Thermal and instrument widths add as variances
Convolving two independent Gaussians adds their variances. The thermal broadening in wavelength uses the first-order Doppler approximation.
Thermal motion / Line widths
How can two hydrogen isotopes give a gas temperature when the spectrometer also blurs the lines? Compare their line widths. At the same temperature the lighter hydrogen atoms move faster, so thermal motion broadens their line more than deuterium's, while the instrument blurs both equally. The difference of the two squared widths then depends only on temperature, and either line gives the instrument's share. If the instrument blur dominates, that small difference drowns in counting noise.
Record separate spectra of light and heavy hydrogen at the same temperature. Infer both Gaussian line widths from the photon counts, then split them into a thermal part and an instrument variance that both lines share.
Normal incidence on a transmission grating; the first diffracted order reaches the rotating collection arm. Physical ray angles are unscaled. Fine scanning motion is tiny; sizes, bandwidth and slit widths are schematic.
Photon counts against calibrated vacuum wavelength
Two sequential scans retain 121 bins for each known isotope. Both samples share the same temperature and Gaussian instrument. Switching gas and acquisition are accelerated; no physical elapsed time is inferred.
Ready. Predict, then acquire.
Recorded bins
Current analyser wavelength
Raw counts with a bin-integrated Poisson fit
Dots retain zero bins; vertical bars show the square root of observed counts. Lines integrate over each bin. The optional gold source expectation is a simulation reference.
Infer from the recorded counts
Inferred temperature
Inferred instrumental width
Width-difference heuristic error
No saved comparison.
Bars show observed variances. When inference is usable, gray is instrumental and green is thermal.
Model check against the kept counts
Poisson deviance per bin defines the squared residual; its zero-count logarithm term is zero. Outliers beyond the plotting range appear as red edge dots. This plot checks the declared profile, not historical evidence. Fit boundaries and conservative identifiability rules can withhold the derived parameter.
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Incident light travels along the positive horizontal axis to a normal-incidence transmission grating. Its period is one micrometre, and the positive first order lies in the horizontal dispersion plane. The collection lens, slit and detector share that outgoing axis. The calibrated Gaussian bandpass is assumed, not derived from the exaggerated slit geometry.
Independent Poisson bins integrate the full line profile. The source budget is the ideal expected signal sum over a complete scan, apart from truncated tails; it is not an absolute radiometric calibration. Background is fitted from the same bins. Counts are synthetic, and recovery of their generating law is not an independent experimental test.
Known proton and deuteron masses plus the electron mass set the approximate atom masses. Both sources have one shared translational temperature and one shared instrumental width. Each real Balmer multiplet is collapsed to one effective line; applying this inversion directly to real hydrogen without resolving its components would bias temperature. The displayed error scale is a leading Gaussian count heuristic, not a fitted confidence interval or significance.
NIST · Atomic spectroscopyTel Aviv · Isotope spectroscopyNIST · Doppler thermometry
Compare: infer a nuclear massHydrogen orbitals and transitionsHistorical spectral evidence
Physics tutorial
BackgroundRecord separate spectra of light and heavy hydrogen at the same temperature. Infer both Gaussian line widths from the photon counts, then split them into a thermal part and an instrument variance that both lines share.
Why it mattersYou infer a constant from the observations you keep, read through a calibrated instrument response.
Start with the essentials
Convolving two independent Gaussians adds their variances. The thermal broadening in wavelength uses the first-order Doppler approximation.
The estimate uses both measured widths. It is given neither the source temperature nor the instrument width.
Typical misconceptionRecovering a source parameter independently confirms the law.
Better mental modelThese synthetic records test how the measurement and the inference work. They are not historical observations, they do not give a confidence interval for the parameter, and they are not outside scientific certification.
Acquire both isotope scans at the same source temperature.
What to observe: The lighter atoms have a broader thermal line.Increase only the source instrumental standard deviation and acquire again for comparison.
What to observe: Both variances rise by the same amount, and their difference still carries the temperature.Choose the Instrument dominates preset.
What to observe: A small difference between the two widths can be swamped by the counting uncertainty.Quantum evidence · Reading path
Articles on this path that use this experiment, followed by the other experiments they suggest.