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Einstein coefficients
View on WikipediaIn atomic, molecular, and optical physics, the Einstein coefficients are quantities describing the probability of absorption or emission of a photon by an atom or molecule.[1] The Einstein A coefficients are related to the rate of spontaneous emission of light, and the Einstein B coefficients are related to the absorption and stimulated emission of light. Throughout this article, "light" refers to any electromagnetic radiation, not necessarily in the visible spectrum.
These coefficients are named after Albert Einstein, who proposed them in 1916.
Spectral lines
[edit]In physics, one thinks of a spectral line from two viewpoints.
An emission line is formed when an atom or molecule makes a transition from a particular discrete energy level E2 of an atom, to a lower energy level E1, emitting a photon of a particular energy and wavelength. A spectrum of many such photons will show an emission spike at the wavelength associated with these photons.
An absorption line is formed when an atom or molecule makes a transition from a lower, E1, to a higher discrete energy state, E2, with a photon being absorbed in the process. These absorbed photons generally come from background continuum radiation (the full spectrum of electromagnetic radiation) and a spectrum will show a drop in the continuum radiation at the wavelength associated with the absorbed photons.
The two states must be bound states in which the electron is bound to the atom or molecule, so the transition is sometimes referred to as a "bound–bound" transition, as opposed to a transition in which the electron is ejected out of the atom completely ("bound–free" transition) into a continuum state, leaving an ionized atom, and generating continuum radiation.
A photon with an energy equal to the difference E2 − E1 between the energy levels is released or absorbed in the process. The frequency ν at which the spectral line occurs is related to the photon energy by Bohr's frequency condition E2 − E1 = hν where h denotes the Planck constant.[2][3][4][5][6][7]
Emission and absorption coefficients
[edit]An atomic spectral line refers to emission and absorption events in a gas in which is the density of atoms in the upper-energy state for the line, and is the density of atoms in the lower-energy state for the line.
The emission of atomic line radiation at frequency ν may be described by an emission coefficient with units of energy/(time × volume × solid angle). ε dt dV dΩ is then the energy emitted by a volume element in time into solid angle . For atomic line radiation, where is the Einstein coefficient for spontaneous emission, which is fixed by the intrinsic properties of the relevant atom for the two relevant energy levels.
The absorption of atomic line radiation may be described by an absorption coefficient with units of 1/length. The expression κ' dx gives the fraction of intensity absorbed for a light beam at frequency ν while traveling distance dx. The absorption coefficient is given by where and are the Einstein coefficients for photon absorption and induced emission respectively. Like the coefficient , these are also fixed by the intrinsic properties of the relevant atom for the two relevant energy levels. For thermodynamics and for the application of Kirchhoff's law, it is necessary that the total absorption be expressed as the algebraic sum of two components, described respectively by and , which may be regarded as positive and negative absorption, which are, respectively, the direct photon absorption, and what is commonly called stimulated or induced emission.[8][9][10]
The above equations have ignored the influence of the spectroscopic line shape. To be accurate, the above equations need to be multiplied by the (normalized) spectral line shape, in which case the units will change to include a 1/Hz term.
Under conditions of thermodynamic equilibrium, the number densities and , the Einstein coefficients, and the spectral energy density provide sufficient information to determine the absorption and emission rates.
Equilibrium conditions
[edit]The number densities and are set by the physical state of the gas in which the spectral line occurs, including the local spectral radiance (or, in some presentations, the local spectral radiant energy density). When that state is either one of strict thermodynamic equilibrium, or one of so-called "local thermodynamic equilibrium",[11][12][13] then the distribution of atomic states of excitation (which includes and ) determines the rates of atomic emissions and absorptions to be such that Kirchhoff's law of equality of radiative absorptivity and emissivity holds. In strict thermodynamic equilibrium, the radiation field is said to be black-body radiation and is described by Planck's law. For local thermodynamic equilibrium, the radiation field does not have to be a black-body field, but the rate of interatomic collisions must vastly exceed the rates of absorption and emission of quanta of light, so that the interatomic collisions entirely dominate the distribution of states of atomic excitation. Circumstances occur in which local thermodynamic equilibrium does not prevail, because the strong radiative effects overwhelm the tendency to the Maxwell–Boltzmann distribution of molecular velocities. For example, in the atmosphere of the Sun, the great strength of the radiation dominates. In the upper atmosphere of the Earth, at altitudes over 100 km, the rarity of intermolecular collisions is decisive.
