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Radiation length
View on WikipediaIn particle physics, the radiation length is a characteristic of a material, related to the energy loss of high energy particles electromagnetically interacting with it. It is defined as the mean length (in cm) into the material at which the energy of an electron is reduced by the factor 1/e.[1]
Definition
[edit]In materials of high atomic number (e.g. tungsten, uranium, plutonium) the electrons of energies >~10 MeV predominantly lose energy by bremsstrahlung, and high-energy photons by e+e− pair production. The characteristic amount of matter traversed for these related interactions is called the radiation length X0, usually measured in g·cm−2. It is both the mean distance over which a high-energy electron loses all but 1⁄e of its energy by bremsstrahlung,[1] and 7⁄9 of the mean free path for pair production by a high-energy photon. It is also the appropriate length scale for describing high-energy electromagnetic cascades.
The radiation length for a given material consisting of a single type of nucleus can be approximated by the following expression:[2]
where Z is the atomic number and A is mass number of the nucleus.
For Z > 4, a good approximation is[3][inconsistent].
where
- na is the number density of the nucleus,
- denotes the reduced Planck constant,
- me is the electron rest mass,
- c is the speed of light,
- α is the fine-structure constant.
For electrons at lower energies (below few tens of MeV), the energy loss by ionization is predominant.
While this definition may also be used for other electromagnetic interacting particles beyond leptons and photons, the presence of the stronger hadronic and nuclear interaction makes it a far less interesting characterisation of the material; the nuclear collision length and nuclear interaction length are more relevant.
Comprehensive tables for radiation lengths and other properties of materials are available from the Particle Data Group.[2][4]
See also
[edit]References
[edit]- ^ a b M. Gupta; et al. (2010). "Calculation of radiation length in materials". PH-EP-Tech-Note. 592 (1–4): 1. arXiv:astro-ph/0406663. Bibcode:2004PhLB..592....1P. doi:10.1016/j.physletb.2004.06.001.
- ^ a b S. Eidelman; et al. (2004). "Review of particle physics". Phys. Lett. B. 592 (1–4): 1–5. arXiv:astro-ph/0406663. Bibcode:2004PhLB..592....1P. doi:10.1016/j.physletb.2004.06.001. (http://pdg.lbl.gov/)
- ^ De Angelis, Alessandro; Pimenta, Mário (2018). Introduction to Particle and Astroparticle Physics (2 ed.). Springer. Bibcode:2018ipap.book.....D. doi:10.1007/978-3-319-78181-5. ISBN 978-3-319-78180-8.
- ^ "AtomicNuclearProperties on the Particle Data Group". Archived from the original on 2021-07-24. Retrieved 2008-01-26.
Radiation length
View on Grokipediawhere is the fine-structure constant, is the classical electron radius, is Avogadro's number, is the atomic mass, is the atomic number, and , , and are tabulated radiative stopping power functions accounting for screening effects.[1] For compounds or mixtures, the effective radiation length follows the weighted harmonic mean: , with as the weight fraction of component .[1] In practical applications, radiation length plays a critical role in the design of particle detectors, particularly electromagnetic calorimeters, where the depth required to contain and measure energy deposits from showers is typically 20–30 thick to achieve high efficiency.[1] For instance, materials like lead tungstate (PbWO₄) are selected for their short (approximately 0.89 cm), enabling compact detectors in experiments such as CMS at the LHC.[2] Values of for common materials vary widely—ranging from about 42.7 g/cm² for carbon to 6.37 g/cm² for lead—reflecting differences in atomic number and density that influence radiation processes.[1][3][4]
Fundamentals
Definition
The radiation length is defined as the mean distance over which a high-energy electron loses all but of its energy by bremsstrahlung in a given material.[5] This characteristic length quantifies the scale at which electromagnetic cascades develop, as high-energy photons lose energy primarily through pair production over a similar distance.[5] The concept was introduced in the mid-20th century by Bruno Rossi and Kenneth Greisen in their seminal review on cosmic-ray theory, amid efforts to model the extensive air showers generated by high-energy cosmic rays interacting with the atmosphere.[6] Radiation length is typically expressed in units of mass thickness, g/cm², which allows direct comparison across materials independent of density; for a specific material, the physical distance in cm is obtained by dividing by the material's density.[5] For relativistic electrons with energies above a few MeV, bremsstrahlung—electromagnetic radiation emitted during deflection by atomic nuclei—dominates energy loss over ionization, leading to the exponential attenuation described by .[5]Physical Basis
