start closer to the boundary and escape more easily.
4. What happens when optical depth is zero?
The medium is effectively transparent. Escape probability becomes one, transmission becomes one, and trapped fraction becomes zero.
5. Can I start from absorbance data?
Yes. Beer–Lambert absorbance converts to optical depth through τ = 2.303A. This calculator uses ε, concentration, and path length to perform that step automatically.
6. Does unit choice matter?
Yes. Units must be internally consistent. For example, if α is in cm-1, then path length should be in cm. Mixed units will distort optical depth.
7. Can this help with fluorescence or emission screening?
Yes, as a first-pass estimate. It is useful for comparing trapping severity. It does not replace full radiative transfer, scattering, anisotropy, or quantum-yield models.
8. Why does escape probability fall with higher optical depth?
Higher optical depth means a photon experiences more attenuation before reaching the surface. That increases the chance of reabsorption or loss inside the medium.