In the cases of thermodynamic equilibrium and of local thermodynamic equilibrium, the number densities of the atoms, both excited and unexcited, may be calculated from the Maxwell–Boltzmann distribution, but for other cases, (e.g. lasers) the calculation is more complicated.
Einstein coefficients
[edit]In 1916, Albert Einstein proposed that there are three processes occurring in the formation of an atomic spectral line. The three processes are referred to as spontaneous emission, stimulated emission, and absorption. With each is associated an Einstein coefficient, which is a measure of the probability of that particular process occurring. Einstein considered the case of isotropic radiation of frequency ν and spectral energy density ρ(ν).[3][14][15][16] Paul Dirac derived the coefficients in a 1927 paper titled "The Quantum Theory of the Emission and Absorption of Radiation".[17][18]
Various formulations
[edit]Hilborn has compared various formulations for derivations for the Einstein coefficients, by various authors.[19] For example, Herzberg works with irradiance and wavenumber;[20] Yariv works with energy per unit volume per unit frequency interval,[21] as is the case in the more recent (2008) [22] formulation. Mihalas & Weibel-Mihalas work with radiance and frequency,[13] as does Chandrasekhar,[23] and Goody & Yung;[24] Loudon uses angular frequency and radiance.[25]
Spontaneous emission
[edit]
Spontaneous emission is the process by which an electron "spontaneously" (i.e. without any outside influence) decays from a higher energy level to a lower one. The process is described by the Einstein coefficient A21 (s−1), which gives the probability per unit time that an electron in state 2 with energy will decay spontaneously to state 1 with energy , emitting a photon with an energy E2 − E1 = hν. Due to the energy-time uncertainty principle, the transition actually produces photons within a narrow range of frequencies called the spectral linewidth. If is the number density of atoms in state i , then the change in the number density of atoms in state 2 per unit time due to spontaneous emission will be
The same process results in an increase in the population of state 1:
Stimulated emission
[edit]
Stimulated emission (also known as induced emission) is the process by which an electron is induced to jump from a higher energy level to a lower one by the presence of electromagnetic radiation at (or near) the frequency of the transition. From the thermodynamic viewpoint, this process must be regarded as negative absorption. The process is described by the Einstein coefficient (m3 J−1 s−2), which gives the probability per unit time per unit energy density of the radiation field per unit frequency that an electron in state 2 with energy will decay to state 1 with energy , emitting a photon with an energy E2 − E1 = hν. The change in the number density of atoms in state 1 per unit time due to induced emission will be where denotes the spectral energy density of the isotropic radiation field at the frequency of the transition (see Planck's law).
Stimulated emission is one of the fundamental processes that led to the development of the laser. Laser radiation is, however, very far from the present case of isotropic radiation.
Photon absorption
[edit]
Absorption is the process by which a photon is absorbed by the atom, causing an electron to jump from a lower energy level to a higher one. The process is described by the Einstein coefficient (m3 J−1 s−2), which gives the probability per unit time per unit energy density of the radiation field per unit frequency that an electron in state 1 with energy will absorb a photon with an energy E2 − E1 = hν and jump to state 2 with energy . The change in the number density of atoms in state 1 per unit time due to absorption will be
Detailed balancing
[edit]The Einstein coefficients are fixed probabilities per time associated with each atom, and do not depend on the state of the gas of which the atoms are a part. Therefore, any relationship that we can derive between the coefficients at, say, thermodynamic equilibrium will be valid universally.
At thermodynamic equilibrium, we will have a simple balancing, in which the net change in the number of any excited atoms is zero, being balanced by loss and gain due to all processes. With respect to bound-bound transitions, we will have detailed balancing as well, which states that the net exchange between any two levels will be balanced. This is because the probabilities of transition cannot be affected by the presence or absence of other excited atoms. Detailed balance (valid only at equilibrium) requires that the change in time of the number of atoms in level 1 due to the above three processes be zero:
Along with detailed balancing, at temperature T we may use our knowledge of the equilibrium energy distribution of the atoms, as stated in the Maxwell–Boltzmann distribution, and the equilibrium distribution of the photons, as stated in Planck's law of black body radiation to derive universal relationships between the Einstein coefficients.
