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Τι (ποιος) είναι radiation$66417$ - ορισμός
USED TO SOLVE THE HELMHOLTZ EQUATION
Sommerfield radiation condition; Radiation condition; Radiation conditions
Synchrotron radiation
.svg?width=200 "Synchrotron radiation from an undulator")
ELECTROMAGNETIC RADIATION EMITTED WHEN CHARGED PARTICLES ARE ACCELERATED RADIALLY
Synchrotron Radiation; Synchrotron emission; Synchotron radiation; Synchrotron light; Curvature radiation; Magnetobremsstrahlung; Gyro radiation
Synchrotron radiation (also known as magnetobremsstrahlung radiation) is the electromagnetic radiation emitted when relativistic charged particles are subject to an acceleration perpendicular to their velocity (). It is produced artificially in some types of particle accelerators, or naturally by fast electrons moving through magnetic fields.
synchrotron radiation
ELECTROMAGNETIC RADIATION EMITTED WHEN CHARGED PARTICLES ARE ACCELERATED RADIALLY
Synchrotron Radiation; Synchrotron emission; Synchotron radiation; Synchrotron light; Curvature radiation; Magnetobremsstrahlung; Gyro radiation
¦ noun Physics polarized radiation emitted by a charged particle spinning in a magnetic field.
Background radiation
![gamma radiation]] level is 9.8 [[μR/h]] (0.82 mSv/a) This is very close to the world average background radiation of 0.87 mSv/a from cosmic and terrestrial sources.](https://commons.wikimedia.org/wiki/Special:FilePath/Atomic Testing Museum weather display cropped.jpg?width=200 "gamma radiation]] level is 9.8 [[μR/h]] (0.82 mSv/a) This is very close to the world average background radiation of 0.87 mSv/a from cosmic and terrestrial sources.")
LEVEL OF IONIZING RADIATION PRESENT IN THE NATURAL ENVIRONMENT
Background Radiation; Natural radioactivity; Terrestrial radiation; Natural radiation; Background count; Natural background radiation; Environmental radiation; Radiation background; Ambient radiation
Background radiation is a measure of the level of ionizing radiation present in the environment at a particular location which is not due to deliberate introduction of radiation sources.
Βικιπαίδεια
Sommerfeld radiation condition
In applied mathematics, the Sommerfeld radiation condition is a concept from theory of differential equations and scattering theory used for choosing a particular solution to the Helmholtz equation. It was introduced by Arnold Sommerfeld in 1912 and is closely related to the limiting absorption principle (1905) and the limiting amplitude principle (1948).
