The origin of solar particle events with low Fe/O

The origins of particle events which have low Fe/O are studied, and it is found that the majority are associated with interplanetary shocks. Separately Fe/O associated with all strong shocks in the same time period are examined. The important role played by shocks is substantiated by establishing that the average Fe/O ratio for days when a strong shock passes is 0.1, below the average value of 0.2 for large solar proton events and the solar wind. The variations of other elements are also shown.