Abstract

Recent beam physics studies on the two-stream e-p instability at the LANL proton storage ring (PSR) have focused on the role of the electron cloud generated in quadrupole magnets where primary electrons, which seed beam-induced multipacting, are expected to be largest due to grazing angle losses from the beam halo. A new diagnostic to measure electron cloud formation and trapping in a quadrupole magnet has been developed, installed, and successfully tested at PSR. Beam studies using this diagnostic show that the ``prompt'' electron flux striking the wall in a quadrupole is comparable to the prompt signal in the adjacent drift space. In addition, the ``swept'' electron signal, obtained using the sweeping feature of the diagnostic after the beam was extracted from the ring, was larger than expected and decayed slowly with an exponential time constant of 50 to $100\text{ }\text{ }\ensuremath{\mu}\mathrm{s}$. Other measurements include the cumulative energy spectra of prompt electrons and the variation of both prompt and swept electron signals with beam intensity. Experimental results were also obtained which suggest that a good fraction of the electrons observed in the adjacent drift space for the typical beam conditions in the 2006 run cycle were seeded by electrons ejected from the quadrupole.

Highlights

  • Electron cloud effects (ECE), including an electron cloud-induced instability, have long been observed at the Los Alamos Proton Storage Ring (PSR) [1,2,3]

  • To study electron cloud generation and trapping in a PSR quadrupole, we have developed a diagnostic which can measure the electron flux striking the wall during a beam-induced multipactor, and by pulsing a sweeping electrode can measure electrons trapped in the quadrupole after the beam pulse has left the magnet [21]

  • We have developed and successfully tested a new electron cloud diagnostic which can measure both the electron flux striking the vacuum chamber wall and electrons trapped in a quadrupole field

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Summary

INTRODUCTION

Electron cloud effects (ECE), including an electron cloud-induced instability, have long been observed at the Los Alamos Proton Storage Ring (PSR) [1,2,3]. Simulations made assuming a constant production rate (per lost proton) for primary or seed electrons from beam losses uniformly distributed around the ring reproduced a number of important features of the RFA measurements in drift spaces at PSR [9], including the time profile (pulse shape) and energy spectrum of electrons striking the wall (prompt electron signal) as well as the approximate signal amplitude. The latter effect was subsequently verified by an analytical calculation This suggests that electrons ejected from the quadrupole magnet, rather than those produced directly from beam losses in the drift space, may be the main source of seed electrons for the adjacent drift spaces. These will subsequently be amplified by a trailing edge multipactor in the drift space

QUADRUPOLE DIAGNOSTIC
EXPERIMENTAL RESULTS
Electron signals from the diagnostic
Electrons trapped in the quadrupole
Signal variation with beam loss
Prompt electron energy spectra
Evidence for electrons ejected from quadrupole
Results with an electron mirror
SIMULATIONS OF THE MEASUREMENTS
SUMMARY AND CONCLUSIONS
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