From Boltzmann distribution we have for the number of excited atomic species i: where n is the total number density of the atomic species, excited and unexcited, k is the Boltzmann constant, T is the temperature, is the degeneracy (also called the multiplicity) of state i, and Z is the partition function. From Planck's law of black-body radiation at temperature T we have for the spectral radiance (radiance is energy per unit time per unit solid angle per unit projected area, when integrated over an appropriate spectral interval)[26] at frequency ν where[27] where is the speed of light and is the Planck constant.
Substituting these expressions into the equation of detailed balancing and remembering that E2 − E1 = hν yields or
The above equation must hold at any temperature, so from one gets and from
Therefore, the three Einstein coefficients are interrelated by and
When this relation is inserted into the original equation, one can also find a relation between and , involving Planck's law.
Oscillator strengths
[edit]The oscillator strength is defined by the following relation to the cross section for absorption:[19]
where is the electron charge, is the electron mass, and and are normalized distribution functions in frequency and angular frequency respectively. This allows all three Einstein coefficients to be expressed in terms of the single oscillator strength associated with the particular atomic spectral line:
Dipole approximation
[edit]The value of A and B coefficients can be calculated using quantum mechanics where dipole approximations in time dependent perturbation theory is used. While the calculation of B coefficient can be done easily, that of A coefficient requires using results of second quantization. This is because the theory developed by dipole approximation and time dependent perturbation theory gives a semiclassical description of electronic transition which goes to zero as perturbing fields go to zero. The A coefficient which governs spontaneous emission should not go to zero as perturbing fields go to zero. The result for transition rates of different electronic levels as a result of spontaneous emission is given as (in SI units):[28][19][29]
For B coefficient, straightforward application of dipole approximation in time dependent perturbation theory yields (in SI units):[30][29]
Note that the rate of transition formula depends on dipole moment operator. For higher order approximations, it involves quadrupole moment and other similar terms.
Here, the B coefficients are chosen to correspond to energy distribution function. Often these different definitions of B coefficients are distinguished by superscript, for example, where term corresponds to frequency distribution and term corresponds to distribution.[19] The formulas for B coefficients varies inversely to that of the energy distribution chosen, so that the transition rate is same regardless of convention.
Hence, AB coefficients are calculated using dipole approximation as: where and B coefficients correspond to energy distribution function.
Hence the following ratios are also derived: and
Derivation of Planck's law
[edit]It follows from theory that:[29] where and are number of occupied energy levels of and respectively, where . Note that from time dependent perturbation theory application, the fact that only radiation whose is close to value of can produce respective stimulated emission or absorption, is used.
Where Maxwell distribution involving and ensures
Solving for for equilibrium condition using the above equations and ratios while generalizing to , we get: which is the angular frequency energy distribution from Planck's law.[29]
See also
[edit]- Transition dipole moment
- Oscillator strength
- Breit–Wigner distribution
- Electronic configuration
- Fano resonance
- Siegbahn notation
- Atomic spectroscopy
- Molecular radiation, continuous spectra emitted by molecules
References
[edit]- ^ Hilborn, Robert C. (1982). "Einstein coefficients, cross sections, f values, dipole moments, and all that". American Journal of Physics. 50 (11): 982–986. arXiv:physics/0202029. Bibcode:1982AmJPh..50..982H. doi:10.1119/1.12937. ISSN 0002-9505. S2CID 119050355.
- ^ Bohr, N. (1913). "On the constitution of atoms and molecules" (PDF). Philosophical Magazine. 26 (153): 1–25. Bibcode:1913PMag...26..476B. doi:10.1080/14786441308634993. Archived from the original (PDF) on 2017-08-09. Retrieved 2011-12-02.
- ^ a b Einstein, A. (1916). "Strahlungs-Emission und -Absorption nach der Quantentheorie". Verhandlungen der Deutschen Physikalischen Gesellschaft. 18: 318–323. Bibcode:1916DPhyG..18..318E. Translated in Alfred Engel. The Berlin Years: Writings, 1914-1917. Vol. 6. pp. 212–216.
