Spectral line

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Spectral-lines-continuous.svg
Continuous spectrum
Spectral-lines-absorption.svg
Absorption spectrum with Absorption lines (discrete spectrum)
Absorption lines for air, under indirect illumination, so that the gas is not directly between source and detector. Here, Fraunhofer lines in sunlight and Rayleigh scattering of this sunlight is the "source." This is the spectrum of a blue sky somewhat close to the horizon, looking east with the sun to the west at around 3-4 pm on a clear day. Spectrum of blue sky.svg
Absorption lines for air, under indirect illumination, so that the gas is not directly between source and detector. Here, Fraunhofer lines in sunlight and Rayleigh scattering of this sunlight is the "source." This is the spectrum of a blue sky somewhat close to the horizon, looking east with the sun to the west at around 3–4 pm on a clear day.

A spectral line is a weaker or stronger region in an otherwise uniform and continuous spectrum. It may result from emission or absorption of light in a narrow frequency range, compared with the nearby frequencies. Spectral lines are often used to identify atoms and molecules. These "fingerprints" can be compared to the previously collected ones of atoms [1] and molecules, [2] and are thus used to identify the atomic and molecular components of stars and planets, which would otherwise be impossible.

Contents

Types of line spectra

Continuous spectrum of an incandescent lamp (mid) and discrete spectrum lines of a fluorescent lamp (bottom) Simple spectroscope.jpg
Continuous spectrum of an incandescent lamp (mid) and discrete spectrum lines of a fluorescent lamp (bottom)

Spectral lines are the result of interaction between a quantum system (usually atoms, but sometimes molecules or atomic nuclei) and a single photon. When a photon has about the right amount of energy (which is connected to its frequency) [3] to allow a change in the energy state of the system (in the case of an atom this is usually an electron changing orbitals), the photon is absorbed. Then the energy will be spontaneously re-emitted, either as one photon at the same frequency as the original one or in a cascade, where the sum of the energies of the photons emitted will be equal to the energy of the one absorbed (assuming the system returns to its original state).

A spectral line may be observed either as an emission line or an absorption line. Which type of line is observed depends on the type of material and its temperature relative to another emission source. An absorption line is produced when photons from a hot, broad spectrum source pass through a cooler material. The intensity of light, over a narrow frequency range, is reduced due to absorption by the material and re-emission in random directions. By contrast, a bright emission line is produced when photons from a hot material are detected, perhaps in the presence of a broad spectrum from a cooler source. The intensity of light, over a narrow frequency range, is increased due to emission by the hot material.

Spectral lines are highly atom-specific, and can be used to identify the chemical composition of any medium. Several elements, including helium, thallium, and caesium, were discovered by spectroscopic means. Spectral lines also depend on the temperature and density of the material, so they are widely used to determine the physical conditions of stars and other celestial bodies that cannot be analyzed by other means.

Depending on the material and its physical conditions, the energy of the involved photons can vary widely, with the spectral lines observed across the electromagnetic spectrum, from radio waves to gamma rays.

Nomenclature

Strong spectral lines in the visible part of the electromagnetic spectrum often have a unique Fraunhofer line designation, such as K for a line at 393.366 nm emerging from singly-ionized calcium atom, Ca+, though some of the Fraunhofer "lines" are blends of multiple lines from several different species.

In other cases, the lines are designated according to the level of ionization by adding a Roman numeral to the designation of the chemical element. Neutral atoms are denoted with the Roman numeral I, singly ionized atoms with II, and so on, so that, for example:

Cu II copper ion with +1 charge, Cu1+

Fe III iron ion with +2 charge, Fe2+

More detailed designations usually include the line wavelength and may include a multiplet number (for atomic lines) or band designation (for molecular lines). Many spectral lines of atomic hydrogen also have designations within their respective series, such as the Lyman series or Balmer series. Originally all spectral lines were classified into series: the principal series , sharp series , and diffuse series . These series exist across atoms of all elements, and the patterns for all atoms are well-predicted by the Rydberg-Ritz formula. These series were later associated with suborbitals.

