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Spectroscopy Nomenclature

Spectroscopic results are often numerically correct but semantically incomplete. A value called a wavelength may be a vacuum wavelength, an air wavelength, or a wavelength inside a sample. An absorbance may use a base-10 or natural logarithm. A quoted linewidth may be a full width at half maximum, a half width, a Gaussian standard deviation, or a decay rate. These are not typographical details: changing the convention changes the number and sometimes the physical interpretation.

This page is a compact vocabulary and conversion reference. It states enough of each definition to audit a table, spectrum, or methods section. The canonical derivations remain in Constants and Conversions, Absorption and Emission, and Line Shape Reference.

This entry owns:

  • vacuum wavelength, medium wavelength, ordinary frequency, angular frequency, spectroscopic wavenumber, and angular wavenumber conventions;
  • transmittance, decadic and Napierian absorbance, absorptance, attenuation, and optical depth;
  • microscopic cross sections and their connection to macroscopic coefficients;
  • the minimum metadata needed to interpret a linewidth;
  • elementary diatomic branch notation and warnings for open-shell spectra; and
  • a reporting checklist for reproducible spectra.

It does not own:

  • numerical values of fundamental constants;
  • detailed line-profile theory or broadening mechanisms;
  • transition moments, oscillator strengths, or Einstein coefficients;
  • radiative-transfer solutions with distributed emission;
  • molecular term-symbol construction; or
  • a full assignment theory for polyatomic, asymmetric-top, or predissociative spectra.

Follow the linked canonical pages when those details matter.

No symbol is self-defining. The following collisions are common enough that a paper or database should resolve them in words.

SymbolCommon meaningsSafer practice
AAdecadic absorbance; Einstein spontaneous-emission coefficient; areawrite A10A_{10} for decadic absorbance and AulA_{ul} for an Einstein coefficient
TTtransmittance; temperature; kinetic energy in some Hamiltoniansdefine T=P/P0T=\mathcal P/\mathcal P_0 beside the first optical use
ν\nuordinary frequency; an occasional label for a vibrational quantum numberuse vv for a vibrational quantum number when confusion is possible
ν~\tilde\nu or σ\sigmaspectroscopic wavenumber; σ\sigma also denotes a cross sectionprefer ν~\tilde\nu for wavenumber and attach units
kkangular wavenumber; Boltzmann constant; rate coefficientwrite k0=2π/λk_0=2\pi/\lambda and kBk_{\mathrm B} explicitly
σ\sigmamicroscopic cross section; Gaussian standard deviation; wavenumber in some tablesadd a subscript such as σabs\sigma_{\mathrm{abs}} or σν\sigma_\nu
Γ\Gammadecay rate; Lorentzian FWHM; Lorentzian HWHM; complex-energy widthstate both the observable and its units
SSline strength; integrated intensity; action; source functiongive the defining integral or matrix element
IIirradiance; spectral intensity; detector counts; angular momentuminclude the denominator, such as W m−2\mathrm{W\,m^{-2}} or counts per bin
RRreflectance; resolving power; rotational branch letteruse context-specific subscripts or words

A units column is necessary but not sufficient. Both ν\nu and a linewidth Δν\Delta\nu can be reported in hertz, and both an absorption cross section and a scattering cross section have units of area.

The ordinary frequency ν\nu counts cycles per unit time:

[ν]=Hz=s−1.[\nu]=\mathrm{Hz}=\mathrm{s^{-1}}.

The angular frequency is

ω=2πν,\omega=2\pi\nu,

with units customarily written rad s−1\mathrm{rad\,s^{-1}}. The radian is dimensionless in SI, but retaining “rad” in prose or a table helps prevent a missing factor of 2π2\pi.

For a photon,

E=hν=ℏω.E=h\nu=\hbar\omega.

Frequency is fixed by the temporal phase. For a stationary interface, the frequency and angular frequency are continuous across the interface even though wavelength and spatial wavenumber change.

The vacuum wavelength is

λvac=cν.\lambda_{\mathrm{vac}} = \frac{c}{\nu}.

In a homogeneous medium with phase refractive index n(ν)n(\nu),

λmed=cn(ν)ν=λvacn(ν).\lambda_{\mathrm{med}} = \frac{c}{n(\nu)\nu} = \frac{\lambda_{\mathrm{vac}}}{n(\nu)}.

Thus a bare statement such as “the wavelength is 500 nm500\,\mathrm{nm}” is incomplete whenever the vacuum/air distinction is relevant. Atomic line lists may report an observed wavelength or a Ritz wavelength computed from optimized level energies. Those are different provenance labels even when their numerical values agree within uncertainty.