- ^ Sommerfeld, A. (1923). Atomic Structure and Spectral Lines. Brose, H. L. (transl.) (from 3rd German ed.). Methuen. p. 43.
- ^ Heisenberg 1925, p. 108.
- ^ Brillouin, L. (1970). Relativity Reexamined. Academic Press. p. 31. ISBN 978-0-12-134945-5.
- ^ Jammer, M. (1989). The Conceptual Development of Quantum Mechanics (2nd ed.). Tomash Publishers American Institute of Physics. pp. 113, 115. ISBN 0-88318-617-9.
- ^ Weinstein, M. A. (1960). "On the validity of Kirchhoff's law for a freely radiating body". American Journal of Physics. 28 (2): 123–25. Bibcode:1960AmJPh..28..123W. doi:10.1119/1.1935075.
- ^ Burkhard, D. G.; Lochhead, J. V. S.; Penchina, C. M. (1972). "On the validity of Kirchhoff's law in a nonequilibrium environment". American Journal of Physics. 40 (12): 1794–1798. Bibcode:1972AmJPh..40.1794B. doi:10.1119/1.1987065.
- ^ Baltes, H. P. (1976). On the validity of Kirchhoff's law of heat radiation for a body in a nonequilibrium environment, Chapter 1, pages 1–25 of Progress in Optics XIII, edited by E. Wolf, North-Holland, ISSN 0079-6638.
- ^ Milne, E. A. (1928). "The effect of collisions on monochromatic radiative equilibrium". Monthly Notices of the Royal Astronomical Society. 88 (6): 493–502. Bibcode:1928MNRAS..88..493M. doi:10.1093/mnras/88.6.493.
- ^ Chandrasekhar, S. (1950), p. 7.
- ^ a b Mihalas, D., Weibel-Mihalas, B. (1984), pp. 329–330.
- ^ Loudon, R. (2000), Section 1.5, pp. 16–19.
- ^ Einstein, A. (1916). "Zur Quantentheorie der Strahlung". Mitteilungen der Physikalischen Gessellschaft Zürich. 18: 47–62. Bibcode:1916PhyGZ..18...47E.
- ^ Einstein, A. (1917). "Zur Quantentheorie der Strahlung". Physikalische Zeitschrift. 18: 121–128. Bibcode:1917PhyZ...18..121E. Translated in ter Haar, D. (1967). The Old Quantum Theory. Pergamon. pp. 167–183. LCCN 66029628. Also in Boorse, H. A., Motz, L. (1966). The world of the atom, edited with commentaries, Basic Books, Inc., New York, pp. 888–901.
- ^ Dirac, Paul (1927). "The quantum theory of the emission and absorption of radiation". Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 114 (767): 243–265. Bibcode:1927RSPSA.114..243D. doi:10.1098/rspa.1927.0039. ISSN 0950-1207.
- ^ Duck, Ian; Sudarshan, E.C.G. (1998). "Chapter 6: Dirac's Invention of Quantum Field Theory". Pauli and the Spin-Statistics Theorem. World Scientific Publishing. pp. 149–167. ISBN 978-9810231149.
- ^ a b c d Hilborn, Robert (2002). "Einstein coefficients, cross sections, f values, dipole moments, and all that" (PDF).
- ^ Herzberg, G. (1950).
- ^ Yariv, A. (1967/1989), pp. 171–173.
- ^ Garrison, J. C., Chiao, R. Y. (2008), pp. 15–19.
- ^ Chandrasekhar, S. (1950), p. 354.
- ^ Goody, R. M., Yung, Y. L. (1989), pp. 33–35.
- ^ Loudon, R. (1973/2000), pp. 16–19.
- ^ Robert W. Boyd, Radiometry and the Detection of Optical Radiation, John Wiley and Sons, 1983
- ^ Hubeny, Ivan; Mihalas, Dimitri (2015). Theory of stellar atmospheres : an introduction to astrophysical non-equilibrium quantitative spectroscopic analysis. Princeton University Press. pp. 116–118. ISBN 9780691163291.
- ^ Zettili, Nouredine (2009). Quantum mechanics: concepts and applications (2nd ed.). Chichester: Wiley. pp. 594–596. ISBN 978-0-470-02679-3.
- ^ a b c d Segre, Carlo. "The Einstein coefficients - Fundamentals of Quantum Theory II (PHYS 406)" (PDF). p. 32.
