Why Does Spectral Line Darkening Occur Despite Photon Re-Emission?

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In summary, spectral line darkening occurs due to the complex interactions between photons and atomic systems. When photons are absorbed by atoms, they can be re-emitted in different directions, leading to a decrease in the intensity of specific spectral lines. This phenomenon is influenced by factors such as the density of absorbing atoms, the Doppler effect, and the redistribution of energy levels. As a result, despite the re-emission of photons, the overall effect is a reduction in the observed brightness of certain spectral lines, contributing to the darkening observed in spectra.
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Joe Prendergast
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Suppose a photon from the sun's photosphere, initially traveling toward earth, is absorbed by an atom in the sun's chromosphere. The electron then transitions to its first excited state and spectral darkening is observed at a distinct wavelength on earth. I've read that the electron only stays in its excited state for a brief instant. When the electron transitions back to its ground state it emits a photon with the same wavelength where the spectral darkening had occurred. Why would this not get rid of the darkening seen from earth? Is it because the emitted photon travels in a random direction (not necessarily toward earth)?
 
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Joe Prendergast said:
Is it because the emitted photon travels in a random direction (not necessarily toward earth)?
Yes, that's correct.
 
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That may be true in the low density chromosphere, but there is more to the question of "line darkening" (usually called absorption lines, or "Fraunhoefer lines") because most of those lines are formed in the deep photosphere where the density is very high. In very high density conditions, often when an atom absorbs a photon it experiences a collision with another particle that removes that excitation energy before the photon can be reemitted. This "absorbs" the photon instead of "scattering" it, in which case the energy shows up somewhere else in the continuum spectrum of H minus opacity, rather than in the line. So there it is not the direction the photon is traveling that gets changed, it is the wavelength where the energy eventually emerges.

And even when it is scattering that is causing the absorption line, the change in direction alone could not produce such a darkening, because the Sun is a sphere so making the light come out at a different angle means it is still seen somewhere outside the Sun, so that wavelength photon would eventually be seen coming from somewhere on the Sun by somebody (and the Earth is not in a special position to see anything different). To get a true darkening still requires absorption, it's just that if you bounce the light back downward toward the Sun, it has a good chance of being absorbed by non scattering processes before it gets out again. So absorption lines are typically caused by a combination of scattering that changes the direction and photon destruction that moves the energy out of the line bandwidth.
 
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FAQ: Why Does Spectral Line Darkening Occur Despite Photon Re-Emission?

What is spectral line darkening?

Spectral line darkening, often referred to as absorption lines or Fraunhofer lines in the context of the Sun, occurs when specific wavelengths of light are absorbed by atoms or molecules in a star's atmosphere. This absorption creates dark lines in the spectrum when it is observed through a spectrometer.

Why does spectral line darkening occur despite photon re-emission?

Spectral line darkening occurs because the absorbed photons are often re-emitted in random directions rather than in the original direction of the incoming light. This scattering causes a net loss of intensity along the line of sight, resulting in dark lines in the observed spectrum.

What role do atomic transitions play in spectral line darkening?

Atomic transitions play a crucial role in spectral line darkening. When atoms or molecules absorb photons, electrons are excited to higher energy levels. These transitions are highly specific to certain wavelengths, creating distinct absorption lines. The re-emission of these photons is not directional, leading to the observed darkening.

How does the temperature of a star's atmosphere affect spectral line darkening?

The temperature of a star's atmosphere affects the population of atoms and molecules in different energy states. Higher temperatures can ionize atoms, reducing the number of available absorbers, while lower temperatures can increase the number of atoms in a state that can absorb specific wavelengths. This variation influences the depth and width of the spectral lines.

Can spectral line darkening provide information about the composition of a star?

Yes, spectral line darkening can provide valuable information about the composition of a star. By analyzing the specific wavelengths at which absorption lines occur, scientists can identify the elements and molecules present in the star's atmosphere. This technique, known as spectroscopy, is fundamental in astrophysics for determining the chemical makeup of celestial objects.

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