An air wavelength is a medium wavelength inferred using a specified refractive-index formula:

λair=λvacnair.\lambda_{\mathrm{air}} = \frac{\lambda_{\mathrm{vac}}}{n_{\mathrm{air}}}.

The air conditions and dispersion formula belong in precision metadata. Database defaults can also change with spectral region, so the column header or database documentation is authoritative, not an assumed wavelength range.

The spectroscopic wavenumber is the reciprocal vacuum wavelength:

ν~=1λvac=νc.\tilde\nu = \frac{1}{\lambda_{\mathrm{vac}}} = \frac{\nu}{c}.

Its coherent SI unit is m−1\mathrm{m^{-1}}, but molecular spectroscopy commonly uses cm−1\mathrm{cm^{-1}}. The conversion is

1 cm−1=100 m−1.1\ \mathrm{cm^{-1}} = 100\ \mathrm{m^{-1}}.

The photon-energy relation becomes

E=hcν~.E = hc\tilde\nu.

The angular wavenumber, often written kk, is instead

kvac=2πλvac=ωc=2πν~.k_{\mathrm{vac}} = \frac{2\pi}{\lambda_{\mathrm{vac}}} = \frac{\omega}{c} = 2\pi\tilde\nu.

Therefore “wavenumber” can conceal a factor of 2π2\pi. In routine optical spectroscopy, a value in cm−1\mathrm{cm^{-1}} almost always denotes ν~\tilde\nu, not kk.

For a vacuum photon, the basic conversion chain is

ν=cλvac=cν~,ω=2πν,kvac=2πν~,E=hν=ℏω=hcλvac=hcν~.\begin{aligned} \nu &= \frac{c}{\lambda_{\mathrm{vac}}} = c\tilde\nu, \\ \omega &= 2\pi\nu, \\ k_{\mathrm{vac}} &= 2\pi\tilde\nu, \\ E &= h\nu = \hbar\omega = \frac{hc}{\lambda_{\mathrm{vac}}} = hc\tilde\nu. \end{aligned}
CoordinateDefinitionTypical unitIncreases with photon energy?
vacuum wavelength λvac\lambda_{\mathrm{vac}}c/νc/\nunm, μm\mu\mathrm m, or Åno
frequency ν\nucycles per timeHz, GHz, THzyes
angular frequency ω\omega2πν2\pi\nurad s−1\mathrm{rad\,s^{-1}}yes
spectroscopic wavenumber ν~\tilde\nu1/λvac1/\lambda_{\mathrm{vac}}cm−1\mathrm{cm^{-1}}yes
angular wavenumber kk2π/λ2\pi/\lambdam−1\mathrm{m^{-1}}yes
photon energy EEhνh\nuJ or eVyes

Because wavelength runs opposite to energy, a plot that increases from left to right in wavelength decreases from left to right in frequency, wavenumber, and photon energy.

Changing the horizontal coordinate of a spectrum requires more than relabeling tick marks when the vertical quantity is a density per unit coordinate. If a conserved spectral amount is written

dQ=qx(x) dx=qy(y) ∣dy∣,dQ = q_x(x)\,dx = q_y(y)\,|dy|,

then

qy(y)=qx(x(y))∣dxdy∣.q_y(y) = q_x(x(y)) \left| \frac{dx}{dy} \right|.

For frequency and vacuum wavelength,

∣dνdλvac∣=cλvac2.\left| \frac{d\nu}{d\lambda_{\mathrm{vac}}} \right| = \frac{c}{\lambda_{\mathrm{vac}}^2}.

Consequently,

qλ(λvac)=qν(c/λvac)cλvac2.q_\lambda(\lambda_{\mathrm{vac}}) = q_\nu(c/\lambda_{\mathrm{vac}}) \frac{c}{\lambda_{\mathrm{vac}}^2}.

The peak of a broad density can move under this transformation. A spectrum per nanometre and one per terahertz are not expected to have identical vertical shapes.

For spectroscopic wavenumber expressed in m−1\mathrm{m^{-1}},

dν=c dν~.d\nu = c\,d\tilde\nu.

If the numerical wavenumber is instead in cm−1\mathrm{cm^{-1}}, the Jacobian contains an additional factor of 100100. A normalized line profile must name its coordinate:

∫ϕν(ν) dν=∫ϕν~(ν~) dν~=1.\int \phi_\nu(\nu)\,d\nu = \int \phi_{\tilde\nu}(\tilde\nu)\,d\tilde\nu = 1.