- ^ Zwiebach, Barton. "Quantum Physics III Chapter 4: Time Dependent Perturbation Theory | Quantum Physics III | Physics". MIT OpenCourseWare. pp. 108–110. Retrieved 2023-11-03.
Cited bibliography
[edit]- Chandrasekhar, S. (1950). Radiative Transfer, Oxford University Press, Oxford.
- Garrison, J. C., Chiao, R. Y. (2008). Quantum Optics, Oxford University Press, Oxford UK, ISBN 978-019-850-886-1.
- Goody, R. M., Yung, Y. L. (1989). Atmospheric Radiation: Theoretical Basis, 2nd edition, Oxford University Press, Oxford, New York, 1989, ISBN 0-19-505134-3.
- Heisenberg, W. (1925). "Über quantentheoretische Umdeutung kinematischer und mechanischer Beziehungen". Zeitschrift für Physik. 33 (1): 879–893. Bibcode:1925ZPhy...33..879H. doi:10.1007/BF01328377. S2CID 186238950. Translated as "Quantum-theoretical Re-interpretation of kinematic and mechanical relations" in
van der Waerden, B. L. (1967). Sources of Quantum Mechanics. North-Holland Publishing. pp. 261–276.
- Herzberg, G. (1950). Molecular Spectroscopy and Molecular Structure, vol. 1, Diatomic Molecules, second edition, Van Nostrand, New York.
- Loudon, R. (1973/2000). The Quantum Theory of Light, (first edition 1973), third edition 2000, Oxford University Press, Oxford UK, ISBN 0-19-850177-3.
- Mihalas, D., Weibel-Mihalas, B. (1984). Foundations of Radiation Hydrodynamics, Oxford University Press, New York ISBN 0-19-503437-6.
- Yariv, A. (1967/1989). Quantum Electronics, third edition, John Wiley & sons, New York, ISBN 0-471-60997-8.
- Hubeny, Ivan; Mihalas, Dimitri (2015). Theory of stellar atmospheres : an introduction to astrophysical non-equilibrium quantitative spectroscopic analysis. Princeton University Press. ISBN 9780691163291.
Other reading
[edit]- Condon, E. U.; Shortley, G. H. (1964). The Theory of Atomic Spectra. Cambridge University Press. ISBN 0-521-09209-4.
{{cite book}}: ISBN / Date incompatibility (help) - Rybicki, G. B.; Lightman, A. P. (1985). Radiative processes in Astrophysics. John Wiley & Sons, New York. ISBN 0-471-82759-2.
- Shu, F. H. (1991). The Physics of Astrophysics. Vol. 1: Radiation. University Science Books, Mill Valley, CA. ISBN 0-935702-64-4.
- Robert C. Hilborn (2002). "Einstein coefficients, cross sections, f values, dipole moments, and all that". Am. J. Phys. 50: 982–986. arXiv:physics/0202029. Bibcode:2002physics...2029H.
- Taylor, M. A.; Vilchez, J. M. (2009). "Tutorial: Exact solutions for the populations of the n-level ion". Publications of the Astronomical Society of the Pacific. 121 (885): 1257–1266. arXiv:0709.3473. Bibcode:2009PASP..121.1257T. doi:10.1086/648121. S2CID 16116964.
