We investigate discharge inception in air, in uniform background electric
fields above and below the breakdown threshold. We perform 3D particle
simulations that include a natural level of background ionization in the form
of positive and O2− ions. When the electric field rises above the
breakdown and the detachment threshold, which are similar in air, electrons can
detach from O2− and start ionization avalanches. These avalanches
together create one large discharge, in contrast to the `double-headed'
streamers found in many fluid simulations.
On the other hand, in background fields below breakdown, something must
enhance the field sufficiently for a streamer to form. We use a strongly
ionized seed of electrons and positive ions for this, with which we observe the
growth of positive streamers. Negative streamers were not observed. Below
breakdown, the inclusion of electron detachment does not change the results
much, and we observe similar discharge development as in fluid simulations