Pointwise transmittance at a physical photon energy is unchanged by reparameterizing the axis. A density, normalized profile, or integrated area does require the Jacobian.

Let P0\mathcal P_0 be incident radiant power in a declared beam and P\mathcal P the power reaching the declared transmitted channel. Detector counts may substitute for power only after establishing proportionality and correcting dark counts, nonlinearity, and wavelength-dependent response.

The transmittance is

T=PP0.T = \frac{\mathcal P}{\mathcal P_0}.

It is dimensionless. For a passive sample and a consistently defined channel, 0≤T≤10\leq T\leq1. A value above unity can indicate gain, emission into the collection channel, normalization drift, or a data-reduction error.

Internal transmittance isolates propagation through the sample. Total transmittance can also include interface reflection, scattering, aperture loss, and other losses in the measurement geometry. The two should not be interchanged in a Beer–Lambert analysis.

Percent transmittance is

T%=100T.T_{\%}=100T.

It is not a new physical quantity; it is a rescaling of the dimensionless ratio.

The decadic absorbance is

A10=−log⁡10T=log⁡10 ⁣(P0P).A_{10} = -\log_{10}T = \log_{10}\!\left( \frac{\mathcal P_0}{\mathcal P} \right).

The Napierian absorbance is

Ae=−ln⁡T.A_{\mathrm e} = -\ln T.

They are related by

Ae=(ln⁡10)A10,A_{\mathrm e} = (\ln 10)A_{10},

and inverted by

T=10−A10,T=e−Ae.\begin{aligned} T &= 10^{-A_{10}}, \\ T &= e^{-A_{\mathrm e}}. \end{aligned}

Both absorbances are dimensionless. A logarithm does not carry a unit, and a reported absorbance should identify its base. In much of analytical spectroscopy, unqualified absorbance means the decadic quantity; in radiative transfer and AMO theory, the natural-log quantity is more common.

The absorptance is the fraction of incident radiant power actually absorbed. For a passive sample,

A=PabsorbedP0.\mathcal A = \frac{\mathcal P_{\mathrm{absorbed}}}{\mathcal P_0}.

It is a linear fraction, not a logarithm. If reflectance RR and all other loss channels are negligible,

A=1−T.\mathcal A = 1-T.

More generally, energy conservation can require

1=T+R+A+L,1 = T+R+\mathcal A+\mathcal L,

where L\mathcal L collects scattering or other channels not included in the declared transmitted and reflected beams. Therefore 1−T1-T is not automatically the absorptance.

For a monochromatic collimated beam propagating through a linear, homogeneous, nonscattering medium with no source term,

dIds=−αI.\frac{dI}{ds} = -\alpha I.

Here II is irradiance and α\alpha is a Napierian linear attenuation or absorption coefficient, according to which loss mechanisms are included. For constant α\alpha over path length LL,

I(L)=I(0)e−αL.I(L) = I(0)e^{-\alpha L}.

Thus

T=e−αL.T=e^{-\alpha L}.

The assumptions matter. Saturation, spatial inhomogeneity, multiple scattering, fluorescence into the detector, interference, or a distributed source term can invalidate this one-parameter interpretation.

The optical depth along a path is

τ=∫pathα(s) ds.\tau = \int_{\mathrm{path}} \alpha(s)\,ds.

For the direct beam under the conditions above,

T=e−τ.T=e^{-\tau}.

Therefore

τ=−ln⁡T=Ae=(ln⁡10)A10.\tau = -\ln T = A_{\mathrm e} = (\ln 10)A_{10}.

The equality between optical depth and Napierian absorbance is conditional on matching beam and loss definitions. Optical depth may describe total extinction, whereas an experimental absorbance may contain interface and instrument contributions.

Independent layers add in optical depth:

τtot=∑iτi,\tau_{\mathrm{tot}} = \sum_i\tau_i,

while their direct-beam transmittances multiply:

Ttot=∏iTi.T_{\mathrm{tot}} = \prod_i T_i.

This additivity is one reason optical depth is useful for heterogeneous paths.

Cross Sections and Macroscopic Coefficients

Section titled “Cross Sections and Macroscopic Coefficients”

A cross section is an effective area that converts incident particle or photon flux into an event rate. For one target in a weak incident beam,

Revent=σΦ,R_{\mathrm{event}} = \sigma\Phi,

where Φ\Phi is the incident number flux in m−2 s−1\mathrm{m^{-2}\,s^{-1}}. Hence

[σ]=m2.[\sigma]=\mathrm{m^2}.