Line broadening and shift

There are a number of effects which control spectral line shape. A spectral line extends over a tiny spectral band with a nonzero range of frequencies, not a single frequency (i.e., a nonzero spectral width). In addition, its center may be shifted from its nominal central wavelength. There are several reasons for this broadening and shift. These reasons may be divided into two general categories – broadening due to local conditions and broadening due to extended conditions. Broadening due to local conditions is due to effects which hold in a small region around the emitting element, usually small enough to assure local thermodynamic equilibrium. Broadening due to extended conditions may result from changes to the spectral distribution of the radiation as it traverses its path to the observer. It also may result from the combining of radiation from a number of regions which are far from each other.

Broadening due to local effects

Natural broadening

The lifetime of excited states results in natural broadening, also known as lifetime broadening. The uncertainty principle relates the lifetime of an excited state (due to spontaneous radiative decay or the Auger process) with the uncertainty of its energy. Some authors use the term "radiative broadening" to refer specifically to the part of natural broadening caused by the spontaneous radiative decay. [4] A short lifetime will have a large energy uncertainty and a broad emission. This broadening effect results in an unshifted Lorentzian profile. The natural broadening can be experimentally altered only to the extent that decay rates can be artificially suppressed or enhanced. [5]

Thermal Doppler broadening

The atoms in a gas which are emitting radiation will have a distribution of velocities. Each photon emitted will be "red"- or "blue"-shifted by the Doppler effect depending on the velocity of the atom relative to the observer. The higher the temperature of the gas, the wider the distribution of velocities in the gas. Since the spectral line is a combination of all of the emitted radiation, the higher the temperature of the gas, the broader the spectral line emitted from that gas. This broadening effect is described by a Gaussian profile and there is no associated shift.

Pressure broadening

The presence of nearby particles will affect the radiation emitted by an individual particle. There are two limiting cases by which this occurs:

  • Impact pressure broadening or collisional broadening: The collision of other particles with the light emitting particle interrupts the emission process, and by shortening the characteristic time for the process, increases the uncertainty in the energy emitted (as occurs in natural broadening). [6] The duration of the collision is much shorter than the lifetime of the emission process. This effect depends on both the density and the temperature of the gas. The broadening effect is described by a Lorentzian profile and there may be an associated shift.
  • Quasistatic pressure broadening: The presence of other particles shifts the energy levels in the emitting particle (see spectral band), thereby altering the frequency of the emitted radiation. The duration of the influence is much longer than the lifetime of the emission process. This effect depends on the density of the gas, but is rather insensitive to temperature. The form of the line profile is determined by the functional form of the perturbing force with respect to distance from the perturbing particle. There may also be a shift in the line center. The general expression for the lineshape resulting from quasistatic pressure broadening is a 4-parameter generalization of the Gaussian distribution known as a stable distribution. [7]

Pressure broadening may also be classified by the nature of the perturbing force as follows:

  • Linear Stark broadening occurs via the linear Stark effect, which results from the interaction of an emitter with an electric field of a charged particle at a distance , causing a shift in energy that is linear in the field strength.
  • Resonance broadening occurs when the perturbing particle is of the same type as the emitting particle, which introduces the possibility of an energy exchange process.
  • Quadratic Stark broadening occurs via the quadratic Stark effect, which results from the interaction of an emitter with an electric field, causing a shift in energy that is quadratic in the field strength.
  • Van der Waals broadening occurs when the emitting particle is being perturbed by Van der Waals forces. For the quasistatic case, a Van der Waals profile [note 1] is often useful in describing the profile. The energy shift as a function of distance between the interacting particles is given in the wings by e.g. the Lennard-Jones potential.

Inhomogeneous broadening

Inhomogeneous broadening is a general term for broadening because some emitting particles are in a different local environment from others, and therefore emit at a different frequency. This term is used especially for solids, where surfaces, grain boundaries, and stoichiometry variations can create a variety of local environments for a given atom to occupy. In liquids, the effects of inhomogeneous broadening is sometimes reduced by a process called motional narrowing .