Bremsstrahlung, or braking radiation, occurs when a charged particle, such as an electron, is decelerated by the Coulomb field of an atomic nucleus in a material, resulting in the emission of a photon whose energy is drawn from the particle's kinetic energy.[5] This process is the primary mechanism for radiative energy loss in high-energy charged particles interacting with matter.[5] In the relativistic regime, where the electron energy (with ), bremsstrahlung losses dominate over collisional ionization losses, leading to a rapid degradation of the electron's energy through successive photon emissions.[5] The transition between these regimes is marked by the critical energy , defined as the electron energy at which the bremsstrahlung and ionization energy losses per radiation length are equal; approximately, for solids and liquids, and for gases, in a material of atomic number .[5] Atomic screening effects, arising from the cloud of orbital electrons around the nucleus, modify the effective Coulomb potential and thus alter the bremsstrahlung spectrum, particularly at low photon energies where the process is more sensitive to the screened nuclear field.[5] These effects reduce the cross section for soft photon emission compared to an unscreened point-charge model. The quantum mechanical foundation for bremsstrahlung cross sections in this context is provided by the Bethe-Heitler formula, which calculates the differential cross section for photon emission by relativistic electrons scattering off atomic nuclei, incorporating first-order quantum electrodynamics and accounting for screening in the high-energy limit.Theoretical Formulation
Derivation of the Formula
The radiation length characterizes the mean distance over which a high-energy electron loses all but a fraction of its energy through bremsstrahlung radiation, leading to the approximate differential energy loss in the relativistic regime.[1] This relation arises from the fact that the bremsstrahlung spectrum at high energies results in a constant fractional energy loss per unit path length, solving the differential equation to yield the exponential attenuation .[7] The derivation assumes the relativistic limit where the electron energy , complete screening of the nuclear Coulomb field by atomic electrons, and neglect of multiple scattering effects in the basic formulation.[8] To obtain from first principles, the total radiated energy per unit path length is computed by integrating the Bethe-Heitler differential cross-section for bremsstrahlung over the photon energy spectrum. The Bethe-Heitler cross-section gives the probability for an electron to emit a photon of energy (with ) while scattering off a nucleus, approximated in the high-energy limit with complete screening as , where is the fine-structure constant, is the classical electron radius, is the atomic number, for accounts for the screening parameter in the Coulomb logarithm, and is a small correction for finite nuclear size and distant collisions given by .[8] [7] [5] The energy loss is then , where is the number density of atoms ( is Avogadro's number, is density, and is atomic mass). In the approximation where the cross-section scales as and the logarithmic terms are nearly constant for , the integral simplifies to , yielding .[1] Comparing to , the radiation length follows as . Expressing in units of g/cm² (independent of density) gives the standard form , where the numerical prefactor arises from evaluating with CODATA values.[1] [8] This derivation neglects the Landau-Pomeranchuk-Migdal (LPM) effect, which suppresses bremsstrahlung at ultra-high energies ( in typical materials) due to quantum interference in multiple scattering, representing a limitation of the formula for extreme conditions.[1] A more complete expression includes an additional term (with ) accounting for electron-electron scattering contributions, but it is subdominant for .[8]Key Parameters and Approximations