External links
[edit]Einstein coefficients
View on GrokipediaBackground on Atomic Transitions
Spectral Lines
Spectral lines are discrete wavelengths of light emitted or absorbed by atoms when electrons transition between quantized energy levels. These lines arise from the specific energy differences between atomic orbitals, producing sharp features in otherwise continuous spectra.[6] In the early 19th century, Joseph von Fraunhofer observed hundreds of dark absorption lines in the spectrum of sunlight, mapping their positions with high precision using improved prisms. These features, now known as Fraunhofer lines, were initially enigmatic but marked the beginning of systematic spectral analysis. Later, in 1859, Gustav Kirchhoff provided the key insight by demonstrating that these dark lines correspond to absorption by chemical elements in the Sun's cooler outer atmosphere, matching the bright emission lines produced when the same elements are heated in laboratory flames. This work established the atomic origin of spectral lines and laid the foundation for spectroscopy as a tool for elemental identification.[7][8] The underlying quantum model explains spectral lines through the relation between energy levels and photon frequencies. The energy difference between two atomic levels determines the frequency of the emitted or absorbed radiation via where is Planck's constant. This equation, rooted in the quantization of energy, predicts the precise wavelengths of lines for each transition in an atom.[9] Spectral lines manifest in two primary forms depending on the physical conditions. Emission lines appear as bright features against a dark background in the spectra of hot, low-density gases where excited atoms radiate photons directly. In contrast, absorption lines show as dark gaps in a continuous spectrum when light from a hot source passes through cooler, intervening gas that selectively absorbs photons at matching wavelengths. These distinctions follow from Kirchhoff's laws of spectroscopy, which describe the conditions for continuous, emission, and absorption spectra.[8] In spectroscopy, spectral lines act as unique signatures of atomic structure, enabling the identification of elements in distant stars, nebulae, and laboratory samples without direct contact. The wavelengths and relative strengths of lines reveal details about electron configurations and energy level spacings, providing insights into atomic composition and environmental conditions. The intensities of these lines are governed by the rates of atomic transitions quantified by Einstein coefficients.[10][11]Emission and Absorption Processes
In atomic physics, the interaction between matter and electromagnetic radiation occurs through three primary processes: absorption, spontaneous emission, and stimulated emission. These mechanisms describe how atoms transition between discrete energy levels, exchanging energy with photons of frequency , and form the basis for understanding radiative transitions that produce spectral lines.[12] Absorption takes place when an atom in a lower energy state encounters a photon with energy matching the difference between two energy levels, leading to excitation to the higher state. This process is probabilistic, with the transition rate increasing with the radiation intensity at the resonant frequency, reflecting the atom's inherent susceptibility to the electromagnetic field.[13] Spontaneous emission involves an excited atom decaying randomly to a lower energy state, releasing a photon of energy in the process. Unlike absorption, this decay occurs without external prompting, driven solely by the instability of the excited state; the emitted photon's direction, phase, and polarization are random, resulting in incoherent light. The probability of spontaneous emission is characterized by a fixed transition rate for a given atomic system, independent of surrounding radiation.[12][14] Stimulated emission arises when an incoming photon of energy interacts with an atom in an excited state, prompting the atom to drop to the lower energy level while emitting a second photon identical to the first in frequency, phase, and propagation direction. This induced process amplifies the incident radiation coherently, as the two photons emerge in lockstep, contrasting with the randomness of spontaneous emission. The likelihood of stimulated emission mirrors that of absorption but applies to de-excitation, scaling with the photon density.[12][13] Classically, descriptions of radiation-matter interactions, such as those in the Rayleigh-Jeans law for blackbody spectra, treated energy as continuously distributed and waves as classical fields, leading to the ultraviolet catastrophe where predicted energy diverges to infinity at short wavelengths, contradicting observations. This failure highlighted the need for a quantum framework, where energy is quantized in discrete photon units, as pioneered by Planck and extended by Einstein to encompass discrete atomic transitions and photon-based absorption and emission.[15][14]Formal Definition of Einstein Coefficients
Spontaneous Emission Coefficient