Broadening due to non-local effects

Certain types of broadening are the result of conditions over a large region of space rather than simply upon conditions that are local to the emitting particle.

Opacity broadening

Opacity broadening is an example of a non-local broadening mechanism. Electromagnetic radiation emitted at a particular point in space can be reabsorbed as it travels through space. This absorption depends on wavelength. The line is broadened because the photons at the line center have a greater reabsorption probability than the photons at the line wings. Indeed, the reabsorption near the line center may be so great as to cause a self reversal in which the intensity at the center of the line is less than in the wings. This process is also sometimes called self-absorption.

Macroscopic Doppler broadening

Radiation emitted by a moving source is subject to Doppler shift due to a finite line-of-sight velocity projection. If different parts of the emitting body have different velocities (along the line of sight), the resulting line will be broadened, with the line width proportional to the width of the velocity distribution. For example, radiation emitted from a distant rotating body, such as a star, will be broadened due to the line-of-sight variations in velocity on opposite sides of the star (this effect usually referred to as rotational broadening). The greater the rate of rotation, the broader the line. Another example is an imploding plasma shell in a Z-pinch.

Combined effects

Each of these mechanisms can act in isolation or in combination with others. Assuming each effect is independent, the observed line profile is a convolution of the line profiles of each mechanism. For example, a combination of the thermal Doppler broadening and the impact pressure broadening yields a Voigt profile.

However, the different line broadening mechanisms are not always independent. For example, the collisional effects and the motional Doppler shifts can act in a coherent manner, resulting under some conditions even in a collisional narrowing, known as the Dicke effect.

Spectral lines of chemical elements

Bands

The phrase "spectral lines", when not qualified, usually refers to lines having wavelengths in the visible band of the full electromagnetic spectrum. Many spectral lines occur at wavelengths outside this range. At shorter wavelengths, which correspond to higher energies, ultraviolet spectral lines include the Lyman series of hydrogen. At the much shorter wavelengths of X-rays, the lines are known as characteristic X-rays because they remain largely unchanged for a given chemical element, independent of their chemical environment. Longer wavelengths correspond to lower energies, where the infrared spectral lines include the Paschen series of hydrogen. At even longer wavelengths, the radio spectrum includes the 21-cm line used to detect neutral hydrogen throughout the cosmos.

Visible light

For each element, the following table shows the spectral lines which appear in the visible spectrum at about 400-700 nm.