The radiation length scales with the square of the atomic number primarily due to the enhanced strength of the nuclear Coulomb field, which increases the probability of bremsstrahlung emission by electrons interacting with the atomic nucleus.[1] This dependence arises in the leading term of the theoretical formula for , reflecting the cross-section for bremsstrahlung proportional to the square of the nuclear charge.[1] A key parameter in the formula is the radiative logarithmic term for , which accounts for the screening of the nuclear field by orbital electrons, modifying the logarithmic term in the bremsstrahlung spectrum integration; the correction is subtracted from for accuracy across elements and is given by , with and the fine-structure constant.[1] [5] The density effect is incorporated by defining as a mass thickness in g/cm², independent of material density; the corresponding physical length is then , where is the material's density in g/cm³, allowing direct comparison of penetration depths across substances.[1] At low energies, modifications to the formula are necessary due to incomplete screening for soft photons (low fractional energy ), where the high-energy Bethe-Heitler approximation breaks down and the spectrum requires adjustments for atomic binding effects.[1] Practical calculations often introduce adjustments for ultra-soft photons to mitigate infrared divergences and transition to regimes where ionization losses dominate over radiation.[1] At high energies, the Landau-Pomeranchuk-Migdal (LPM) effect suppresses bremsstrahlung through interference from multiple scattering within the photon formation length, effectively increasing by a factor scaling up to for electron energies TeV.[1] This suppression is parameterized approximately by the characteristic energy for onset .[1] The standard formula for , including these parameters and corrections, is accurate for electron energies in the range 10 MeV < E < 1 TeV, with deviations at lower energies from screening incompleteness and at higher energies from LPM suppression.[1]Material Properties
Calculation for Composite Materials
The radiation length for composite materials, including mixtures and compounds, is computed using the mixture rule, which approximates the effective radiation length by considering the weighted contributions from each constituent. Specifically, for a material composed of components with weight fractions and individual radiation lengths , the reciprocal of the effective radiation length is given by This formula, recommended by the Particle Data Group (PDG), provides a practical approximation for homogeneous mixtures where the constituents are well-intermixed on the scale of particle interactions. For chemical compounds, the mixture rule is applied using the atomic composition to determine the weight fractions of each element. The radiation length of each element is taken from tabulated values derived from the theoretical formula adjusted for atomic number and mass number . For example, in water (), the weight fraction of hydrogen is and of oxygen is . Using g/cm² and g/cm² yields so g/cm², consistent with the PDG tabulated value of 36.08 g/cm² for liquid water. This approach accounts for the electron density and -dependence inherent in the elemental radiation lengths.[9][10][11] In layered structures, such as those in particle detector sandwiches with alternating materials, the effective radiation length is determined by path-length averaging along the particle trajectory. The total areal mass density (in g/cm², where is the mass thickness of the -th layer) relates to the effective via which again follows from the mixture rule since the weight fractions are . This method is commonly used for estimating material budgets in multilayer detectors, where the particle traverses discrete layers sequentially.[12] The radiation length scales inversely with the electron density , as bremsstrahlung and pair production probabilities depend primarily on the number of electrons per unit mass, with adjustments for variations in that affect screening and logarithmic terms in the cross-sections. In composites, differences in across components introduce small deviations from pure scaling, but the mixture rule incorporates these through the elemental . For practical computations, the PDG provides recipes that ensure accuracy to within a few percent, including considerations for finite size effects in thin layers where boundary corrections or incomplete screening may alter the effective interaction probability compared to bulk materials.Tabulated Values and Examples
The radiation length for various materials is typically expressed in units of g/cm² to account for density-independent properties, but can also be converted to physical length in cm by dividing by the material's density . These values demonstrate the Z-dependence for elements, where higher atomic numbers lead to shorter due to increased electromagnetic interaction probabilities.[13] Representative values for selected elements are tabulated below, compiled from experimental and calculated data.[13]| Material | (g/cm²) | (g/cm³) | (cm) |
|---|---|---|---|
| Air (dry, 1 atm) | 36.62 | 0.001205 | 30400 |
| Aluminum (Al) | 24.01 | 2.699 | 8.89 |
| Silicon (Si) | 21.82 | 2.329 | 9.37 |
| Lead (Pb) | 6.37 | 11.35 | 0.56 |
