Properties of Heavy Cosmic Nuclei Phosphorus, Chlorine, Argon, Potassium, and Calcium: Results from the Alpha Magnetic Spectrometer

Phys. Rev. Lett. 136, 241002 (2026)
Published on:
Abstract

We report the unique properties of cosmic phosphorus (P), chlorine (Cl), argon (Ar), potassium (K), and calcium (Ca) fluxes in the GV to TV rigidity range collected by the Alpha Magnetic Spectrometer (AMS) on the International Space Station. With a total of one million events collected over 13.5 years, we observed that the rigidity dependencies of the five fluxes are well described by the sums of a primary cosmic ray component and a secondary cosmic ray component. The abundance ratios of all five elements to Si at the source are accurately determined independent of cosmic ray propagation. The source abundance of Ar and Ca (even-𝑍 elements) is larger than P, Cl, and K (odd-𝑍 elements). The secondary components of the P and the Cl fluxes are each ∼1/3 of the F flux, and the secondary components of the Ar, K, and Ca fluxes are each ∼1/2 of the F flux. The twenty elements measured by AMS, from He to Ca and Fe, can be categorized into four classes, two primary and two secondary, based on their rigidity dependence.

Supplemental Material
Download AMS Data

The P flux $\Phi_\mathrm{P}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The Cl flux $\Phi_\mathrm{Cl}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The Ar flux $\Phi_\mathrm{Ar}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error. 

The K flux $\Phi_\mathrm{K}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The Ca flux $\Phi_\mathrm{Ca}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The Si flux $\Phi_\mathrm{Si}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The F flux $\Phi_\mathrm{F}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The S flux $\Phi_\mathrm{S}$ as a function of rigidity at the top of AMS in units of $\mathrm{[m^2\cdot sr \cdot s \cdot GV]^{-1}}$ including errors due to statistics (stat.); contributions to the systematic error from the trigger, background, and acceptance (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The contributions of individual sources to the systematic error are added in quadrature to arrive at the total systematic error.

The phosphorus to sulfur flux ratio $\Phi_\mathrm{P}/\Phi_\mathrm{S}$ as a function of rigidity including errors due to statistics (stat.); contributions to the systematic error from the trigger, acceptance, and background  (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.).  The statistical errors are the sum in quadrature of the ratios of phosphorus and sulfur flux statistical errors  to the corresponding flux values,  multiplied by $\Phi_\mathrm{P}/\Phi_\mathrm{S}$.  The systematic errors from the background subtraction, the trigger, and the event reconstruction and selection are likewise added in quadrature.  The correlations in the systematic errors from the uncertainty in nuclear interaction cross sections, the unfolding and the absolute rigidity scale between the phosphorus and sulfur fluxes have been taken into account in calculating the corresponding systematic errors of $\Phi_\mathrm{P}/\Phi_\mathrm{S}$.  The contribution of individual sources to the systematic error are added in quadrature to arrive at the total systematic uncertainty.

The chlorine to argon flux ratio $\Phi_\mathrm{Cl}/\Phi_\mathrm{Ar}$ as a function of rigidity including errors due to statistics (stat.); contributions to the systematic error from the trigger, acceptance, and background  (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The statistical errors are the sum in quadrature of the ratios of chlorine and argon flux statistical errors to the corresponding flux values, multiplied by $\Phi_\mathrm{Cl}/\Phi_\mathrm{Ar}$.  The systematic errors from the background subtraction, the trigger, and the event reconstruction and selection are likewise added in quadrature.  The correlations in the systematic errors from the uncertainty in nuclear interaction cross sections, the unfolding and the absolute rigidity scale between the chlorine and argon fluxes have been taken into account in calculating the corresponding systematic errors of $\Phi_\mathrm{Cl}/\Phi_\mathrm{Ar}$.  The contribution of individual sources to the systematic error are added in quadrature to arrive at the total systematic uncertainty.

The potassium to calcium flux ratio $\Phi_\mathrm{K}/\Phi_\mathrm{Ca}$ as a function of rigidity including errors due to statistics (stat.); contributions to the systematic error from the trigger, acceptance, and background (acc.); the rigidity resolution function and unfolding (unf.); the absolute rigidity scale (scale); and the total systematic error (syst.). The statistical errors are the sum in quadrature of the ratios of potassium and calcium flux statistical errors to the corresponding flux values, multiplied by $\Phi_\mathrm{K}/\Phi_\mathrm{Ca}$.  The systematic errors from the background subtraction, the trigger, and the event reconstruction and selection are likewise added in quadrature.  The correlations in the systematic errors from the uncertainty in nuclear interaction cross sections, the unfolding and the absolute rigidity scale between the potassium and calcium fluxes have been taken into account in calculating the corresponding systematic errors of $\Phi_\mathrm{K}/\Phi_\mathrm{Ca}$.  The contribution of individual sources to the systematic error are added in quadrature to arrive at the total systematic uncertainty.

External Databases
AMS Data at CRDB (Cosmic-ray DataBase)

The CRDB at LPSC/IN2P3/CNRS, online since 2013, is fully described in Maurin et al. (2014, 2020)

AMS Data at Cosmic Ray DataBase (CRDB) © SSDC

The CRDB © SSDC is developed at the Space Science Data Center, a facility of the Italian Space Agency (ASI).