The elemental makeup and energy-dependent behavior of cosmic rays, including anomalies in heavy nuclei.Cosmic ray composition refers to the relative abundance of different atomic nuclei and particles that make up cosmic rays—high-energy particles from space that constantly bombard Earth. These particles are primarily protons (hydrogen nuclei) and alpha particles (helium nuclei), but also include heavier nuclei up to iron and beyond, as well as electrons and positrons. The composition is not uniform; it varies with energy and can reveal the sources and acceleration mechanisms of these particles.
The discovery of cosmic rays is credited to Victor Hess in 1912, who found radiation increasing with altitude. The detailed study of their composition began in the mid-20th century with the advent of particle detectors on high-altitude balloons and later in space.
Cosmic rays are detected indirectly by the showers of secondary particles they produce when they hit Earth's atmosphere, or directly by detectors on satellites and balloons. By measuring the charge and mass of individual particles, scientists can determine the elemental composition. Anomalies, such as the overabundance of certain odd-Z nuclei (like nitrogen, fluorine, or sodium) at specific energies, provide clues about the nucleosynthesis processes in their sources, such as supernovae or pulsars.
Understanding cosmic ray composition is crucial for interpreting data from particle physics experiments, for assessing radiation risks for astronauts and electronics in space, and for studying the interstellar medium and stellar evolution.
The abundance of some heavy nuclei in cosmic rays, like titanium, is much higher than in the solar system, suggesting they come from freshly synthesized material in recent supernova remnants, as discussed in the article 'Титан в космических лучах'.
| r | variable | radial coordinate (distance from center) — radius metre |
| M(r) | variable | enclosed mass within radius r — mass kilogram |
| k | variable | constant of motion (related to energy per unit mass) — specific energy metre squared per second squared |
| G | constant | Newtonian constant of gravitation, fundamental strength of gravity — gravitational constant = 6.67430e-11 cubic metre per kilogram per second squared |
| ˙ | operator | derivative with respect to time — time derivative |
| [X/Y] | variable | logarithmic abundance ratio relative to solar — abundance ratio |
| n_X | variable | number density of element X — number density per cubic metre |
| n_Y | variable | number density of element Y — number density per cubic metre |
| (n_X/n_Y)_⊙ | variable | solar ratio of number densities — number density ratio |
| log10 | operator | base-10 logarithm — logarithm base 10 |