Spectral lines of the chemical elements
ElementZSymbolSpectral lines
hydrogen 1H Hydrogen spectrum visible.png
helium 2He Helium spectrum visible.png
lithium 3Li Lithium spectrum visible.png
beryllium 4Be Beryllium spectrum visible.png
boron 5B Boron spectrum visible.png
carbon 6C Carbon spectrum visible.png
nitrogen 7N Nitrogen spectrum visible.png
oxygen 8O Oxygen spectrum visible.png
fluorine 9F Fluorine spectrum visible.png
neon 10Ne Neon spectrum visible.png
sodium 11Na Sodium spectrum visible.png
magnesium 12Mg Magnesium spectrum visible.png
aluminium 13Al Aluminium spectrum visible.png
silicon 14Si Silicon spectrum visible.png
phosphorus 15P Phosphorus spectrum visible.png
sulfur 16S Sulfur spectrum visible.png
chlorine 17Cl Chlorine spectrum visible.png
argon 18Ar Argon spectrum visible.png
potassium 19K Potassium spectrum visible.png
calcium 20Ca Calcium spectrum visible.png
scandium 21Sc Scandium spectrum visible.png
titanium 22Ti Titanium spectrum visible.png
vanadium 23V Vanadium spectrum visible.png
chromium 24Cr Chromium spectrum visible.png
manganese 25Mn Manganese spectrum visible.png
iron 26Fe Iron spectrum visible.png
cobalt 27Co Cobalt spectrum visible.png
nickel 28Ni Nickel spectrum visible.png
copper 29Cu Copper spectrum visible.png
zinc 30Zn Zinc spectrum visible.png
gallium 31Ga Gallium spectrum visible.png
germanium 32Ge Germanium spectrum visible.png
arsenic 33As Arsenic spectrum visible.png
selenium 34Se Selenium spectrum visible.png
bromine 35Br Bromine spectrum visible.png
krypton 36Kr Krypton spectrum visible.png
rubidium 37Rb Rubidium spectrum visible.png
strontium 38Sr Strontium spectrum visible.png
yttrium 39Y Yttrium spectrum visible.png
zirconium 40Zr Zirconium spectrum visible.png
niobium 41Nb Niobium spectrum visible.png
molybdenum 42Mo Molybdenum spectrum visible.png
technetium 43Tc Technetium spectrum visible.png
ruthenium 44Ru Ruthenium spectrum visible.png
rhodium 45Rh Rhodium spectrum visible.png
palladium 46Pd Palladium spectrum visible.png
silver 47Ag Silver spectrum visible.png
cadmium 48Cd Cadmium spectrum visible.png
indium 49In Indium spectrum visible.png
tin 50Sn Tin spectrum visible.png
antimony 51Sb Antimony spectrum visible.png
tellurium 52Te Tellurium spectrum visible.png
iodine 53I Iodine spectrum visible.png
xenon 54Xe Xenon spectrum visible.png
caesium 55Cs Caesium spectrum visible.png
barium 56Ba Barium spectrum visible.png
lanthanum 57La Lanthanum spectrum visible.png
cerium 58Ce Cerium spectrum visible.png
praseodymium 59Pr Praseodymium spectrum visible.png
neodymium 60Nd Neodymium spectrum visible.png
promethium 61Pm Promethium spectrum visible.png
samarium 62Sm Samarium spectrum visible.png
europium 63Eu Europium spectrum visible.png
gadolinium 64Gd Gadolinium spectrum visible.png
terbium 65Tb Terbium spectrum visible.png
dysprosium 66Dy Dysprosium spectrum visible.png
holmium 67Ho Holmium spectrum visible.png
erbium 68Er Erbium spectrum visible.png
thulium 69Tm Thulium spectrum visible.png
ytterbium 70Yb Ytterbium spectrum visible.png
lutetium 71Lu Lutetium spectrum visible.png
hafnium 72Hf Hafnium spectrum visible.png
tantalum 73Ta Tantalum spectrum visible.png
tungsten 74W Tungsten spectrum visible.png
rhenium 75Re Rhenium spectrum visible.png
osmium 76Os Osmium spectrum visible.png
iridium 77Ir Iridium spectrum visible.png
platinum 78Pt Platinum spectrum visible.png
gold 79Au Gold spectrum visible.png
mercury 80Hg Mercury spectrum visible.png
thallium 81Tl Thallium spectrum visible.png
lead 82Pb Lead spectrum visible.png
bismuth 83Bi Bismuth spectrum visible.png
polonium 84Po Polonium spectrum visible.png
astatine 85At
radon 86Rn Radon spectrum visible.png
francium 87Fr
radium 88Ra Radium spectrum visible.png
actinium 89Ac Actinium spectrum visible.png
thorium 90Th Thorium spectrum visible.png
protactinium 91Pa Protactinium spectrum visible.png
uranium 92U Uranium spectrum visible.png
neptunium 93Np Neptunium spectrum visible.png
plutonium 94Pu Plutonium spectrum visible.png
americium 95Am Americium spectrum visible.png
curium 96Cm Curium spectrum visible.png
berkelium 97Bk Berkelium spectrum visible.png
californium 98Cf Californium spectrum visible.png
einsteinium 99Es Einsteinium spectrum visible.png
fermiumoganesson101118FmOg

See also

Notes

  1. "Van der Waals profile" appears as lowercase in almost all sources, such as: Statistical mechanics of the liquid surface by Clive Anthony Croxton, 1980, A Wiley-Interscience publication, ISBN   0-471-27663-4, ISBN   978-0-471-27663-0; and in Journal of technical physics, Volume 36, by Instytut Podstawowych Problemów Techniki (Polska Akademia Nauk), publisher: Państwowe Wydawn. Naukowe., 1995,

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References

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Further reading