An absorption cross section, scattering cross section, photoionization cross section, and extinction cross section answer different event questions. For a passive isolated target,

σext=σabs+σsca.\sigma_{\mathrm{ext}} = \sigma_{\mathrm{abs}} + \sigma_{\mathrm{sca}}.

A gain medium can instead be described by a signed net cross section, but the sign convention and population dependence must then be stated.

For independent absorbers of number density n(s)n(s),

αabs(s)=n(s)σabs.\alpha_{\mathrm{abs}}(s) = n(s)\sigma_{\mathrm{abs}}.

If the cross section is constant along the path,

τabs=σabsNcol,\tau_{\mathrm{abs}} = \sigma_{\mathrm{abs}}N_{\mathrm{col}},

where the column density is

Ncol=∫n(s) ds.N_{\mathrm{col}} = \int n(s)\,ds.

The dimensions close:

[Ncol]=m−2,[σNcol]=1.[N_{\mathrm{col}}] = \mathrm{m^{-2}}, \qquad [\sigma N_{\mathrm{col}}] = 1.

When multiple species or internal states contribute,

α(ν,s)=∑jnj(s)σj(ν).\alpha(\nu,s) = \sum_j n_j(s)\sigma_j(\nu).

The state populations are part of the model. A database line strength does not by itself specify the cross section of an unequilibrated sample.

The common decadic Beer–Lambert form is

A10=ε10cML,A_{10} = \varepsilon_{10}c_{\mathrm M}L,

where cMc_{\mathrm M} is molar concentration and the units of ε10\varepsilon_{10} must match those chosen for concentration and path length. A frequently used combination is

[ε10]=L mol−1 cm−1,[cM]=mol L−1,[L]=cm.[\varepsilon_{10}] = \mathrm{L\,mol^{-1}\,cm^{-1}}, \quad [c_{\mathrm M}] = \mathrm{mol\,L^{-1}}, \quad [L] = \mathrm{cm}.

For those units, the corresponding microscopic cross section in m2\mathrm{m^2} is

σabs=ln⁡1010NAε10.\sigma_{\mathrm{abs}} = \frac{\ln 10}{10N_{\mathrm A}} \varepsilon_{10}.

The factor 1010 is a unit-conversion factor, not spectroscopy. It combines litres with cubic metres and centimetres with metres. In coherent SI units, one can instead write

αe=κec,\alpha_{\mathrm e} = \kappa_{\mathrm e}c,

with κe\kappa_{\mathrm e} in m2 mol−1\mathrm{m^2\,mol^{-1}} and cc in mol m−3\mathrm{mol\,m^{-3}}, giving

σabs=κeNA.\sigma_{\mathrm{abs}} = \frac{\kappa_{\mathrm e}}{N_{\mathrm A}}.

A line-centre cross section is a pointwise area:

σ0=σ(ν0).\sigma_0 = \sigma(\nu_0).

An integrated cross section includes the chosen spectral coordinate:

Σν=∫σ(ν) dν.\Sigma_\nu = \int \sigma(\nu)\,d\nu.

Its units are m2 Hz\mathrm{m^2\,Hz}, not m2\mathrm{m^2}. An integral over wavenumber or angular frequency has a different numerical value and different units. If

σ(ν)=Σνϕν(ν),\sigma(\nu) = \Sigma_\nu\phi_\nu(\nu),

then

∫ϕν(ν) dν=1,\int\phi_\nu(\nu)\,d\nu=1,

so ϕν\phi_\nu has units Hz−1\mathrm{Hz^{-1}}. Never compare a line-centre cross section with an integrated cross section, or two integrated values on different coordinates, without converting the measure.

The Oscillator Strength Reference owns the corresponding integrated-strength relations.

The following table separates quantities that are often all called “absorption.”

