Phys. Rev. A 98, 022705 (2018)

Decays of excited silver-cluster anions Ag_n, n=4 to 7, in the Double ElectroStatic Ion Ring ExpEriment

E. K. Anderson^1,*, M. Kamińska^1,2, K. C. Chartkunchand¹, G. Eklund¹, M. Gatchell^1,3, K. Hansen^4,5, H. Zettergren¹, H. Cederquist1, and H. T. Schmidt¹

1 Department of Physics, Stockholm University, AlbaNova, SE-106 91 Stockholm, Sweden

2 Institute of Physics, Jan Kochanowski University, 25-369 Kielce, Poland

3 Institute for Ion Physics and Applied Physics, University of Innsbruck, Technikerstr. 25, A-6020 Innsbruck, Austria

4 Center for Joint Quantum Studies and Department of Physics, Tianjin University, 92 Weijin Road, Tianjin 300072, China

5 Department of Physics, University of Gothenburg, 41296 Gothenburg, Sweden

* emma.anderson@fysik.su.se

ABSTRACT

Spontaneous decays of small, hot silver-cluster anions ${\text{Ag}}_n^{-}$, $n=4–7$, have been studied using one of the rings of the Double ElectroStatic Ion Ring ExpEriment (DESIREE). Observation of these decays over very long time scales is possible due to the very low residual gas pressure ($\sim {10}^{-14}$) and cryogenic (13 K) operation of DESIREE. The yield of neutral particles from stored beams of ${\text{Ag}}_6^{-}$ and ${\text{Ag}}_7^{-}$ anions were measured for 100 milliseconds and were found to follow single power-law behavior with millisecond time-scale exponential cutoffs. The ${\text{Ag}}_4^{-}$ and ${\text{Ag}}_5^{-}$ anions were stored for 60 s and the observed decays show two-component power-law behaviors. We present calculations of the rate constants for electron detachment from and fragmentation of ${\text{Ag}}_4^{-}$ and ${\text{Ag}}_5^{-}$. In these calculations, we assume that the internal energy distribution of the clusters are flat and with this we reproduce the early steep parts of the experimentally measured decay curves for ${\text{Ag}}_4^{-}$ and ${\text{Ag}}_5^{-}$, which extends to tens and hundreds of milliseconds, respectively. The fact that the calculations reproduce the early slopes of ${\text{Ag}}_4^{-}$ and ${\text{Ag}}_5^{-}$, which differ for the two cases, suggests that it is the changes in fragmentation rates with internal cluster energies of ${\text{Ag}}_4^{-}$ and ${\text{Ag}}_5^{-}$ rather than conditions in the ion source that determine this behavior. Comparisons with the measurements strongly suggest that the neutral particles detected in these time domains originate from ${\text{Ag}}_4^{-}\to {\text{Ag}}_3^{-}+\text{Ag}$ and ${\text{Ag}}_5^{-}\to {\text{Ag}}_3^{-}+{\mathrm{Ag}}_2$ fragmentation processes.