Abstract
Spectra of x rays emitted from Ar gas at atmospheric pressure under bombardment by heavy ions (atomic number 6–79) were measured in high resolution using a curved crystal spectrometer. Values of the apparent average fraction of vacancies at the time of x-ray emission were determined from the observed satellite and hypersatellite intensity distributions. A systematic comparison of the values for the monatomic gas Ar with those obtained previously for a variety of solid targets provided a quantitative assessment of the role interatomic transitions play in the -vacancy transfer process that occurs prior to x-ray decay.
- Received 28 August 2008
DOI:https://doi.org/10.1103/PhysRevA.79.012708
©2009 American Physical Society