QuantityDefinitionUnitsMain warning
transmittance TTtransmitted/incident radiant power1depends on collection channel
decadic absorbance A10A_{10}−log⁡10T-\log_{10}T1state the logarithm base
Napierian absorbance AeA_{\mathrm e}−ln⁡T-\ln T1equals τ\tau only for matched definitions
absorptance A\mathcal Aabsorbed/incident radiant power1not A10A_{10} and not always 1−T1-T
optical depth τ\tau∫α ds\int\alpha\,ds1identify absorption or total extinction
linear coefficient α\alphalocal fractional loss per lengthm−1\mathrm{m^{-1}}identify included loss processes
cross section σ\sigmaevent rate per target divided by number fluxm2\mathrm{m^2}name the event and internal state
column density NcolN_{\mathrm{col}}∫n ds\int n\,dsm−2\mathrm{m^{-2}}state species and state population
molar decadic coefficient ε10\varepsilon_{10}A10/(cML)A_{10}/(c_{\mathrm M}L)often L mol−1 cm−1\mathrm{L\,mol^{-1}\,cm^{-1}}units are convention dependent

The older phrase extinction coefficient is especially ambiguous: it has been used for a Napierian attenuation coefficient, a decadic coefficient, a molar absorptivity, and the imaginary part of a refractive index. Prefer the specific modern quantity name and equation.

A reproducible linewidth should specify:

  1. the profile or operational estimator;
  2. full width, half width, standard deviation, or decay-rate convention;
  3. the spectral coordinate and unit; and
  4. whether the width is observed, instrument-corrected, homogeneous, inhomogeneous, or model decomposed.

For example, “Gaussian FWHM ΔνG=12.0 MHz\Delta\nu_{\mathrm G}=12.0\,\mathrm{MHz} after instrument-response deconvolution” is interpretable. “Γ=12\Gamma=12” is not.

For a Gaussian profile with standard deviation σν\sigma_\nu,

ΔνFWHM(G)=22ln⁡2 σν.\Delta\nu_{\mathrm{FWHM}}^{(\mathrm G)} = 2\sqrt{2\ln2}\,\sigma_\nu.

For a Lorentzian written with HWHM γν\gamma_\nu,

L(ν)∝γν(ν−ν0)2+γν2,L(\nu) \propto \frac{\gamma_\nu} {(\nu-\nu_0)^2+\gamma_\nu^2},

the full width is

ΔνFWHM(L)=2γν.\Delta\nu_{\mathrm{FWHM}}^{(\mathrm L)} = 2\gamma_\nu.

A symbol Γ\Gamma may denote either of these widths or an angular-frequency decay rate. The equation defining Γ\Gamma is therefore part of the result.

LabelMeaningConversion
Gaussian σν\sigma_\nustandard deviationFWHM =22ln⁡2 σν=2\sqrt{2\ln2}\,\sigma_\nu
Lorentzian γν\gamma_\nuHWHMFWHM =2γν=2\gamma_\nu
FWHMseparation of the two half-maximum pointsprofile dependent
HWHMhalf of FWHM for a symmetric profileFWHM =2 HWHM=2\,\mathrm{HWHM}
1/e1/e half-widthoffset where amplitude or intensity falls to 1/e1/estate amplitude versus intensity
decay rateinverse time constantrelation to spectral width depends on coherence convention

The Line Shape Reference gives the canonical normalized profiles, convolution rules, and lifetime-broadening relations.

For a line narrow enough that the coordinate transformation is nearly linear across its width,

Δω≃2πΔν,\Delta\omega \simeq 2\pi\Delta\nu, Δν~≃Δνc,\Delta\tilde\nu \simeq \frac{\Delta\nu}{c},

where ν~\tilde\nu is in m−1\mathrm{m^{-1}}, and

Δλvac≃λvac2cΔν.\Delta\lambda_{\mathrm{vac}} \simeq \frac{\lambda_{\mathrm{vac}}^2}{c} \Delta\nu.

The last equation gives a positive width; the derivative dλ/dνd\lambda/d\nu itself is negative. For broad or asymmetric features, transform the two endpoints or the full profile rather than applying a single central Jacobian.

Resolving power is a dimensionless instrument or observation metric,

R=x0Δx,\mathcal R = \frac{x_0}{\Delta x},

for a declared coordinate and width convention. It is not itself a physical linewidth.

Molecular spectroscopy commonly marks upper-state quantum numbers with a prime and lower-state quantum numbers with a double prime:

J′andJ′′.J' \quad\text{and}\quad J''.

For absorption, define

ΔJ=J′−J′′.\Delta J = J'-J''.

The standard rotational branch letters are:

BranchΔJ\Delta JSimple absorption assignment
O−2-2J′=J′′−2J'=J''-2
P−1-1J′=J′′−1J'=J''-1
Q00J′=J′′J'=J''
R+1+1J′=J′′+1J'=J''+1
S+2+2J′=J′′+2J'=J''+2

Which branches are allowed depends on transition type, molecular symmetry, and angular-momentum coupling. The existence of a letter in this table is not a selection rule.