The spontaneous emission coefficient, denoted as , was introduced by Albert Einstein in 1917 as part of his foundational work on the quantum theory of radiation, where he analyzed the statistical equilibrium between matter and radiation to derive Planck's law.[16] In this context, characterizes the probability of a molecule or atom transitioning from an upper energy state 2 to a lower state 1 by emitting a photon without external stimulation from the radiation field.[17] Formally, is defined as the transition probability per unit time for spontaneous emission from the upper level 2 to the lower level 1.[18] Its units are s (inverse seconds), reflecting its role as a rate constant.[17] Physically, determines the natural lifetime of the excited state, given by , which represents the average time an atom remains in the upper state before decaying via spontaneous emission, assuming no other decay channels.[18] This lifetime is crucial for understanding the duration of excited states in isolated atoms or dilute gases. In non-equilibrium conditions, such as in astrophysical plasmas or laboratory discharges, governs the contribution of spontaneous emission to the overall intensity of spectral lines, where the emission rate is proportional to times the population of the upper level.[17] This process complements stimulated emission but dominates in low-radiation-density environments.Stimulated Emission and Absorption Coefficients
The Einstein coefficients and quantify the rates of stimulated emission and absorption, respectively, for a two-level atomic system interacting with a radiation field. Introduced by Albert Einstein in his 1917 paper on the quantum theory of radiation, these coefficients represent the transition probability per unit time per unit spectral energy density for an atom in the upper state (level 2) to emit a photon or in the lower state (level 1) to absorb one, driven by the incident radiation.[16] The stimulated emission rate, expressed as the number of transitions per unit time per unit volume, is , where is the population density of atoms in the upper level, and is the energy density of the radiation per unit frequency interval at frequency . Analogously, the absorption rate is , with the population density in the lower level. These rates vanish in the absence of radiation, distinguishing stimulated processes from spontaneous emission, which occurs independently of the external field.[16] In systems without level degeneracy, , reflecting the symmetry between absorption and stimulated emission processes. For degenerate levels, the relation generalizes to , where and are the degeneracies of the lower and upper levels.[16] The coefficients are typically defined using frequency , as in Einstein's original formulation, with SI units of when has units of ; in cgs units, they are . Equivalent cgs formulations exist for historical atomic physics contexts. In some modern treatments, particularly in quantum optics, angular frequency is employed, requiring to preserve the invariance of the product under the transformation .[19][20]Thermodynamic Relations
Principle of Detailed Balancing
The principle of detailed balancing states that, in thermal equilibrium, the net rate of transitions between any two energy levels of an atomic system is zero, implying that the rate of upward transitions (absorption) precisely equals the rate of downward transitions (total emission). This condition ensures no net change in the population of the levels over time, reflecting the microscopic reversibility of the processes under thermodynamic equilibrium.[16] For a two-level atomic system, with level 1 as the lower energy state and level 2 as the upper, the principle manifests in the equality of transition rates involving the Einstein coefficients. The absorption rate from level 1 to 2 is given by , where is the population of level 1, is the absorption coefficient, and is the spectral energy density of the radiation field at frequency . The total emission rate from level 2 to 1 comprises spontaneous emission and stimulated emission , where and are the population and spontaneous emission coefficient for level 2, respectively. Thus, detailed balancing requires: [21][16] In thermal equilibrium, the populations and follow the Boltzmann distribution, accounting for the degeneracies and of the levels: [16][21] where is Planck's constant, is the Boltzmann constant, and is the temperature. Albert Einstein introduced this principle in his 1917 analysis to reconcile classical radiation theory with quantum hypotheses, demonstrating that equilibrium demands both spontaneous and stimulated emission processes; this argument provided key evidence for the quantization of electromagnetic radiation by linking atomic transitions to a discrete energy exchange of .[16] While the principle of detailed balancing generalizes to any reversible microscopic process in equilibrium—such as chemical reactions or particle collisions—its application here is confined to radiative transitions in atomic systems, where it constrains the interplay between matter and radiation. This condition establishes foundational relations among the Einstein coefficients without presupposing the form of the equilibrium radiation spectrum.[21][16]Equilibrium Conditions
In thermal equilibrium, the principle of detailed balancing ensures that the rates of upward and downward transitions between two energy levels are equal, leading to specific relations among the Einstein coefficients.[16] Consider two levels: the lower level 1 with energy and degeneracy , and the upper level 2 with energy and degeneracy . The population of the levels follows Maxwell-Boltzmann statistics, so , where is Boltzmann's constant and is the temperature.[16] Under isotropic radiation, the equilibrium condition balances absorption and emission rates: , where is the spectral energy density at frequency .[16] In the limit of high temperature or large , spontaneous emission becomes negligible compared to stimulated processes, yielding . Substituting the Boltzmann population ratio gives , or equivalently, .[16] This adjustment accounts for degeneracy effects, ensuring the coefficients reflect the statistical weights of the levels when . For the full equilibrium including spontaneous emission, rearranging the balance equation produces .[16] To connect this to blackbody radiation, the form of matches Planck's law only if , where is the speed of light; this relation is derived by imposing consistency with the known spectral energy density of thermal radiation.[16] The assumptions of isotropic radiation and Maxwell-Boltzmann population statistics underpin these derivations, treating the radiation field as uniform and the atomic ensembles as classical in their thermal distribution.[16] This framework verifies consistency with classical limits at low frequencies, where . The exponential approximates to , so . Substituting the relation yields , recovering the Rayleigh-Jeans law for the ultraviolet catastrophe regime.[16]Related Physical Quantities
