PAMELA Measurements of Cosmic-Ray Proton and Helium Spectra
Abstract
Protons and helium nuclei are the most abundant components of the cosmic radiation. Precise measurements of their fluxes are needed to understand the acceleration and subsequent propagation of cosmic rays in our Galaxy. We report precision measurements of the proton and helium spectra in the rigidity range 1 gigavolt to 1.2 teravolts performed by the satellite-borne experiment PAMELA (payload for antimatter matter exploration and light-nuclei astrophysics). We find that the spectral shapes of these two species are different and cannot be described well by a single power law. These data challenge the current paradigm of cosmic-ray acceleration in supernova remnants followed by diffusive propagation in the Galaxy. More complex processes of acceleration and propagation of cosmic rays are required to explain the spectral structures observed in our data.
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References and Notes
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PAMELA comprises a number of high-performance detectors, capable of identifying particles through the determination of charge (Z), rigidity (R = pc/|Z|e, where p is the momentum of a particle of charge Ze, c is the speed of light, and e is the electron charge), and velocity (β = v/c, where v is the velocity) over a wide energy range. The device is built around a permanent magnet with a six-plane double-sided silicon microstrip tracker, providing absolute charge information and track-deflection (η = ±1/R, with the sign depending on the sign of the charge derived from the curvature direction) information. A scintillator system, composed of three double layers of scintillators (S1, S2, S3 in fig. S2) provides the trigger, a time-of-flight measurement, and an additional estimation of absolute charge. A silicon-tungsten tracking calorimeter, a bottom scintillator (S4), and a neutron detector are used to perform lepton-hadron discrimination. An anticoincidence system is used off-line to reject spurious event triggers generated by particles interacting in the apparatus. Respect to balloon-borne experiments, PAMELA has the advantage of a substantially longer period of uninterrupted observing time. Furthermore, taking data in space is not affected by environmental systematics such as those due to correction for secondary particles produced in the residual atmosphere that affects balloon-borne experiments. A more detailed description of PAMELA and the analysis methodology can be found in (32, 33) and in the SOM.
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Science
Volume 332 | Issue 6025
1 April 2011
1 April 2011
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Copyright © 2011, American Association for the Advancement of Science.
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Submission history
Received: 18 October 2010
Accepted: 9 February 2011
Published in print: 1 April 2011
Acknowledgments
We thank P. Blasi, F. Donato, P. Lipari, and I. Moskalenko for helpful discussions concerning the interpretation of our results and D. Marinucci for helpful discussions on statistical methods. We acknowledge support from the Italian Space Agency, Deutsches Zentrum für Luft- und Raumfahrt, the Swedish National Space Board, the Swedish Research Council, the Russian Space Agency (Roscosmos), and the Russian Foundation for Basic Research.
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