In the common simple-diatomic convention, the integer in a label such as R(3)R(3) is the lower-state rotational quantum number:

R(3):J′′=3⟶J′=4,P(3):J′′=3⟶J′=2,Q(3):J′′=3⟶J′=3.\begin{aligned} R(3):\quad &J''=3\longrightarrow J'=4, \\ P(3):\quad &J''=3\longrightarrow J'=2, \\ Q(3):\quad &J''=3\longrightarrow J'=3. \end{aligned}

Emission papers and specialized databases may order or label states differently. A line list should define its convention rather than relying on the reader to infer the direction.

A vibronic band is often identified by

(v′,v′′),(v',v''),

with upper and lower vibrational quantum numbers in that order. Thus the (1,0)(1,0) band and the line R(3)R(3) within it encode different parts of the assignment.

Open-shell molecules can carry both rotational angular momentum excluding spin, often NN, and total angular momentum including spin, JJ. A compound branch label can then encode both

ΔN=N′−N′′andΔJ=J′−J′′.\Delta N=N'-N'' \quad\text{and}\quad \Delta J=J'-J''.

For example, a source may use a two-letter label in which one letter tracks ΔN\Delta N and the other tracks ΔJ\Delta J. Superscripts and subscripts may also identify spin components, parity, KK, or fine-structure ladders. There is no safe universal decoding rule without the source’s definition.

The minimum defensible practice is to print the relevant upper and lower quantum numbers in a table and treat the compact branch string as a convenience label. See Rotational Spectroscopy and Term Symbol Reference for the underlying angular-momentum labels.

A spectrum or fitted line table is reproducible when it records:

  • the horizontal coordinate, unit, and vacuum/air/medium convention;
  • the refractive-index equation and environmental conditions for air or medium wavelengths;
  • observed, calculated, or Ritz provenance for line positions;
  • the vertical observable and whether it is a density per unit coordinate;
  • the incident and transmitted channels used to define TT;
  • logarithm base for absorbance;
  • absorption, scattering, or total-extinction scope for α\alpha, τ\tau, and σ\sigma;
  • species, isotope, internal state, temperature, pressure, and column density where relevant;
  • line-profile model, width convention, coordinate, and instrument-response treatment;
  • upper and lower quantum-number definitions for branch labels;
  • calibration, baseline, and uncertainty procedures; and
  • database release, query date, and original data source.

For machine-readable work, store the convention in metadata rather than in a plot caption alone. A numerical column named width or intensity is not a stable data model.

Treating air wavelength as photon energy divided by a different constant

Section titled “Treating air wavelength as photon energy divided by a different constant”

Photon energy is determined by frequency:

E=hν.E=h\nu.

At a stationary interface ν\nu does not change. The medium wavelength changes because the phase velocity changes; the photon has not acquired a different vacuum frequency merely because λmed\lambda_{\mathrm{med}} is shorter.

Confusing reciprocal centimetres with angular wavenumber

Section titled “Confusing reciprocal centimetres with angular wavenumber”

A spectroscopic value in cm−1\mathrm{cm^{-1}} normally means ν~=1/λvac\tilde\nu=1/\lambda_{\mathrm{vac}}. Inserting it as k=2π/λk=2\pi/\lambda introduces a factor of 2π2\pi.

Replacing ν\nu by c/λc/\lambda on the horizontal axis while leaving a “per hertz” vertical density unchanged does not conserve integrated area. Transform both coordinates and density.

Calling one minus transmittance the absorbance

Section titled “Calling one minus transmittance the absorbance”

1−T1-T is a linear missing-power fraction. Absorbance is logarithmic:

A10=−log⁡10T.A_{10}=-\log_{10}T.

Even the missing-power fraction is not necessarily absorptance when reflection and scattering occur.

For the same transmittance,

Ae=(ln⁡10)A10.A_{\mathrm e} = (\ln10)A_{10}.

A fitted concentration or cross section will inherit the factor-of-ln⁡10\ln10 error if the base is guessed incorrectly.

Mixing line-centre and integrated cross sections

Section titled “Mixing line-centre and integrated cross sections”

σ(ν0)\sigma(\nu_0) has units of area. ∫σ(ν)dν\int\sigma(\nu)d\nu has units of area times frequency. Their ratio depends on linewidth and line shape.

Neither “10 MHz10\,\mathrm{MHz}” nor “Γ=10 MHz\Gamma=10\,\mathrm{MHz}” reveals whether the value is FWHM, HWHM, a Gaussian standard deviation, an angular rate divided by 2π2\pi, or an instrument-limited width.