Oscillator Strengths
The oscillator strength , for a transition from a lower energy level 1 to an upper level 2, is a dimensionless parameter that quantifies the intensity or probability of an atomic or molecular transition in the context of electromagnetic radiation absorption or emission. It originates from the classical model of a damped electron oscillator, where the electron is bound harmonically and driven by an oscillating electric field at the transition frequency . In this analogy, represents the effective number of classical electrons contributing to the radiation at that frequency, providing a bridge between classical radiation theory and quantum mechanical transition probabilities. Oscillator strengths typically range from to 1 for allowed transitions, with values near unity indicating strong lines comparable to classical dipole radiation.[17] The oscillator strength is directly related to the Einstein coefficient for stimulated absorption through the equation where is the electron mass, the elementary charge, the vacuum permittivity, Planck's constant, the transition frequency, and , the statistical weights (degeneracies) of the lower and upper levels, respectively; this relation holds in SI units. This connection allows oscillator strengths to be computed from known values or vice versa, facilitating the use of empirical data in quantum calculations. The formula underscores how scales the quantum transition rate to match the classical absorption cross-section for a single electron.[17] A key theoretical constraint on oscillator strengths is the Thomas-Reiche-Kuhn (TRK) sum rule, which states that for a given initial state (often the ground state), the sum of absorption oscillator strengths over all possible final states equals the number of non-relativistic electrons available for excitation: . This rule, derived from the commutator of the dipole operator with the Hamiltonian, ensures conservation of the total transition strength and serves as a benchmark for the accuracy of computed or measured values across an atom's spectrum; for example, in hydrogen (), the sum is exactly 1. Violations or modifications occur in relativistic or multi-electron systems but remain approximately valid. Experimentally, oscillator strengths are determined from the relative intensities of spectral lines in absorption or emission spectra under controlled conditions, such as in optically thin plasmas or beams, where line strength is proportional to (with the degeneracy factor). Alternatively, they can be inferred from radiative lifetimes of excited states, since and relates to via the Einstein relations and the above formula for . These methods are essential in astrophysics for interpreting stellar spectra and abundance determinations, as well as in plasma diagnostics to infer ion densities and temperatures from observed line ratios. For instance, precise -values for iron lines enable modeling of solar photospheric conditions.[22]Dipole Approximation
The electric dipole approximation provides a quantum mechanical framework for computing the Einstein coefficients from transition matrix elements, applicable when the wavelength of the emitted or absorbed radiation is much longer than the spatial extent of the atomic or molecular system, typically on the order of 0.1 nm for atoms compared to visible light wavelengths of 400–700 nm.[23] In this regime, the interaction between the electromagnetic field and the system is dominated by the electric dipole (E1) term in the multipole expansion of the Hamiltonian, as higher-order terms like magnetic dipole or electric quadrupole contributions are suppressed by factors of (atomic size / wavelength).[17] This approximation simplifies the perturbation to , where is the electric dipole operator for electrons and is the electric field of the radiation.[23] The coefficients are derived using time-dependent perturbation theory, where the transition probability per unit time follows Fermi's golden rule:with the density of final states accounted for in the continuum of photon modes.[23] For spontaneous emission, summing over photon polarizations and directions yields the Einstein A coefficient for a transition from upper state |2⟩ to lower state |1⟩ (assuming non-degenerate levels for simplicity):
where is the transition angular frequency and is the dipole matrix element (in SI units, with often averaged over orientations).[17] For stimulated emission and absorption, the rate depends on the radiation energy density , leading to the B coefficient:
Degeneracies are incorporated via , where is the degeneracy of level , and may include sums over magnetic sublevels.[17] This approach highlights the E1 transitions as the primary mechanism for allowed lines in spectra, with selection rules and arising from the vector nature of the dipole operator.[23] However, the approximation fails for forbidden transitions where due to parity or angular momentum conservation, requiring inclusion of weaker M1 or E2 terms that are smaller by factors of to .[23] The dipole matrix element also connects to the classical oscillator strength , bridging quantum and semiclassical descriptions.[17]