Each time you press “Save scenario” the calculator adds the current plasma state to this table, letting you contrast stellar layers, lab setups, or coursework exercises without retyping numbers.
This upgrade keeps the familiar Saha equation while exposing the ingredients you adjust in real analyses: temperature T, electron density nₑ, ionization energy χ, and the statistical weight ratio gi+1/gi. The script converts χ from electronvolts to joules, evaluates the full prefactor 2·(gi+1/gi)·(2πmₑkT/h²)3/2, and balances it against your density entry. A logistic transform keeps the ionized fraction stable even when the raw ratio spans hundreds of orders of magnitude.
The classical form of the Saha equation links the population ratio directly to temperature, density, and statistical weights:
1e20
is accepted), then adjust χ or the g-ratio if your
source uses different data.
The presets anchor the drop-down menu. Feel free to overwrite them after they load if your environment requires different numbers.
Stage | χ (eV) | gi+1/gi | Typical temperature | Use case |
---|---|---|---|---|
Hydrogen I → H II | 13.60 | 2.0 | 7,000–15,000 K | Balmer-line photospheres, H II regions |
Helium I → He II | 24.59 | 1.0 | 12,000–25,000 K | Hot B-type stellar atmospheres |
Helium II → He III | 54.42 | 2.0 | 25,000–50,000 K | Extreme-UV sources and white dwarf envelopes |
Sodium I → Na II | 5.14 | 2.0 | 3,000–6,000 K | Cool stellar photospheres, discharge lamps |
Calcium II → Ca III | 11.87 | 1.5 | 6,000–10,000 K | Chromospheric diagnostics |
Iron I → Fe II | 7.90 | 1.6 | 5,000–9,000 K | Line-blanketing studies, laboratory plasmas |
Use the sweep inputs to map a stellar layer or an experiment. A handful of rows spanning a few thousand kelvin reveal when log10(ni+1/ni) crosses zero, signalling equal populations. After running a sweep, click “Save scenario” on the most relevant temperatures to build a casebook. The comparison log stores up to eight entries—ideal for contrasting main-sequence versus giant-branch photospheres or before-and-after states of a discharge tube.
Consider a stellar layer at 10,000 K with an electron density of 1×1020 m-3. Choose the hydrogen preset (χ = 13.60 eV, g-ratio = 2) and run the calculation. The tool reports an ionized fraction near 50%, classifying the plasma as mixed. Doubling the temperature pushes the fraction toward 90%, while halving the density drops it below 30%. Saving the scenario lets you compare it directly against cooler layers (for example 7,000 K) and identify where Balmer absorption is strongest.
Switch to the helium preset without changing T or nₑ and the ionized fraction plunges, demonstrating why helium lines require hotter stars. Add a sweep from 15,000 to 25,000 K to tabulate how the helium fraction climbs and copy the table into lab notes or an assignment write-up.
The ratio gi+1/gi reflects the relative statistical weights (degeneracies) of the ionized and neutral states. Hydrogen doubles its degeneracy after ionization, hence the preset value of 2. Multi-electron atoms often use partition functions evaluated at the working temperature. Setting the ratio to 1 reproduces the textbook simplified form, but adjusting it improves fidelity for species with dense term structures.
The equation assumes local thermodynamic equilibrium with collisions dominating over radiation. In tenuous nebulae or rapidly changing laser plasmas the result becomes a first-order guide rather than a final answer. If the scenario insight shows large swings when you tweak density or temperature, consider following up with a non-LTE or kinetic model.
That message indicates the logarithmic term is so extreme that the raw ratio overflows standard floating-point numbers. The logistic formulation still produces a meaningful ionized fraction: you are effectively in a fully ionized or fully neutral limit. Narrow the sweep range or adjust density to explore the transition region if you need more granularity.
Yes. After any calculation, press “Save scenario” to add it to the comparison log. Up to eight rows are retained. Use the “Copy summary” button to grab the current synopsis for lab books or observation planning documents, and clear the log when you start a new project.
Common conversions include 1 cm-3 = 106 m-3 and 1 mm-3 = 109 m-3. If you are working from mass densities, divide by the mean molecular weight and multiply by Avogadro’s number before entering the electron number density. Keeping a short conversion table next to the calculator reduces transcription errors.
Use this calculator as a launchpad for deeper modelling. Try saving states for successive ionization levels of the same element, compare them with observed spectral lines, or feed the ionized fractions into opacity or emissivity codes. The combination of presets, sweep exploration, and casebook logging provides a lightweight workflow for both lecture notes and professional planning.