Reading a branch letter as a complete assignment

Section titled “Reading a branch letter as a complete assignment”

RR says ΔJ=+1\Delta J=+1 only in the declared branch convention. It does not specify electronic state, vibrational band, parity, spin component, or whether another angular momentum also changes.

A transition has vacuum wavelength λvac=780.000 nm\lambda_{\mathrm{vac}}=780.000\,\mathrm{nm}. Find ν\nu, ω\omega, ν~\tilde\nu in cm−1\mathrm{cm^{-1}}, and the photon energy in eV.

Solution

Using the exact SI values of cc, hh, and the elementary charge,

ν=cλvac=3.84349305×1014 Hz.\nu = \frac{c}{\lambda_{\mathrm{vac}}} = 3.84349305\times10^{14}\ \mathrm{Hz}.

Then

ω=2πν=2.41493791×1015 rad s−1.\omega = 2\pi\nu = 2.41493791\times10^{15}\ \mathrm{rad\,s^{-1}}.

The spectroscopic wavenumber is

ν~=1780.000×10−7 cm=1.28205128×104 cm−1.\tilde\nu = \frac{1}{780.000\times10^{-7}\ \mathrm{cm}} = 1.28205128\times10^4\ \mathrm{cm^{-1}}.

Finally,

Ee=hceλvac=1.58954101 eV.\frac{E}{e} = \frac{hc}{e\lambda_{\mathrm{vac}}} = 1.58954101\ \mathrm{eV}.

The wavelength carries six significant digits, so reporting more than six significant digits in the results would not represent measurement precision.

A line has λvac=500.000 nm\lambda_{\mathrm{vac}}=500.000\,\mathrm{nm}. Using nair=1.000277n_{\mathrm{air}}=1.000277, find its air wavelength. What happens to its frequency at a stationary vacuum–air interface?

Solution

The air wavelength is

λair=500.000 nm1.000277=499.8615 nm.\lambda_{\mathrm{air}} = \frac{500.000\ \mathrm{nm}}{1.000277} = 499.8615\ \mathrm{nm}.

The frequency remains

ν=cλvac=5.99584916×1014 Hz.\nu = \frac{c}{\lambda_{\mathrm{vac}}} = 5.99584916\times10^{14}\ \mathrm{Hz}.

The shorter medium wavelength reflects the smaller phase velocity, not a change in frequency.

A sample has transmittance T=0.200T=0.200. Find the decadic absorbance, Napierian absorbance, and optical depth for a pure-attenuation direct-beam model.

Solution

The decadic absorbance is

A10=−log⁡10(0.200)=0.698970.A_{10} = -\log_{10}(0.200) = 0.698970.

The Napierian absorbance is

Ae=−ln⁡(0.200)=1.609438.A_{\mathrm e} = -\ln(0.200) = 1.609438.

Under the stated model,

τ=Ae=1.609438.\tau = A_{\mathrm e} = 1.609438.

The numerical values differ because absorbance conventions use different logarithm bases.

Exercise 4: Column density and cross section

Section titled “Exercise 4: Column density and cross section”

A uniform ensemble has column density Ncol=2.00×1020 m−2N_{\mathrm{col}}=2.00\times10^{20}\,\mathrm{m^{-2}} and absorption cross section σ=3.00×10−21 m2\sigma=3.00\times10^{-21}\,\mathrm{m^2}. Find τ\tau, TT, and A10A_{10}.

Solution

The optical depth is

τ=Ncolσ=0.600.\tau = N_{\mathrm{col}}\sigma = 0.600.

Hence

T=e−0.600=0.548812,T = e^{-0.600} = 0.548812,

and

A10=τln⁡10=0.260577.A_{10} = \frac{\tau}{\ln10} = 0.260577.

Multiplying TT by 100100 gives 54.8812%54.8812\% transmittance; it does not give the absorbance.

Exercise 5: Molar coefficient to microscopic cross section

Section titled “Exercise 5: Molar coefficient to microscopic cross section”

A solution has ε10=1.50×104 L mol−1 cm−1\varepsilon_{10}=1.50\times10^4\, \mathrm{L\,mol^{-1}\,cm^{-1}}, concentration cM=20.0 μmol L−1c_{\mathrm M}=20.0\,\mu\mathrm{mol\,L^{-1}}, and path length L=1.00 cmL=1.00\,\mathrm{cm}. Find A10A_{10}, TT, τ\tau, and the corresponding microscopic cross section.

Solution

The concentration is

cM=2.00×10−5 mol L−1.c_{\mathrm M} = 2.00\times10^{-5}\ \mathrm{mol\,L^{-1}}.

Therefore

A10=ε10cML=0.300.A_{10} = \varepsilon_{10}c_{\mathrm M}L = 0.300.

The transmittance and optical depth are

T=10−0.300=0.501187,τ=(ln⁡10)(0.300)=0.690776.\begin{aligned} T &= 10^{-0.300} = 0.501187, \\ \tau &= (\ln10)(0.300) = 0.690776. \end{aligned}

Using the stated litre–mole–centimetre convention,

σ=ln⁡1010NAε10=5.735×10−21 m2.\begin{aligned} \sigma &= \frac{\ln10}{10N_{\mathrm A}} \varepsilon_{10} \\ &= 5.735\times10^{-21}\ \mathrm{m^2}. \end{aligned}

The conversion would change if the numerical value of ε\varepsilon used a different concentration or length unit.

A line is centred at ν0=500.0 THz\nu_0=500.0\,\mathrm{THz} and has ordinary-frequency FWHM Δν=100.0 MHz\Delta\nu=100.0\,\mathrm{MHz}. Find the central vacuum wavelength and the approximate FWHM in angular frequency, cm−1\mathrm{cm^{-1}}, and picometres.

Solution

The central wavelength is

λ0=cν0=599.5849 nm.\lambda_0 = \frac{c}{\nu_0} = 599.5849\ \mathrm{nm}.

The angular-frequency width is

Δω=2πΔν=6.28319×108 rad s−1.\Delta\omega = 2\pi\Delta\nu = 6.28319\times10^8\ \mathrm{rad\,s^{-1}}.

The spectroscopic-wavenumber width is

Δν~=Δνc=0.00333564 cm−1.\begin{aligned} \Delta\tilde\nu &= \frac{\Delta\nu}{c} \\ &= 0.00333564\ \mathrm{cm^{-1}}. \end{aligned}

The wavelength width is

Δλ≃λ02cΔν=0.119917 pm.\begin{aligned} \Delta\lambda &\simeq \frac{\lambda_0^2}{c}\Delta\nu \\ &= 0.119917\ \mathrm{pm}. \end{aligned}

Because Δν/ν0=2.0×10−7\Delta\nu/\nu_0=2.0\times10^{-7}, the local linear conversion is well justified.

In a simple diatomic absorption spectrum, decode R(4)R(4), P(4)P(4), and Q(4)Q(4) in terms of J′′J'' and J′J'. Does the notation alone prove all three lines are allowed?

Solution

The parenthesized number labels the lower state:

R(4):J′′=4,J′=5,P(4):J′′=4,J′=3,Q(4):J′′=4,J′=4.\begin{aligned} R(4):\quad &J''=4,\quad J'=5, \\ P(4):\quad &J''=4,\quad J'=3, \\ Q(4):\quad &J''=4,\quad J'=4. \end{aligned}

The labels encode ΔJ=+1,−1,0\Delta J=+1,-1,0, respectively. They do not prove that the branches are allowed. Electronic symmetry, transition multipolarity, parity, spin, and other angular momenta determine the actual selection rules.

Exercise 8: Audit an ambiguous line record

Section titled “Exercise 8: Audit an ambiguous line record”

A data file contains the row A = 0.50, sigma = 12500 cm^-1, Gamma = 10 MHz, S = 2.1e-20. List the minimum questions needed before using it in a model.

Solution

At least the following information is missing:

  • whether AA is decadic or Napierian absorbance, an Einstein coefficient, or another quantity;
  • if it is absorbance, the incident and transmitted channels and logarithm base;
  • whether “sigma” is the spectroscopic vacuum wavenumber ν~=1/λvac\tilde\nu=1/\lambda_{\mathrm{vac}} or another symbol;
  • whether the position is observed or Ritz/calculated;
  • whether Γ\Gamma is FWHM, HWHM, Gaussian standard deviation, or a decay rate expressed after division by 2π2\pi;
  • whether the width is observed, deconvolved, homogeneous, or instrument-limited;
  • what SS means, its units, and the coordinate used by any defining integral;
  • which species, isotope, states, temperature, and pressure the row describes; and
  • the source, uncertainty, and database release.

The row cannot be repaired by guessing from the numerical magnitudes. Its schema needs physical definitions.